Halliburton - Surface Data Logging Manual

Surface Data LoggingApplied Fundamentals

Sperry-Sun Drilling ServicesHouston, Texas

i

Technical Document TDTM0002ACourse 237

January 2001

Surface Data LoggingApplied Fundamentals

Sperry-Sun Drilling ServicesCourse 237

Document Number: TDTM0002A

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company iJanuary 2001

This manual contains CONFIDENTIAL AND PROPRIETARY INFORMATION and is the property of Sperry-Sun,a Halliburton Company. Neither this manual nor information contained herein shall be reproduced in any form, used, or disclosed to others for any purpose including manufacturing without the express written permission of Sperry-Sun. Manuals are company property and non-transferable to other employees, unless authorized by Management. You are responsible for this manual. DO NOT leave this manual where it may be photocopied by others.

This manual is designed to provide information useful for the optimal utilization of Sperry-Sun equipment. Charts, descriptions, tables and other information contained herein may have been derived from actual tests, simulated tests, or mathematical models. Although information has been carefully prepared and is believed to be accurate, Sperry-Sun cannot guarantee the accuracy of all information contained herein. Sperry-Sun reserves the right to modify equipment, software and documentation, and field equipment and/or procedures may differ from those described herein.

Trained Sperry-Sun personnel act as consultants to Sperry-Sun customers. Practical judgement and discretion must be used, based upon experience and knowledge, to review the circumstances for a particular job and then to perform the job in a professional manner. Accordingly, the information contained herein should be used as a guide by trained personnel, and no warranties, expressed or implied, including warranty of merchantability or fitness for use, are made in connection herewith. In no event will Sperry-Sun be liable for indirect or consequential damages arising from the use of the information contained in this manual, including without limitation, subsurface damage or trespass, or injury to well or reservoir.

Users are responsible for ensuring that they have the latest version of this manual. To verify the latest version, contact Sperry-Sun Drilling Services at (281) 871-5166.

© 2001 Sperry-Sun, a Halliburton CompanyUnpublished work, all rights reserved.Printed in the U.S.A.

ii © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Contents

. 11-18

. .

Table of Contents

Chapter 1 - Fundamentals of Petroleum Geology 1-1Physical Geology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-1

The Earth’s Size and Shape . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-2The Earth’s Relief Features . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-2Gravity . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-3

Isostasy . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-4Minerals . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-6

Cleavage . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-6Fracture . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-6Form . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-7Color . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-7Streak . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-7Luster . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-7Hardness . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-7Specific Gravity . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-8Other Properties . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-8

Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-9Igneous Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-10Metamorphic Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-13Sedimentary Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-14Deposition of Sedimentary Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-16Classification of Sedimentary Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-16Textures of Sedimentary Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-18Characteristics of the Common Sedimentary Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .Structural Features of Sediments . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-23Stratigraphic Relations of Sediments . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-24Isostatic Control of Sediments . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-28

Diastrophism and Structural Geology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-29Attitude of Strata . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-29Warps . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-30Folds . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-31Kinds of Faults . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-31

Historical Geology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-33Petroleum . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-35

Chemistry of Petroleum . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-35Chemical Properties . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-35Aliphatic Hydrocarbons . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-36Carbocycles or Aromatic Hydrocarbons . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-37

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company iiiJanuary 2001

Contents

. . . 2-. . .

. . 2-1

. . 2-18

. . 2-25 . 2-25

Origin of Petroleum . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-38Transformation of Organic Material into Petroleum . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-41Migration and Accumulation of Petroleum . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1-42

Chapter 2 - Sample Examination 2-1Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-1Collecting Cuttings Samples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-2

Shaker Samples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-3Settling Box Samples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-3Collecting the Cutting Samples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-4Collecting “Wet” Samples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-5

Washing the Cuttings . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-6Washing Cuttings From Water-Based Muds . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6Cleaning Samples From Oil-Based Muds . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-6

Processing the Samples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-8Sieve Processing . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-8

Logging While Coring . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-10Sidewall Coring . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-10

Sample Description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-11Sample Quality and Examination Techniques . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1Use of Transmitted Light . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-12Abbreviations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-12Order of Written Description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-13Rock Types . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-13Color . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-13Texture . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-14Grain or Crystal Sizes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-14Shape . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-14Sorting . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-15Cement and Matrix . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-15Fossils and Accessories . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-16

Sedimentary Structures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-17Porosity and Permeability . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-17Hydrocarbon Shows . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-17Some Criteria and Procedures For Rock and Mineral Identification . . . . . . . . . . . . . . . . . . . . . . . . .

Testing Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-18Test for Specific Rocks and Minerals . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-21

Porosity and Permeability . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-23Detection and Types . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-23Choquette and Pray’s Carbonate Porosity Classification . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Archie's Classification of Porosity in Carbonate Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

iv © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Contents

Hydrocarbons . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-26Routine Hydrocarbon Detection Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-27Other Hydrocarbon Detection Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-30Solid Hydrocarbons and Dead Oil . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-32Generalizations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-32

Problems in Interpreting Drill Cuttings . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-33Contamination from Previously Penetrated Beds . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-33Other Contaminants . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-34Miscellaneous Interpretation Problems . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-35

Geological Notes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-37Unconformities . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-37Environments . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-38

Equipment, Special Techniques and Procedures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-39Equipment and Supplies for Routine Sample Examination . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-39Thin Sections from Drill Cuttings . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-41Staining Techniques for Carbonate Rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-42Detailed Insoluble Residue Studies . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-43Versenate Analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-45Limestone-Dolomite Differentiation Using Fairbanks Solution . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-47Sperry-Sun Calcimeter . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-47Shale Factor . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-53Shale Density . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2-56

Chapter 3 - Show Evaluation 3-1Gas Determination from the Drilling Mud . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-1

Aeration Gas Trap . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-2Transportation Equipment . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-4Gas Detection Equipment . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-5

Origins of Gas Shows . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-6Definitions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-6

Sources of Gas in Mud . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-8Gas from Drilling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-8Free Gas and Liquefied Gas . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-9Dissolved Gas . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-9Effective Porosity and Permeability . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-10Summary . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-14

Factors Influencing the Amounts of Gas in Mud . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-15Flushing . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-15Fluid Invasion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-19Mode of Penetration . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-26

Circulating System . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-29

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Contents

. . .

Recovery at the Surface . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-29Borehole Contamination . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-31

Surface Influences on Gas Shows . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-32Flowline . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-32Gas Trap . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-33Gas Detection Systems . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-34

Show Evaluation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-35Background Suction Pit Mud Sample . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-35Flowline Mud Sample . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-36Steam Still . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-36Show Evaluation of Gas-In-Mud Chromatographs . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-39

Determination of Oil in the Cuttings . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-48Evaluation of a Cuttings Oil Show . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-49Determination and Evaluation of an Oil Show from Mud . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3-52

Chapter 4 - Well Control 4-1Causes of Kicks and Warning Signs of Kicks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-1

Causes of Kicks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-2Warning Signs of Kicks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-10

Basic Kill Operations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-15Shut-In Procedures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-15

Well Control Theory . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-20Kill Procedures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-27

Slow Pump Rate . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-27Shut-In Pressure . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-29Influx Identification . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-30Kill Weight Mud . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-32

Kick Killing Procedures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-32Wait and Weight Method . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-33Driller’s Method . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-37Concurrent Method . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-38

Kill Procedures with Subsurface BOP Stacks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-41Other Considerations In Deepwater Drilling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .4-48

Comparison of the Three Methods of Well Control . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-49Gas Kicks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-49Kick Tolerance . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-56Saltwater or Oil Kicks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-57

Special Problems in Well Control . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-60Lost Returns . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-60Drill Pipe Plugged or Bit Plugged . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-66Washed or Plugged Choke . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-67

vi © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Contents

Hole in the Drill Pipe . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-67Drill Pipe Off Bottom or Out of the Hole . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-68

Shallow Gas Hazards . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-69Shut-In Versus Diversion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-70Use of the Marine Riser . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-71Diverter Operation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-72

Gas Bubble Migration and Expansion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4-73

Appendices

Appendix A SPWLAR-Recommended Abbreviations for Lithology Descriptions A-1

Appendix B Classification Tables . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . B-1

Appendix C Buoyancy Factors . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . C-1

Appendix D “Formation Evaluation by Analysis of Hydrocarbon Ratios” (Pixler Paper) . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . D-1

Appendix E “Wellsite Formation Evaluation by Analysis of Hydrocarbon Ratios” (Ferrie Paper) . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .E-1

Appendix F “Factors Affecting the Surface Expression of Hydrocarbon Shows” (George Paper) . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .F-1

Appendix G Glossary . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . G-1

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Contents

viii © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Fundamentals of Petroleum GeologyPhysical Geology

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ence

Chapter 1 Fundamentals of Petroleum Geology

The initial step in acquiring a board understanding of the drilling technologies is the development of some basic understanding of petroleum geology. To understand some of the engineering requirements in oil field drilling operations requires a comprehension of the nature of the formation to be drilled.

Historically, geological studies have been concentrated in the area of the utilization of geological data as a means of locating formations having economic value.

The following discussion is intended to provide the geological background needed for sound well planning and engineering.

Specifically, this discussion will include information concerning the theory of the origin of subsurface formation, composition of formation, formation structural differences and rock mechanics. Simply stated, the intent of this section is to answer some of the basic questions concerning the nature of the formation being drilled, such as: How were rocks formed? What are they made of? How are they structured? How do rocks behave when a hole is drilled in them?

1.1 Physical Geology

Relatively few of the problems of geology are so simple that they can be solved by one method of approach. Many geologic problems require supplementary investigation using the methods, data, and theories of chemistry, biology, physics and engineering. In turn, geology has contributed data and ideas to these bordering sciences. In the natural sciences, progress in one advances all the others.

Physical geology is concerned with the physical processes that operate on and within the Earth - the processes that have given the rocks of the Earth’s crustcomposition and structure, and the forces that have shaped its surface. Manseparate sciences contribute to the broad field of physical geology. Among thmore important are: mineralogy, the science of minerals; petrology, the scienrocks; structural geology, the science which seeks to interpret the structures in the rocks; and geomorphology, the science which deals with the origin of landscapes.

Also closely associated with physical geology is historical geology, the sciencthat traces the evolution and development of the Earth and its plants and aniThis science draws extensively on paleontology, which deals with the study oanimals and plants of the geologic past. It also draws on stratigraphy, the sci

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company 1-1January 2001


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that is concerned with the order and sequence of the rocks that make up the Earth’s crust.

1.1.1 The Earth’s Size and Shape

More than 2000 years ago the Greeks discovered by geometric calculation that the Earth was spherical in shape. They regarded the Earth’s shape as a perfect snot as an ellipsoid which it is. This mistake led them to calculate the Earth’s sto be about 25% smaller than it is. Later in history this mistake became quitesignificant when Columbus mistook America for India.

The most recent calculations indicate the Earth to be an oblate ellipsoid. Thatsay, the Earth is not a perfect sphere but rather slightly flattened at the polesdiameter of the Earth from the north pole to the south pole is calculated to be7,900.4 miles, whereas the diameter through the equator is calculated to be 7,927.0 miles. Although the difference between the two diameters is only 26.6 miles, it must be taken into account in mapping and navigation. These measurements are now accepted and used internationally as the basis for ofmapping.

1.1.2 The Earth’s Relief Features

The major irregularities of the Earth’s surface are the continents and the ocebasins. Careful studies indicate that about 70% of the Earth’s surface is ocea30% land. The surface of the land is not smooth, but broken with areas of diffeelevations. Low, relatively smooth plains, usually make up the central interiorcontinents. Higher and somewhat rougher surfaced plateaus lie between theplains and the mountains. Areas of the highest elevation, the mountains, ofteclosely parallel the borders of the continents. Combinations of these three feaform the typical landscape of continents.

For our purpose as surface Data loggers, the most important relief features ooceans are the continental shelves. These border the continents and lie betwthe shore line and the edge of the abysmal depths of the oceans. From the slines, the shelves slope seaward, increasing in depth at a rate of about 12 to 6per mile, to an average depth of between 420 and 600 feet where the bottombeings to descend abruptly. The continental shelf of North America varies in dat its outer edge and even more greatly in width along different parts of its exIn the Gulf of Mexico it varies up to more than 100 miles in width (Figure 1.1)

The extreme relief features of the Earth vary from the highest of 29,002 feet asea level (Mount Everest) to 34,000 feet below sea level (Philippine Deep). Tis a vertical distance of 12 miles. It may seem fantastic, but when compared

1-2 © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001


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relation to the radius of the Earth, it dwindles into insignificance. In relation to its size, the Earth is about as smooth as a billiard ball.

Figure 1.1 Diagram Showing the Continental Shelf and the Gulf of Mexico

1.1.1 Gravity

True, the variations of the Earth’s surface may seem insignificant in relation toEarth’s size; yet, understanding them, and finding the forces which caused thnecessarily involve the basic concept of geology. The forces responsible for shaping all of the Earth’s features are part of the universal “Law of GravitatioThis law states that “every particle in the universe attracts every other particlwith a force that is directly proportional to the product of their masses, and inversely proportional to the square of the distance between them.”

Because of the Earth’s great size and density, gravity has a strong attractionobjects on or near its surface. It holds the atmosphere and hydrosphere (watthe Earth’s surface. It holds the Earth together and attracts all objects to it. Grthen is responsible for the falling of the rains, which cut away at the mountainfor the flow of streams and rivers which erode the land masses; and for the deposition of sediments in lakes and oceans.

C O N T I N E N T A L S H E L F


Fundamentals of Petroleum GeologyIsostasy

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Three factors - altitude, latitude, and variations in density of nearby rocks - affect the force of gravity at any point on the Earth’s surface. The third factor, variain rock density, is responsible for the major differences of the Earth’s featuresBecause the force of gravity is greater on rocks of high density than on rockslow density, it is concluded that heavier rocks would normally tend to occur alower elevation than adjacent lighter rocks. A principle generally accepted bygeologists and geophysicists is that the continents are composed of a lighterthan that which underlies the oceans. Careful examination of rocks taken frocontinents and ocean basins indicates that this principle is well founded.

1.2 Isostasy

The fact that the lighter continental blocks stand higher than the heavy oceansegments suggests that the two units are in equilibrium. The term isostasy (fthe Greek “isos” equal and “stasis” standing) is used to define this condition balance. Such condition means that the pressure at some depth beneath largof the Earth’s crust must be substantially the same, and that any specific differences which develop because of processes in operation at the surface,be adjusted by slow rock movement in the Earth’s plastic interior to maintain balance. Hence, if a heavy load is placed on a certain area on the Earth’s surgradual sinking of the area will follow. Conversely, if a heavy load is removed,area will rise. The isostatic movement of one area is necessarily offset by anopposite isostatic movement of another area (Figure 1.2).

Isostatic movement has not been confined to forming the continents and ocebasins. It has been active throughout the geologic past, creating shallow seamountains. In North America, isostic downwarpings have caused many differgeologic seas to deposit sediments across the entire continental area exceptarea of the Canadian Shield.


Fundamentals of Petroleum GeologyIsostasy

that tatic

Figure 1.2 Diagram Illustrating the Principle of Isostasy

Elsewhere, areas which have undergone glaciation in the recent geologic past are still rising even though the glaciers and ice sheets melted back many thousands of years ago. It is estimated that the Scandinavian area has risen 900 feet since the ice sheet melted about 12,000 years ago. Since this area is still rising, it can be concluded that it has not reached the elevation at which it stood prior to glaciation.

In areas receiving tremendous deposits of sediments, the land is gradually sinking under the increasing loads. The Mississippi River Delta is sinking at a rate of more than 8 feet per century. However, the accumulation of deposits from the river keep the depth of the Gulf of Mexico and the land area of Louisiana about constant.

It can be concluded that gravity, through the principle of isostasy, has been responsible for forming the major features of the Earth’s surface such as continents, oceans, basins, mountains, plains, etc. Also, it can be concludederosion and deposition, being a continuing process, are means by which isosmovement never reaches equilibrium. Thus gravity is the most dynamic forceacting on the Earth’s surface.


Fundamentals of Petroleum GeologyMinerals

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1.3 Minerals

Everyone realizes the importance of minerals in the nation’s industry and economy. Iron ore minerals are required to keep the steel industry operating as barite and bentonite are required by the drilling mud industry. The future oboth of these industries will be determined by the amount of mineral reservesavailable to them for preparing products. Geologists, through the science of mineralogy, are constantly seeking deposits of vital minerals in order to keepindustrial reserves high.

Mineralogy is the study of minerals. It includes their chemical compositions, crystal structure, physical properties, and occurrence.

A mineral is a naturally occurring substance which has a definite chemical composition and internal structure with characteristic physical properties. Ov2,000 minerals have been recognized and described. The vast majority are rMany of them have never been found in more than one location. Others are fonly as precious metals, gemstones, or valuable ores. Only about 20 are fouabundantly in the Earth’s crust. These are called the “rock and soil forming minerals” because they comprise all but a small fraction of the Earth’s rocks soils.

Many minerals can be identified on the basis of a single physical property. Asexample, halite, or rock salt, is identified by taste. However, most minerals reqa combination of two or more physical properties for positive identification.

The more important physical properties for mineral identification are discussebelow.

1.3.1 Cleavage

Many minerals cleave or part along smooth planes. Some minerals such as mhave a perfect cleavage in one direction only, while other, such as galena, haperfect cleavage in three directions. Terms such as perfect, uneven, hard, andare used to describe cleavage planes.

1.3.2 Fracture

Minerals which have no cleavage fracture or break irregularly. Fracture facesdescribed as being conchoidal (like glass), rough, smooth, even, splinter, or fibrous.



he

1.3.3 Form

Minerals tend to crystallize into definite, characteristically shaped crystals, bounded by smooth planes called crystal faces. If crystal faces are present, their shapes and interfacial angles are diagnostic.

1.3.4 Color

All specimens of some minerals, such as magnetite and galena, have a constant or uniform color, but others, such as quartz and calcite, may vary in color because of impurities.

1.3.5 Streak

The color of the powder of a mineral is determined by scratching the surface of the mineral with a knife or file, or it it is not too hard, by rubbing it on an unpolished porcelain surface. The streak of a mineral may be similar, or entirely different from the color of the mineral itself.

1.3.6 Luster

The luster of a mineral refers to the way ordinary light is reflected from its surface. Metallic luster is like that of polished metals; vitreous luster is like that of glass; adamantine like that of diamonds. Other self-explanatory terms used to describe luster are resinous, silky, pearly, dull, Earth, oily, and waxy.

1.3.7 Hardness

The relative hardness of two different minerals can be determined by pushing a pointed corner of one firmly across the flat surface of the other. If the mineral with the point is harder, it will scratch or cut the other. The hardness of minerals is usually recorded in terms of Moh’s Scale of Hardness ranging from 1 to 10. Tnumbers refer to the hardness of 10 minerals, arranged in order of increasinghardness.



are

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When the minerals to make up this series are not available, it is convenient to know that a pocket knife blade is about 5.5, a copper penny 3.5, and the thumbnail about 2.5. Since most minerals have a hardness of less than 6, these “tools”usually adequate for determining the hardness of an unknown specimen.

1.1.1 Specific Gravity

The specific gravity, or density, can be found by the formula:

Specific Gravity is stated as a number indicating the ratio of the weight of thesubstance to that of an equal volume of water. Specific gravity can be determby several different instruments in the laboratory.

1.1.2 Other Properties

Minerals have other physical properties which are often useful in identificatioSome of these properties are odor, taste, fluorescence, magnetism, solubilityothers react to dilute solutions of acids. When identifying minerals, geologistsoften taste, smell, scratch, and otherwise closely examine specimens. It is smwonder they are called “rock hounds.”

Table 1.1 Mineral Hardness

Hardness Mineral Hardness Mineral

1 Talc (least hard) 6 Orhtoclase

2 Gypsum 7 Quartz

3 Calcite 8 Topaz

4 Fluorite 9 Corundum

5 Apatite 10 Diamond (hardest)

SpecificGravityweightofmineralinair( )

weightofmineralinair( ) weightofmineralinwater( )–------------------------------------------------------------------------------------------------------------------------------------------=


Fundamentals of Petroleum GeologyRocks

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1.2 Rocks

One of the basic principles of geology is the Uniformetarian Principle. It may be stated as follows:

“The present is the key to the past,” or applied more specifically to oupresent subject: Rocks from long ago at the Earth’s surface may be understood and explained in accordance with processes presently goon.

It assumes that, in the geologic past, water collected in streams and carried of sediments to the sea; that marine animals lived and died in the ancient seathat their shells were buried in the deposits accumulated on the sea floor. It aassumes that ancient volcanoes erupted and extruded lava flows, just as thetoday. These and other similar assumptions are accepted truths as there is nreason to believe that the physical laws and natural processes of the geologihave changed. Therefore, if features in solid rocks can be recognized as idento those now being formed by volcanoes, streams, and beaches, it is reasonaconclude that they were formed by the same type processes which are preseoccurring.

The Uniformetarian Principle is the underlying theme for all geologic studies.evaluate any rock, which is defined as an aggregate of minerals, it is essentiknow its origin, occurrence, mineral and chemical composition, and the proceprocesses by which it was formed. All this information can usually be obtainethrough the interpretation of the significant features contained within the rockthemselves.

There are three major classes of rocks: igneous, metamorphic, and sedimenThis classification is based on origin. Igneous rocks are formed by the coolingsolidification of molten or liquid rock. Metamorphic rocks are formed by the alteration, through heat and pressure, of existing rocks. Sedimentary rocks aformed by the accumulation of sediments.

Each of these three classes is important in a fundamental study of geology beeach class has a different significance in the Earth’s history. Each class contminerals and ores which may not be found in the other two. In a study of petroleum geology for instance, sedimentary rocks are given much more attethan the other two because petroleum is found almost exclusively within them



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1.2.1 Igneous Rocks

As a geologic term, igneous (from the Greek “ignis” meaning fire) is used to describe phenomena involving natural heat, fire, and molten rocks. This description usually brings to mind an erupting volcano. Actually volcanoes aresource of only one type of igneous rock - volcanic. A second type of igneous is classified as plutonic.

The two differ mainly in their mode of origin, or the place in which they were formed. Volcanic rocks were formed on the Earth’s surface; plutonic rocks beneath it. Volcanic rocks naturally cooled much more rapidly than plutonic rocks, and as a result they are composes of very fine mineral crystals and ofhave the appearance of glass. The minerals in the volcanic rocks were allowlittle time to crystallize and grow before the liquid rocks solidified. Opposed tothis, plutonic rocks were cooled very slowly, and the mineral crystals allowedtime to grow very large. Consequently, plutonic rocks are composed of largecrystals of pure minerals. Obsidian, or volcanic glass, is a good example of volcanic rock. Granite is a good example of plutonic rock. No mineral crystalsbe distinguished in obsidian, but large crystals fragments of quartz, feldspar,magnetite may be easily distinguished in most granites.

Igneous rocks of high silica content are called acidic because of their high proportion of silica (SiO2), the acid-forming radical. As a rule, they are light in color and relatively low gravity. Igneous rocks containing a predominance of bases such as lime, magnesium, and iron are called basic rocks. They are udark-colored and heavy because of their high content of iron-bearing minera

Liquid rock material within the Earth (magma) may be spewed onto the Earthsurface through volcanic activity, or it may be intruded into rocks beneath theEarth’s surface by plutonic activity.

When magma is erupted onto the Earth’s surface, it is called lava. Lava maysolidified in two different forms; either as volcanic cones or extensive lava floThe Devil’s Postpile in California is an ancient lava flow, and the entire islandHawaii is built of volcanic cones, flows, and fragments. Volcanic rocks are in way related to the origin of petroleum, and their presence in old rocks simplyindicates ancient volcanic activity.

The underground movement of magma cannot be observed while it is in progbut the rock masses resulting from the solidification of such intrusions becomaccessible to view after being uncovered by erosion.

“Pluton” is the term given to any body of intruded igneous rock. Such masses greatly in composition and texture and in their relation to the enclosing rock. Different masses of magmas have different viscosities, and consequently a gintrusive mass represents the line of least resistance for that particular mater



Based on their shapes and sizes, plutonic rock bodies are classified as dikes, sills, laccoliths, volcanic necks, stocks, or batholiths (Figure 1.3).

Figure 1.3 Sketch of Various Modes of Occurrence of Igneous Rocks



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Dikes

Dikes are tabular bodies of igneous rocks that fill former fractures in the Eartcrust. They may cut across formations, or they may cut into masses of older igneous rocks. They vary in width from less than 1 inch to many feet, and in length from a few yards to many miles.

Sills

Sills, like dikes, are tabular intrusive masses. They differ from dikes in that thlie parallel to the formations of the enclosing rocks. Some sills are small, coveareas of only a few acres, but others are very large. Most are less than 100 fthick.

Laccoliths

Laccoliths are large lenticular masses of igneous rock similar in origin to sillsThey are formed when intruded masses lift up overlying beds into domelike structures. Laccoliths may range from 1/2 to 4 miles in diameter.

Volcanic Necks

The igneous rock solidified in the conduits that once fed volcanoes often remas remnants after erosion has removed the rest of the volcano. These cylindmasses are termed necks or plugs. They may be several thousand feet in dia

Batholiths

Batholiths are the largest and originally the deepest intrusive bodies of igneorock known. They are believed to have been the feeder sources of liquid matfor the igneous masses formed at a higher level. Batholiths are so large that are never sufficiently exposed to permit measurement of all three dimensionsMany are 50 to 100 miles wide and more than 1,000 miles long, and they exdownward to great but unknown depths. Most batholiths occur as the cores ofolded mountain system.

Igneous activity is generally considered to be the origin of most metallic mineores. Gold, silver, and copper are often found as native metals in veins of plurocks. Ores of other metals, such as lead, zinc, and nickel, are believed to habeen deposited by hot solutions from igneous rocks. Understandably, certain



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igneous rocks, especially plutonic rocks, are constantly being sought for their mineral content.

1.3.1 Metamorphic Rocks

Every rock is the product of a definite environment. Sedimentary rocks are products of deposition. Igneous rocks are products of igneous activity. There are other rocks which possess structural features different from those of either sedimentary or igneous rocks. A careful study of these rocks show that they were formed through the alteration of pre-existing igneous and sedimentary rocks. Such transformed rocks are called “metamorphic.”

Metamorphism is defined as the process that transforms rocks and minerals.factors that cause metamorphism are temperature, pressure, and chemical aThese factors increase in intensity with nearness to igneous intrusions and wdepth in the Earth.

Great heat in metamorphism usually develops a group of new minerals. Thisespecially true when sedimentary rocks are involved. High temperatures prosuch minerals as garnet and graphite from materials in sedimentary rocks. Tthe presence of garnet and graphite in a metamorphic rock indicates a condithigh temperature. However, no such distinction can be made in the case ignrocks because heat cannot be expected to greatly modify rocks formed fromcooling of molten material.

Pressures associated with metamorphism are of two types: static and dynam

Static pressure is uniform and is associated with burial. In general, static preincreases the solubility of minerals, while a release of pressure causes precipitation. Changes in static pressure thus favor recrystallization. Rocks thare metamorphosed by static pressure often show the development of enlargmineral grain size.

Dynamic pressures are uneven due to folding or deformation caused by intruDynamic pressure, if rapidly applied, causes the rock to become granulated broken down into smaller grains. If the force is gradually applied, it causes throck to flow because of internal movement of crystals. This results in deformmineral crystals. For example, a crystal cube may be elongated into a trapezRocks containing elongated, crushed, and deformed minerals indicate that thwere formed under conditions of dynamic metamorphism.

The chemically active agents which cause metamorphism are fluids, vapors,gases. The origin of these agents must be from either the rocks being metamorphosed or from intruded magma. These agents may be any compou



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water, the halogens, sulfur, carbon dioxide, iron, silica, etc. They carry many metallic elements into rocks being metamorphosed. Rocks metamorphosed by chemical activity are characterized by the presence of new minerals.

1.3.2 Sedimentary Rocks

“Sedimentary” (from the Latin word “sedimentum”) is applied to the rocks formed by the deposition of materials on the Earth’s surface. This includes roformed by the settling of materials in water; by materials precipitated from sewater, and materials deposited upon the land by wind and ice. The great maof all sedimentary rocks, however, were formed from materials deposited in tocean or in bodies of water directly connected with it.

Sedimentary rocks are the most common on the surface of the Earth. They capproximately 75% of the land surface. Geologists estimate that they range ithickness from a thin film to more than 40,000 feet.

Most of the material of which sedimentary rocks are composed comes from tweathering and erosion of older rocks. The two materials produced by weathare fragments of rocks and soluble salts. The fragments are called clastic (brmaterials; the soluble salts are called chemical materials. The former are transported from their place of origin by water or wind, while the latter are removed in solution. A third type of material found in sediments is derived froplants and animals. It is called organic material. The deposition of these thretypes of material has formed all sedimentary rocks. Something of the origin ahistory, of sedimentary rocks can be learned by studying the materials of whithey are composed.

Clastic Material

The deposition of clastic materials produces clastic rocks such as shales, sandstones, and conglomerates. The essential difference between these rocthe size of the fragments of which they are composed.

A size scale of clastic materials is shown in the following table. These sizes athe ones commonly accepted by geologists.



Clastic fragments are sorted by the action of various transporting agents. Thus, if the materials have about the same specific gravity, fragments of about the same size will be deposited together. If the materials differ in specific gravity, large fragments of light material will be mixed with small fragments of heavy material in deposition.

The shapes of fragments may be described as angular, sub-angular, and rounded. Rounded fragments usually result from wear during prolonged transportation. Sharp, broken fragments generally have been deposited near their source. Thus, the shape and size of clastic materials are important guides to geologists.

Chemical Materials

The most abundant soluble salts are calcium carbonate, silica, sodium chloride, and compounds of magnesium, potassium, iron, and aluminum. These salts are of varying solubilities in river water. Some of them are very soluble in sea water, while others are not. The manner in which these compounds form sedimentary rocks will be discussed later.

Organic Materials

The organic materials which form a small part of the sedimentary rocks are derived from land and marine plants and animals. They contribute organic material in the form of carbon. Under very special conditions, depositions of carbonaceous materials become coal or petroleum. Swamps and lagoons along shores are ideal sites for the deposition of carbonaceous material.

The hard skeletons of shells of marine animals are relatively insoluble in sea water. They are composed largely of calcium carbonate and silicon dioxide. In some areas, these materials have formed thick deposits of sedimentary rocks.

Table 1.2 Size of Clastic Materials

Kinds Diameter (mm)

Boulders over 256

Cobbles 64 to 256

Pebbles 4 to 64

Granules 2 to 4

Sand 1/16 to 2

Silt 1/256 to 1/16

Clay Below 1/256



1.3.3 Deposition of Sedimentary Rocks

At present, sediments are being deposited almost exclusively on the 10,000,000 square miles of the continental shelves. In the geologic past sediments were deposited far inland in seas no longer existing. For example, in the interior of North America, there were seas some 2,000 miles wide. In these seas, materials were carried hundreds of miles out from the existing land, resulting in a single continuous deposit of sandstone, shale, or limestone covering many thousand square miles.

1.3.4 Classification of Sedimentary Rocks

By origin, sedimentary rocks may be classified into three groups: clastic, chemical, and organic. These groups may be shown graphically (Figure 1.4).



Figure 1.4 Sedimentary Rocks Chart

Formed through weathering

Mechanical weathering Chemical weathering

Produces fragments of minerals and rocks that are removed mechanically and deposited as the Clastic Sedimentary Rocks.

Produces insoluble products that are Produces soluble products that are

BouldersConglomerates CobblesBreccias Pebbles

GranulesSandstone SandSiltstone SiltShale Clay

Chemical Sedimentary Rocks

Removed in solution by streams and deposited as the

Organic Sedimentary Rocks

The rocks formed from substances slightly soluble in sea water; hence deposited soon after reaching the sea.

The rocks formed from substances very soluble in sea water; hence deposited only as a result of evaporation.

Limestone...CaCO3

ChalkDolomite... MgCO3

Chert..........Solublesilica

FlintHematite ......... IronLimonite ......oxides

Calcareous Limestone

in order of deposition

Gypsum .CaSO42H2OAnhydrite........ CaSO4

Salt (halite) ........NaCl

Potassium and Magnesium minerals

Siliceous Diatomite

CarbonaceousCoal

PetroleumNatural Gas

The carbon is derived dominantly from CO2, hydrogen from water, other constituents, indirectly, through weathering and alteration.



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1.4.1 Textures of Sedimentary Rocks

There are many different classifications of textures of sedimentary rocks. For surface data loggers, only four of these require definitions:

1. Fragmental textures range from very fine-ground clays to coarse boulders or blocks. They occur in clastic rocks.

2. Crystalline textures occur in evaporites and other chemical rocks precipitated from aqueous solutions. The crystals may be microscopic, as in chert; fine-grained, as in common limestone; or coarse-grained, as in some rock salt.

3. Oolitic textures occur in some limestones and sandstones. The term means egglike. Thus, an Oolitic rock is made up of small shotlike bodies crowded into a solid mass. The individual “egglike” bodies are composed of concenlayers of calcite deposited about a minute grain, such as sand. Oolites mformed of calcite, silica, hematite, and other minerals.

4. Textures resulting directly from the activities of organisms, such as shellsclassified as organic structures instead of textures.

1.4.2 Characteristics of the Common Sedimentary Rocks

Breccia

A rock composed of cemented angular fragments of other rocks is a breccia.Breccias are common along fault zones. They sometimes grade into conglomerates when the fragments are slightly rounded. Breccias are deposvery near their source; when the fragments of which they are composed are carried a greater distance from the source, the fragments are rounded througwear, and a conglomerate results.

Conglomerates

A conglomerate may be made up of any kind of rock fragments held togethesome cementing material such as shale or clay. Its distinguishing characterisrounded coarse fragments. Conglomerates are necessarily younger than thefragments of which they are composed.

Sandstones

Sandstone is composed of fragments and grains from a size smaller than thoconglomerate down to grains of about the size of ordinary granulated table sThe principal distinction between coarse sandstone and fine conglomerate is



the sandstone is more apt to contains grains or fragments of rather uniform size, without any unduly large pebbles. Sandstone can be described as fine, coarse, or medium. It should be described as soft if it can be crumbled in the fingers, hard if it breaks with difficulty with a hammer and medium-hard if it breaks under an ordinary hammer blow.

Sandstones are usually deposited in water relatively close to a seashore. Such an area along the shore is today, and has been in the past, the home of numerous shellfish, such as clams, oysters, conch shells, scallops, sand dollars, and related forms of life. These shells are composed of calcium carbonate or calcite. As previously mentioned calcite is the principal natural cement and the presence of numerous shells in the sandstone is a source of calcite which may in time, dissolve and be redeposited again among the sand-grains cementing them together into a solid rock. Complete fossil seashells are also common in sandstones.

Wind-Deposited Sandstones

Sandstones are also formed by the solidification of wind-blown sands on land. A wind-blown sand deposit might be found underneath marine water deposited sediments if an area such as the Sahara Desert should be suddenly submerged beneath the sea. Wind-deposited sandstones are, on the whole, rare among oilfield sediments and do not warrant much discussion. However, their present is significant if they are found, as it indicates that the area was dry land and not ocean at the time of deposition. This might be of great importance, since the source of oil is almost universally marine organic material.

A well known wind-deposited sandstone formation is the Navajo sandstone of the Navajo-Grand Canyon-Zion National Park area.

Siltstone

Siltstone is a rock composed of material whose small particles are larger than the fine material of true shale and too small to be called sandstone. When broken in the fingers, it is gritty rather than slippery, and often it is composed of a mixture of fine sand grains and mud. For general purposes, a coarse siltstone could be included under sandstone or a very fine siltstone might be included with shale.

Shale

Shale is the rock formed from compaction and solidification of the fine materials of sedimentation which originally settled out in the water as mud. Consequently, it is a deposit formed at greater distances from the shore than a conglomerate or a sandstone, the material of which drops to the bottom as soon as the speed of the



fers

ings.

is

depositing current is reduced where a river runs into the ocean. The tiny particles which make up shale will remain suspended for a long time even in still water. Fine material washed into an ocean by a river may be caught in some of the slow-moving ocean currents and transported for many miles. Hence, deposits of shale of decidedly uniform character may be deposited over thousands of square miles of ocean bottom.

Often the deposition of shale is periodic, not continuous. This may be due to several causes, and much remains yet to be learned on the subject. Seasonal floods, for example, may be a cause. Rivers often carry large loads of erosion products during floods, and are relatively clear and carry nothing for other periods of the year. In such cases, a film or layer of mud would be deposited on the bottom after each storm or flood, and in long geological time, many thousands of such films or layers would pile up. Shale formed by the solidification of such a deposit of many layers, would be banded or bedded rock, and a core or surface exposure of it would show bedding or stratification. There would actually be visible fine line or bands in the rock. According to local conditions which caused the bedding or stratification, the beds or strata might be a fraction of an inch thick or several feet.

All material that is fine is not necessarily of the same composition. The fine materials which accumulates to form shale is naturally ground up (and perhaps altered) material of the rocks of the land from which it was eroded. Since numerous kinds of rocks exist at different localities, their erosion products are different, even though ground up to the same size particles. For this reason, all the shale in the world is not alike. The particles of which it was composed are alike, but only in size. Therefore, there are many different kinds of shale.

As there is no particular advantage in using new names for the different varieties, they are all generally called shale, without another qualifying word added to indicate what kind. A shale containing an important amount of calcium carbonate (line) is referred to as a calcareous shale or simply limey shale. Likewise, shale containing a large amount of silica, such as much of the Monterey shale of California, is called siliceous shale. Many local characteristics are also used, such as as “nodular shale”, “poke chip shale” (when the cores split into smooth waor plates resembling poker chips), “paper shale”, and others.

Limestones

Limestone is different from any of the above described sedimentary rocks, because it is a chemically deposited sediment and not from mechanical settlThe relation of erosion to the formation of limestone is not the carrying fine particles of calcite (CaCO3 - the mineral of which limestone is composed) but it to carry instead, calcium carbonate to the ocean in solution.



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This calcium carbonate is in solution in sea water as is salt. Certain animals living in the sea, principally corals, and small forms of life known as bacteria, are able to extract calcium carbonate from the sea water and, by rather vaguely known like processes, to resolidify or precipitate it as small, solid crystals of calcite. By this process, deposits of limestone rock accumulate on sea floors where there is an abundance of coral or peculiar bacterial life.

Certain plants such as algae can also extract calcium carbonate from sea water and deposit it as limestone.

The life forms which are able to deposit limestone live in warm tropical or sub-tropical waters, such as the Coral Sea north of the Great Barrier Reef, which extends for more than a thousand miles along the northeast coast of Australia. These animals require, in addition to warm temperatures, clear waters, fairly free from stifling turbidity. Such conditions existed in past geological time in the limestone area from the Gulf of Mexico far north to Canada. If the small, oil-containing forms of life are also present and accumulate with the limestone, a pertroliferous or oil-bearing limestone will be deposited. Such rocks have produced oil fields in many parts of the world.

Dolomite

If a large part of the calcium in a limestone is replaced by magnesium, the rock is dolomite. Dolomitization is a common process in limestones of all ages, and it is often accomplished during the process of sedimentation. In fact, many so called “limestones” are dolomites.

Chalk

Chalk is a special type of limestone composed of small shells, or fragments, cemented together. Forminifera shells constitute a large part of the material, the presence of shells or other organisms is common. Chalk usually is soft, porous, and white or grey, and some of it is massive in appearance. The chacliffs of Dover, England, are an example. Some of the chalks of the Southweparticularly those of Texas, grade into denser beds that are as well consolidaordinary limestone.

Marl

The porous masses of shells and shell fragments that accumulate on the botof may freshwater lakes form marls. The term marl is used also to designatecalcarious shales in which clay and finely divided particles of calcium carbonare mixed.



Coquina

This term usually is applied to the more recent deposits of cemented shell accumulations.

Reefs

Fossilized corals and associated marine life form another type of limestone known as coral reefs. These limestones possess the skeletal features of the organism of which they are formed. Reefs are formed in tropical waters along the shore of land masses and around islands. They were probably formed in all of the ancient inland seas of North America. Reefs are more technically known as bioherns.

Chert

Chert is a hard, compact, dense, siliceous material that occurs as distinct layers, or as pebbles, in the beds of other rocks. Either colloidal silica was deposited with the other sediments, or after deposition, silica-bearing waters partially replaced the associated sediments.

Diatomaceous Earth

Diatoms are minute plants that live in great numbers in the sea and in freshwater lakes. When they die, their siliceous skeletons accumulate to form diatomaceous Earth. At many places diatomaceous Earth is interbedded with shales.

Coal

Coal is formed by the compacting and partial decomposition of vegetable accumulations. The alteration of vegetation into peat, lignite, and various other grades of coal is a long process. The grade of coal is dependent upon the kind of material deposits and the amount of alteration that has taken place.

Salts and Gypsum

Several different metallic salts are present in sea water. They are listed in the following table.



When sea water is evaporated to dryness, the salts come and are deposited. The least soluble salts are deposited first. Calcium carbonate and iron oxide, if present in the water, are the first to be deposited. Gypsum follows, and often with it some anyhdrite is deposited. After gypsum, sodium chloride, or common table salt, is deposited. The bitter salts consisting of sulfates and chlorides of potassium and magnesium are deposited last. These are so soluble that they are not always deposited with salt and gypsum. The rocks formed in this manner are called evaporites. Thick deposits of evaporites were probably formed in evaporating bodies of sea water which intermittently received influxes of fresh sea water.

Associated with salt and gypsum in many places are red beds, composed mainly of red sandstones and shales. These are red because they contain small amounts of iron oxide. It is believed that they have been formed under arid conditions.

1.4.3 Structural Features of Sediments

Stratification

The most distinctive structural feature of sedimentary rocks is their arrangement in beds, layers, or strata.

Cross-bedding

Sediments that show parallel bedding at an angle to the planes of general stratification are cross-bedded. Wherever steep slopes are produced by the rapid deposition of sediments (as at the front of a delta or on offshore bars, barriers, etc.)

Table 1.3 Salts Present in the Ocean

Composition Percent

Sodium Chloride, NaCl 77.758

Magnesium Chloride, MgCl2 10.878

Magnesium Sulfate, MgSO4 4.737

Calcium Sulfate, CaSO4 3.600

Potassium Sulfate, K2SO4 2.465

Calcium Carbonate, CaCO3 0.345

Magnesium Bromide, MgBr2 0.217

Total 100.000



cross-bedding occurs. Wind-lain deposits, such as sand dunes, are characteristically cross-bedded.

Graded Bedding

When a mixture of particle grains is brought to the site of deposition, the coarser and heavier grains settle more rapidly than others. It follows then that the bed of sediment finally accumulated shows a segregation of the grains as determined by their relative rates of setting. Thus the bottom portion of a bed may consist of coarse or heavy particles, whereas the upper portion is made up of relatively fine or light particles. Such an arrangement is called graded bedding. The presence of graded bedding in rocks indicate seasonal deposition within a relatively still body of water.

1.4.4 Stratigraphic Relations of Sediments

Conformity and Unconformity

Deposition of materials in areas is not always constant. When the area is elevated, or uplifted, deposition ceases and erosion naturally begins. When an area subsides, or sinks, erosion ceases and deposition begins.

When the deposition of a series of beds is constant, one bed is said to lie on the other with conformity. If, however, there is an interruption in deposition, and erosion takes place, the bed deposited immediately after the interruption is said to lie on the eroded surface in an unconformable manner. If the beds below the eroded surface are tilted so that they form an angle with the overlying bed, the contact is called an angular unconformity (Figure 1.5).

Figure 1.5 Sketch of an Unconformity



Overlap and Offlap

Normally, when streams and rivers reach the sea, their velocity is reduced. Because of this, the sediments which they carried are deposited layer upon preceding layer.

If the sea is transgressing on the land, the velocity of the streams and rivers are reduced progressively farther inland; thus, succeeding sediments carried by these agents are deposited progressively farther inland, forming layers which overlie beds formed by preceding deposits and the eroded surface on which the sea has transgressed. This arrangement of layers of sedimentary rocks is called an overlap (Figure 1.6).

Figure 1.6 Diagram Showing an Overlap

A complete reversal of this occurs when the sea is regressing. Sediments carried to the sea by rivers and streams are deposited progressively farther from the original shore line. As the sea regresses, young deposits of sediments are exposed, eroded, and carried once more into the sea and redeposited progressively further from the original shore line. The arrangement of layers of sedimentary rocks is called offlap (Figure 1.7).



Figure 1.7 Diagram Showing an Offlap

Lateral and Vertical Variation of Sediments

In a sedimentary basin constantly receiving sediments at a uniform rate, the sediments become graded laterally prior to deposition. The coarse gravels are deposited near the shore line; the pebbles and sands are deposited farther out; the silts and clays are deposited still farther out; and the limes and calcareous oozes are deposited out beyond the clays in relatively quiet water. The deposition of these sediments may extend to cover an area several hundreds of miles in length and width. The layer of rock that is formed from sediments graded in this manner will occur as a conglomerate in one geographical area, a sandstone in another area, a shale in another area, and a limestone in another. The different types of rocks formed by this grading process in a geographical area are sedimentary equivalents, and they are called facies. This name indicate that they were formed during the same period of deposition.

During a period of deposition, thick layers of like sediments may be accumulated only if the supply of sediments remains uniform and the shore line remains stable. In other words, conglomerates are deposited on top of conglomerates, sands are deposited on sands, etc. If the shore line shifts (because of a transgressing or regressing sea) or if the supply of sediments fluctuates (because of changing velocity of the streams and rivers), the lateral sequence of deposition is also



shifted. Repeated lateral shifting of the depositional sequence causes conglomerates to be deposited over sands, and sands to be deposited over shales, when the shore line shifts seaward. The reverse occurs when the shore line shifts inland. This results in an interfingerng, or interbedding, of lateral facies. Detailed studies of such lateral changes are of utmost importance in the search for petroleum (Figure 1.8).

Figure 1.8 Diagram Showing Ideal Lateral and Vertical Variation Within Sedimentary Rocks



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Fossils and Their Significance

“Fossil” (from the Latin word “fossilis” meaning dug up) refers to any remainsdirect evidence of plant or animal life preserved in the rocks of the Earth’s cru

Since plants have few preservable parts, plants are not so well represented bfossils as are animals. However, some plant fossils do occur as graphitic remor as impressions of leaves and stems in shales and sandstones. The woodyof other plants have been filled in by silica, producing silicified wood as may found in the petrified forest of Arizona.

The shells, bones, teeth, and general skeletal matter of animals, even their trtrails, and burrows have been fossilized. In some cases the entire animal haspreserved, constituting unique fossils of great valve.

Such remnants show the development of life through the long ages of the Eahistory. The more primitive forms of life are found in the earliest rock formatioEvolutional changes are recorded by the fossils in the rocks of succeeding timother words, the oldest sedimentary rocks contain the oldest, most primitive foof animals, and the youngest sediments, those being formed now, will contaitoday’s forms of animal life.

A fossil-bearing rock may be dated by the fossils it contains. Thus, geologistshave come to recognize certain fossil forms as indices, or guides, to certain geologic ages. Many animals evolved into the animal forms of today; whereamany others became extinct at various times during the geologic past. Somethese animals lived for such a short time that their traces may be found only extremely thin zones within a rock formation. These are called “horizon markand they are excellent guides for correlating across facies changes. If the fosoccurring in the sedimentary rocks of two widely separated areas are alike, itfollows that these sediments were accumulating during approximately the saperiod of geologic history.

1.5.1 Isostatic Control of Sediments

As shown by fossils, and other features, a large part of the sedimentary rocksformed in shallow seas and oceans. In several mountain ranges these sedimare tens of thousands of feet thick. The inference is that the accumulation of thick deposits of sediments in shallow waters was made possible by progressubsidence of the sites of deposition. This subsidence is attributed to isostatmovement (the sinking of an area because of a heavy load of sediments). Hothen did this area become a mountain? In precisely the same manner. Whenheavy load lowered a nearby are area, this area was raised as a counterbala


Fundamentals of Petroleum GeologyDiastrophism and Structural Geology

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ith ght t

The character of sedimentation depends in part upon the balance between the rate of subsidence and the rate of filling of a basin. Contemporaneous changes in the source areas also affect the character. Notable uplift adjacent to a basin would supply a great bulk of coarse sediment, whereas long-continued erosion of stable land would change the sediment to fine mud and solutions. If little water reached a basin, evaporation would begin, causing the deposition of evaporites.

Hence, sedimentary rocks, by their composition, texture, thickness, area distribution and other characteristics, reflect the complex interplay of a number of factors. Perhaps the most influential of these is isostatic movement.

1.6 Diastrophism and Structural Geology

Sedimentary rocks are normally deposited horizontally in parallel layers. After deposition some of these rocks were subjected to forces which caused them to become warped, tilted, uplifted or otherwise changed from the original positions and elevations. The forces which cause these changes are called “diastrophmountain building forces. The resulting changes are grouped together underterm “diastrophism.”

The rock patterns formed by diastrophic forces acting on parallel layers of roare called “structures.” Certain types of structures form traps in which petrolemay be found. Therefore, many methods of petroleum prospecting are basedthe location and identification of subsurface structures. For this reason, strucgeology is an essential subject in the study of petroleum geology.

Structures may be classed as (1) gentle warps, (2) folds, (3) joints and (4) faSince these structures are not usually seen in their entirety, the “attitude” of trocks of which they are composed may serve as a guide to identification.

1.6.1 Attitude of Strata

The attitude of a bed of rock or strata refers to its dip and strike. The term dipdesignates the angle a bed is tilted from its original horizontal position. Dip ismeasured in the direction of steepest inclination. For example, a bed may hadip of 30o toward the southeast.

The term strike designates the direction of the intersection of a bed of rock wthe horizontal plane. The direction of strike is measured by a compass at a riangle to the direction of dip. In the example, the strike of the bed is northeas(Figure 1.9).



this e

Figure 1.9 Diagram Illustrating the Dip and the Strike of a Tilted Bed

1.6.2 Warps

Rocks which have been warped form gently sloping structures, such as irregular shaped basins and domes. The beds of rocks in such structures are gently tilted. Uniformly tilted beds are “homoclines.” This name indicates that the strata of structure are inclined in the same direction. Broad downwarped structures arcalled geosynclines (Figure 1.10).



r hich and r

Figure 1.10 Diagram of a Geosyncline

1.6.3 Folds

Where beds of rock have been subjected to extreme horizontal forces, they bend into folds with alternating crests and troughs. The principal types of folded structures are anticlines, synclines, and domes and basins. Where the beds of rock are arched up like the roof of a house, they form an anticline, i.e. the bed dip away from each other. Downfolds, or troughs, where the beds dip toward one another, are call synclines.

1.6.4 Kinds of Faults

If the hanging-wall block of a fault appears to have moved down, the fault is called a “normal fault.” If it appears to have moved up, the fault is a “thrust” o“reverse” fault. Faults that cut across the dip of beds are “dip-faults.” Those wlie parallel to the strike are “strike faults.” Those which cut across both strike dip are “oblique faults.” Dip, strike, and oblique faults may be either normal oreverse.



een

Some faults are neither normal or reverse, but involve longitudinal movement parallel to the fault plane, as in the San Andreas fault of California. Such a fault is a “rift” or “tear fault.”

A block depressed between two faults is a “graben,” and a block raised betwtwo faults is a “horst” (Figure 1.11).

Figure 1.11 Diagrams of Various Types of Faults


Fundamentals of Petroleum GeologyHistorical Geology

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1.7 Historical Geology

Historical geology is that branch of the geologic science that relates to the past history of the Earth. It depends on virtually all knowledge of the field of physical geology gained in the study of minerals, rocks, geologic processes and structures. It uses this knowledge in deducing the conditions and events of the Earth’s p

In the study of Earth’s history we seek to understand the origin and developmof the continents and oceans, the changing geography of the lands and seasappearance and disappearance of great mountain systems, the occurrence oprolific volcanic activity at different times and places, and the great climatic changes. In addition, the study includes the innumerable fossils of prehistoricplants and animals, many of which represent forms of life which have long sibecome extinct. If these remains were not preserved in the rocks, much of thEarth’s history would not be revealed.

In historical geology the term correlation is applied to the process of determinthe age equivalence of rock formations. The basic requirement for correlationin the fact that no one area on the Earth’s surface presents a complete recorgeologic history. Sedimentation was interrupted in one region while it proceein another. Crustal disturbance generally accompanied by vulcanism, was similarly active. The aim of correlation is to determine the relationship of the rocks of one area to those in others. The tools of correlation are formation continuity, lithologic similarity, structural relations, organic remains and fossil

The term “geologic column” refers to the entire succession of rocks, from oldto youngest, that are known to occur in a given region, or on the Earth as a wThus, we speak of the geologic column as a “geologic time scale” or a “stratigraphic section” for a given area because it is a record of the events thtook place in that area. This geologic time scale consists of major and minor divisions arranged in proper time sequence. The names given to the divisiongeologic time differ. However, these variations are confined mainly in the nomenclature of the smaller units.

The largest units of geologic time are called “eras.” An era is a time division consisting of two or more periods. It is recognized as a major chapter in the Earth’s history. Periods are major segments of geologic time which have worldwide application. They comprise successive groupings of lesser formatiEach is broadly characterized by particular organisms. In most parts of the wthere are distinct breaks between rocks of adjacent periods, called unconformJust as eras are divided into periods, periods are divided into epochs.

Variation in the sedimentary record on different continents, or in sedimentarybasins of the same continent, often produce epochs that are only regional in s


Fundamentals of Petroleum GeologyHistorical Geology

The standard geologic time scale is divided into eras, periods, epochs, ages, stages, and substages. Because many local variations in nomenclature this presentation will be limited to a discussion of the eras, periods and epochs as we are concerned with them as surface data loggers.

The following table represents the geologic column and time scale used by the U.S. Geological Survey.

Often a geologic cross-section accompanies a geologic column. A geologic cross-section is a graphic representation, over an extended area, of the attitudes of the subsurface formations.

Table 1.4 Geologic Column and Time Scale

Era Period Epoch

Cenozoic Quaternary Recent Pleistocene

Tertiary PlioceneMioceneOligoceneEocenePaleocene

Mesozoic CretaceousJurassicTriassic

Paleozoic PermianPennsylvanianMississippianDevonianSilurianOrdovicianCambrian

Proterozoic KeweenawanHuronianTimiskamingian

Archeozoic Keewatin


Fundamentals of Petroleum GeologyPetroleum

1.8 Petroleum

1.8.1 Chemistry of Petroleum

Petroleum is a complex mixture of gaseous, liquid, and solid hydrocarbons. In addition there are compounds which contain oxygen, nitrogen, and sulphur. Frequently, relatively small amounts of water and inorganic matter are present.

The properties of different samples of petroleum are not uniform because of varying chemical composition and the presence of impurities. Petroleum occurs in the physical state as a liquid (crude oil), as a gas (natural gas), or in a solid or semi-solid state (as asphalt). Since petroleum in the natural reservoir occurs, in most cases under pressure, some of the gases and certain solid matter are dissolved in the liquid.

1.8.2 Chemical Properties

Hydrocarbons are grouped into two general series on the basis of the chemical union of the carbon atom and the resulting character of the series. The first series, in which the carbon atoms are linked in a straight chain, is known as the open-chain or aliphatic series. The second series, in which the carbon atoms are arranged in a closed-chain or ring, is known as the closed-chain or carbocyclic series. The formula of the open-chain series is arranged in a straight chain as shown by the structural formula for butane (C4H10).

Figure 1.12 Structural Formula for Butane

It is evident that each carbon atom is united with one or more additional carbon atoms, and the remaining unsatisfied valences are united with hydrogen.

The formula for the closed-chain series is arranged in a ring as shown by the structural formula for benzene (C6H6).

CH C C C

H H H H

H

H H H H



Figure 1.13 Structural Formula for Benzene

1.8.3 Aliphatic Hydrocarbons

Paraffin Series

The members of the paraffin series occur extensively in natural gas, crude oil and mineral waxes. This series consists of such widely known compounds as methane, ethane, propane, butane, pentane, etc. Gasoline and kerosene consist mainly of the paraffins. The members of the series are saturated hydrocarbons containing only singly linked carbon atoms. The basic formula for this series is C2H2n+2.

Olefine Series

The Olefine series members contain two less hydrogen atoms than those in the paraffin series. The basic formula for this series is CnH2n. Some of the members of this series are ethylene, propylene, butylene, etc. The Olefines are similar to the paraffins in physical properties but they are different in chemical properties. The olefines have double bonds between some of the carbon atoms, as propylene (C3H6).

Figure 1.14 Structural Formula for Butane

CH C H

CH C H

C

H

H

C

C C C

H H

H

H H H



Acetylene Series

The basic formula for the acetylene series is CnH2n-2. Members of this series have two carbons united by triple bonds. There are two less hydrogen atoms in compounds of this series compared with corresponding members of the olefine series.

Diolefine Series

The diolefines are unsaturated hydrocarbons having the same basic formula as the acetylenes, CnH2n-2. However, the structural formula differs in the the diolefines have two double-bonded carbon atoms instead of one triple-bonded carbon atom.

1.8.4 Carbocycles or Aromatic Hydrocarbons

Benzene Series

The members of the benzene series are all unsaturated cyclic compounds; that is, the carbon atoms are arranged in closed rings. The rings are very stable, but the hydrogen atoms are easily replaced by radicals and side chains. Members of this series are found in almost all crude oil and natural gas.

Cycloparaffin Series

This series is known as alacyclic because it possesses both the properties of aliphatic and cyclic hydrocarbons. It resembles the paraffin series in chemical and physical properties except for density, which is greater. The basic formula is CnH2n, and the structural formula is cyclic, but the members are saturated hydrocarbons since they have single bonds between the carbon atoms.

Napthalene Series

Compounds of this series have the basic formula CnH2n-12. In the structural formula napthalene, C10H8, the nucleus is composed of two rings, which is a typical structural formula for the series.



in of

.

e at the es or to

Figure 1.15 Structural Formula for Napthalene

Crude petroleum is composed, then, almost entirely of a mixture of aliphatic or carbocyclic hydrocarbons. There is little information as to the actual ratio of the two types of hydrocarbons in oil, but it seems probable that the cycloparaffins predominate.

The low boiling fraction of practically all petroleum is composed of paraffin series hydrocarbons. However, the differences in oil from various sources are exhibited in the higher boiling fractions. If residue after the removal of the volatile members consists of large amounts of paraffin or wax, the petroleum is classified as a paraffin base oil. Similarly, if napthalenic hydrocarbons predominate the petroleum is an asphalt base oil.

1.8.5 Origin of Petroleum

The origin of petroleum is one of the unsettled problems of petroleum geology. It is made doubly complex because of petroleum’s migratory nature. Because petroleum is fluid and capable of movement, the source rock (where the petroleum is formed) may or may not also be the reservoir rock (where the petroleum is found). This has caused a great deal of uncertainty about the origpetroleum, resulting in the advancement of innumerable theories.

These theories may be divided into two groups: the inorganic and the organic

Inorganic Theories

Inorganic theories were the first advanced to account for the formation of petroleum. Betheolot, in 1866, suggested that mineral oils were formed by thaction of water on metallic carbides. He based his idea on the assumption thinterior of the Earth contained free alkaline metals with which carbon dioxidecould react at high temperatures to form carbides and acetylides. The carbidacetylides would then react with water to form acetylene, which when heated

HC C

HC C

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HC

CH

CH

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CH



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approximately 900oC, polymerizes to form benzene, one of the hydrocarbon series.

Medeleef, about this time, also showed that the action of carbon dioxide and water upon the alkali metals (sodium and potassium) gave off small quantities of hydrocarbons.

Both of these theories would be acceptable, but for the fact that neither pure carbides nor pure alkali metals are known to exist in the Earth’s crust. If theyexist in the pure state they can do so only at the high temperatures associatevolcanic phenomena. As a greater part of the Earth’s oil fields are far removefrom any center of igneous activity, these theories were never seriously acceby geologists.

Other unacceptable inorganic theories of the origin of petroleum concern thereaction of a volcanic gas (ammonium chloride) with native iron, or the reactibetween limestone and gypsum at very high temperatures which forms disassociated water and carbon.

Organic Theories

The organic origin of petroleum is generally accepted by scientists. But thereremain many problems as yet unsolved. It is generally believed that petroleuoriginated by a series of complex processes from plant and animal substancThe exact nature of the original organic material is not known, although muchvaluable data on this has been assembled. The biological, chemical and geolprocesses necessary for the conversion of the organic matter of plants and aninto hydrocarbons are not completely understood.

It has been reasonably established that petroleum is of organic origin becaus

1. Some petroleums are optically active, i.e., most oils have the power of rotating the plane of polarization of polarized light. Only matter derived froorganic origin could have this power.

2. Petroleum contains nitrogenous compounds. All such compounds found nature are either of plant or animal origin.

3. Some petroleum contains chlorophyll porphyrins, which are derivatives obtained from the chlorophyll of plants or from the blood cells of animals.

4. Some petroleums contain hydrogen sulfide gas which results from bacterdecomposition of plants and animals.

Despite considerable research there is still a wide divergence of opinion as ttype of organic material which can be changed into petroleum.



Organic matter that might be considered as potential source material for petroleum occurs in a wide variety of both animals and plants. This fact alone may explain the great variation in petroleums found in nature. On the other hand, the source material may have consisted predominantly of a single type of organic matter. The variations in composition may have developed later as a result of migration, bacterial action, metamorphism, etc. As yet there is no conclusive evidence indicating whether the primary source material of petroleum consists of many types of organic matter or one predominant type.

The primary source of the organic matter in sediments may be either animal or vegetable remains, or both. Some of this matter is carried to areas of sedimentation by streams, waves, or currents, and some of it remains where it occurred. Since most petroleum deposits are closely associated with marine sediments, it follows, then, that petroleum very likely originated in marine sediments. Consequently, the organic matter of the oceans is of utmost importance in the study of the origin of petroleum.

Most of the organic matter in sea water is either dissolved or is in a colloidal form. The rest is contained in the plant and animal like of the ocean, chiefly in plankton, the microscopic and semi-microscopic free-swimming organisms.

It is difficult to estimate the rate at which organic matter is produced in the sea. Plankton, for instance, is produced at a rate as high as several hundred grams per cubic meter of sea water per year. Photosynthesis (the process whereby plants convert carbon dioxide and water into carbon compounds under the influence of light) has been estimated to produce 12 million tons (80 million barrels) of hydrocarbon material annually in the ocean. A minute fraction of this material, preserved in sedimentary rocks, could be transformed into all known petroleum deposits, plus those that we can expect to discover in the future.

Organic matter is formed not only by plants and animals in the ocean but also by those on land. Much of it formed on land eventually reaches the ocean by streams and rivers in solution or in colloidal dispersion. In fact, of 50% of the sedimentary materials carried by streams and rives may be organic matter.

In this regard, humic substances are probably the most important organic materials formed on land. They are formed by the slow decomposition of lignins in peat. They are found in soil highly charged with decaying vegetation. Vast quantities of humic acid are forming constantly in swampy regions, especially in the tropics.

These substances include humic acid, geic acid, and ulmic acid. There is a close similarity between these substances and petroleum, as illustrated by the deposits of asphalt and other hydrocarbons formed of humic substances along the coast of Florida. The precipitation of such deposits might be caused by the mingling of fresh and salt water.



1.8.6 Transformation of Organic Material into Petroleum

Most investigators agree that organic material is the primary source of petroleum. Yet, the suggested mechanisms by which the material is transformed into petroleum runs the gamut of physical, chemical and geological speculation. The transformation of this matter to petroleum requires energy. In general, the proposed sources of energy fall under the following headings: (1) heat and pressure, (2) bacterial action, (3) radioactive bombardment, and (4) catalytic reactions.

There is a wide discrepancy between the temperature needed to transform organic matter into petroleum in the lab and the low temperature found in a natural environment. One explanation may be that time replaces temperature. That is, some reactions, if given a geologically long period of time, will occur at temperatures lower than those that are necessary in the laboratory. In other words, the reaction would occur at any temperature, but the lower the temperature the longer the time required.

Deep burial and consequent pressures may also play a part in the transformation of petroleum compounds. This is indicated by the changes in composition and gravity (viscosity) of oil which accompany changes in pressure and temperature. More specifically, these changes are: (1) changes in composition occurring with increasing depth of burial, and (2) changes in gravity and character as a result of regional metamorphism.

Bacteria are thought to function in several ways in aiding the final transformation of organic decay products into petroleum. Evidence to support this is derived in part from results in the laboratory and in part from its occurrence in nature. Laboratory experiments have shown that bacteria are able to produce hydrocarbons from organic matter. Although this has not been observed in nature, it is important that it can occur.

Some investigators feel that radioactive phenomena aid or cause the transformation of organic matter into petroleum. However, there is evidence to the contrary. Laboratory experiments indicate that hydrogen atoms are split off hydrocarbons by alpha radiation. This would cause, in geologic time, the formation of progressively heavier oils with a high ratio of carbon to hydrogen; whereas the change from organic matter to petroleum calls for a progressive increase in the ratio of hydrogen to carbon. For this reason, there is considerable doubt as to the value of radiation in the transformation of organic matter into petroleum.

It is believed that certain organic and inorganic substances which commonly occur in sea water may act as catalysts in the transformation of organic material into petroleum. Biochemically active bacteria and allied micro-organisms may be the principal catalyzers of chemical and physico-chemical reactions in recently



deposited sediments. It is known that microbial activity affects some of the properties of recent sediments, such as oxygen tension, oxidation-reduction potential, hydrogen-ion concentration, sulphide and sulphate content, carbonate content, and state of iron and manganese.

Certain metallic elements (such as lead, nickel, vanadium, iron, and copper) are commonly found in petroleum, apparently in some form of organic combination. Some of these elements may act as catalysts in the generation of petroleum.

Conditions

All available evidence suggests that organic materials might have been transformed into petroleum under the following conditions:

1. Deposition of organic material in fine sands and silts in fairly shallow marine water.

2. Rapid burial preventing destruction by bottom dwellers.3. Normal decomposition with burial and the beginning of anaerobic bacterial

activity.4. Conversion of material toward hydrocarbon material. The transformation

continues until the mixture becomes so foul by the accumulation of hydrogen sulfide gas that it kills off all bacteria.

5. Migration and accumulation of oil as sediments are compacted.

1.8.7 Migration and Accumulation of Petroleum

Because oil and gas ordinarily do not occur in commercial deposits in the same rocks in which they originated, migration from the source rock to the reservoir rock is assumed. Geologists believe that further migration takes place through the reservoir rock until the hydrocarbons either escape or are caught in some type of natural trap. There is little dissent to the concept of migration because of the extreme mobility of natural gas.

Migration

The movement or migration of petroleum from the source beds into reservoirs can be divided into two parts: (1) transverse migration from the source beds into a carrier bed; and (2) longitudinal migration through the carrier bed to a suitable trap. The movement of petroleum through rocks is apparently caused by several types of energy, including compaction, capillarity, differential specific gravity, hydrostatic pressure and gas pressure.



It is believed that compaction within the source beds is the principal force causing the movement of petroleum from source beds into carrier beds. Compaction is also regarded as an important force in the migration of petroleum through the carrier beds. Obviously the fluids occupying the pore space will be driven out by the compaction of the clay, mud or ooze of the source bed. These fluids move in the direction of least resistance into non-compacting porous formations, such as sandstone or porous limestone. Although direct proof that compaction has been an important factor is not to be expected, the direct association of most oil-producing regions with structural basins is an indication that it does play an important part.

Capillarity is action, due to surface tension, by which the surface of a liquid where in contact with a solid, is elevated or depressed. Surface tension of a liquid causes it to act as an elastic enveloping membrane, so that it tends to compact to the minimum area. The surface tension of water is approximately three times that of oil. Capillary action, therefore, would tend to draw water into the finest openings, displacing the oil and gas. In a slow transfer of liquids between shales and sandstone, oil would be displaced from the shales into the sandstones because the water enters fine pores three times as easily as oil and has three times as much difficulty in leaving.

Every oil field is evidence of migration caused by the action of gravity. If present, water occupies the lowest position in the reservoir. Oil floats on water and it occupies the next highest position above the water. Any gas present will occur above oil and will occupy the highest position in reservoirs. Other forces may cause petroleum to migrate great distances, but gravity is responsible for the final arrangement of water, oil, and gas in reservoirs.

The theory behind the action of hydraulic pressure in the migration of petroleum suggests that moving water under hydraulic pressure has been an important agent in the migration and accumulation of petroleum. According to this theory, hydrocarbons are carried along by the flow of underground water. However, the movement of petroleum through rocks is probably faster than the movement of water through rocks. Yet, it is conceivable that oil migration could be aided or hindered, depending on the direction of flow, by the movement of underground water.

Differential gas pressure has been suggested as a factor in the migration and accumulation of petroleum. However, it usually is considered only an aid to other factors, such as capillarity, differential specific gravity, or hydraulic movement.

Transverse Migration

Migration directions are considered in terms of the stratification planes of rocks. Oil either migrates in a longitudinal (parallel) or transverse (vertical) direction to the stratification planes. Generally, the primary migration from source rock to



reservoir rock is transverse, and the secondary migration through the reservoir to the trap is longitudinal.

Transverse migration can be downward or upward. If movement is taking place because of differences in the specific gravity of oil and water, the migration direction of oil will be upward. But if the oil is being squeezed from a rock by compaction it will move in a path of least resistance, whether that be upward, downward, or sideways. The prerequisite for transverse migration is that a receptive layer must be present to receive the flow.

Downward transverse migration is responsible for the occurrences of oil in basement igneous rocks of buried hills. Other examples of transverse migration are the accumulations of oil beneath unconformities, especially those occurring in the leached upper surfaces of thick limestones.

Longitudinal Migration

Longitudinal migration is possible where a porous and permeable rock layer occurs in the sedimentary section. Longitudinal migration is by no means confined to widespread sandstones or regional porous limestones. Sand-filled channels and bars in thick shale sections also may be used.

The confinement of oil accumulations to the highest levels in the reservoir rock is presumptive evidence that oil moved through the rock until those levels were attained. Unless it is assumed that by some strange coincidence oil entered the reservoir where there were traps, it must be concluded that the oil migrated laterally until trapped.

It can be concluded that petroleum has traveled by both longitudinal and transverse migration in moving from the source to the trap.

Accumulation

Many different classifications have been proposed to include the wide range of geologic conditions under which oil and gas pools occur. But because of the many different types of oil and gas pools, it has been difficult to establish a classification which covers all types. One generalization applies to all types; oil and gas accumulate in pools because their upward or lateral migration is stopped by a trap or closure. These traps are formed by stratigraphic conditions which were formed at the time of deposition of the sediments, by later changes in the sediments, by structural deformation, or by a combination of two or more of these factors.

The following is an outline classification of traps or reservoirs.



I. Closed Reservoirs

A. Reservoirs closed by local deformation of strata.

1. Reservoirs closed by folding

a. Reservoirs in closed anticlines and domes

b. Reservoirs in closed synclines and basins

2. Reservoirs developed through the off-setting of strata by faulting of homoclinal structures

3. Reservoirs defined by combinations of folding and faulting

4. Reservoirs formed through the cutting of strata by intrusions

a. Intrusions of salt

b. Intrusions of igneous rock

5. Reservoirs developed in fault and joint fissures and in crush zones.

B. Reservoirs closed because of varying porosity of rocks

1. Reservoirs in sandstone caused by lensing of sandstone or by varying porosity

2. Lensing porous zones in limestones and dolomites

3. Lensing porous zones in igneous and metamorphic rocks

4. Reservoirs in truncated and scaled strata

a. Closed by overlap of relatively impervious rock

b. Closed by seal of viscous hydrocarbons

C. Reservoirs closed by a combination of folding and varying porosity.

II. Open reservoirs

None of commercial importance

Figures 4-16 through 4-24 show the types of traps and where in the trap that oil and gas is likely to accumulate.

Note: In the following illustrations, the symbol at the right shows hydrocarbon accumulation.



Figure 1.16 Types of Oil Traps

Figure 1.17 Cross-Sections of Formation Structures: Fault Bend



Figure 1.18 Cross-Sections of Formation Structures: Fault Propagation

Figure 1.19 Cross-Sections of Formation Structures: Fault Drag



Figure 1.20 Cross-Sections of Formation Structures: Fault Drape

Figure 1.21 Cross-Sections of Formation Structures: Lift Off



Figure 1.22 Cross-Sections of Formation Structures: Chevron/Kink Band

Figure 1.23 Cross-Sections of Formation Structures: Diapir



Figure 1.24 Cross-Sections of Formation Structures: Differential Compaction

Figure 1.25 Cross-Sections of Formation Structures: Fold



Figure 1.26 Cross-Sections of Formation Structures: Fault

Figure 1.27 Cross-Sections of Formation Structures: Piercement



Figure 1.28 Cross-Sections of Formation Structures: Combination Fold/Fault

Figure 1.29 Cross-Sections of Formation Structures: Subunconformity



Figure 1.30 Cross-Sections of Formation Structures: Subunconformity

Figure 1.31 Simple Asymmetric Anticline with Two Oil-bearing Strata



Note the change in the dip of axis of fold (line GH). BC indicates the width of the productive area for the upper sand; EF that of the lower sand. Axes of folds (at A and D) lie near the left edge of the productive area. Well 1 is productive; well 2 only a short distance away, is barren. Well 4 produces from the upper sand only; and well 3 from both the upper and lower sands.

Figure 1.32 Asymmetric Anticlinal Fold Along the Flanks of a Major Uplift

Figure 1.33 illustrates how greater accumulations petroleum may be found on the basinward side of an anticline. Note the difference in the level of the edge-water lines on the opposite flanks of the anticline.

All anticlines are long narrow domes in the sense that they are closed structures. However, domes are usually spoken of as closed structures in which the length does not exceed three times the width.



Figure 1.33 Dome Structure, illustrated in plane view by the structure contours and by the vertical sections through the major and minor axes

Domes may be formed by intrusions of igneous rock or salt from below.

Figure 1.34 Typical Salt Dome Deposit

Oil accumulates in the porous formations above and on the flanks of the salt core. A monocline is formed when the crest of an anticlinal fold is eroded away and a partial cross section of the rock strata is exposed as an outcrop.



like r

at

Figure 1.35 Simple Monoclinal Structure

The shallow well, number 1, produces heavier, more viscous oil than number 2 owing to evaporation of the lighter constituents at the outcrop. Well 3 encounters edge water.

Oil that has migrated to the surface is lost; however, as it accumulates on the Earth’s surface, the lighter fractions evaporate leaving a residue of asphaltic-material. This residue will plug the pore spaces in the rock and prevent furtheloss. Such surface indications of a bituminous nature have resulted in the discovery of many important oil reservoirs.

Faulting will many times place a permeable strata against a shale strata. If conditions are favorable for petroleum accumulation, the oil would be trappedthe fault line. Faults may also allow migration of petroleum from stratum to stratum across fault lines where the permeable beds are adjacent.



Figure 1.36 Faulted Anticlinal Arch

This figure illustrates oil accumulation on both the upthrown and downthrown sides of a fault and show how faulting may leave barren places in an anticlinal structure. Wells 1, 3, and 4 are productive; whereas well 2 encounters edge water; and well 3 intersects the fault plane.

The sealing of tilted, eroded beds by deposition of new sediments form favorable traps for oil accumulation in the older rocks against an unconformity. In other cases, the oil might migrate across the unconformity and ultimately be trapped in beds not related to those in which the oil was originally stored.



Figure 1.37 Accumulation of Petroleum Against an Unconformity

The impervious stratum at the base of the upper series prevents the escape of the oil. Oil seeks out and accumulates in lenses of porous sands imbedded in dense less porous rock strata. Most sedimentary rocks are laid down at or near the shore line so the channels or lenses of sand would be roughly parallel to the shore lines of the period in which they were formed.

Figure 1.38 Accumulation of Petroleum in Sand Lenses



om l

ation n of

n of away e

Lenses of coarse sand embedded oil bearing shales serve as local centers of concentration. Such conditions are common in California fields. Well A encounters four zones of production; whereas well B is barren.

Figure 1.39 Accumulation of Petroleum in a Buried Coral Reef

Another important trap generally referred to as a “stratigraphic trap” occurs frirregularities in bedding and to some extent on structural conditions. A lateravariation of porosity or a pinching out of a porous strata between two impermeable beds will provide favorable conditions for segregation and accumulation of petroleum.

In some regions porous coral limestone has been formed in relatively shallowwater and subsequently covered by impermeable strata. Gravitational segregof the oil, gas and water results in the oil and gas migrating to the upper portiothe reef. Local variations in porosity also determine the areas of accumulatiooil and gas. Sediments adjacent to and above coral reefs usually dip slightly from the reef due to differential compaction of sediments accumulating on thsloping surfaces.




Sample ExaminationIntroduction

hed

e ed as

ger’s rply,

ogic

Chapter 2 Sample Examination

2.1 Introduction

An accurate sample description is the basic function of geologic work - the foundation on which the entire structure of subsurface analysis rests. This manual has been assembled in an effort to furnish a convenient reference on standard stratigraphic procedures. Techniques of collecting, preparing, examining, and describing well cuttings and core samples are set forth.

At one time the primary responsibility of the surface data logger was to provide correlation for structural mapping, now it has become increasingly important for him to also provide stratigraphic data. The source, transporting medium, environment of deposition, and post-depositional history of the sediments all can be determined by sample examination. There are two elements are involved: (1) logging what is physically present in the samples, and (2) interpretation of the geologic history from the material in the samples.

A description can become so detailed as to obscure important characteristics of the samples; the surface data logger should learn to be selective and report only the important details. Sample analysis should be made carefully and attentively. The accuracy of a study is dependent upon the quality of the samples and the proficiency of the surface data logger. Careful initial examination and description of the samples will save time and prevent the necessity for re-examination. There will be times when it is impossible due to well conditions for the surface data logger to accomplish this the first time. It is more important that the samples be caught first.

There are two general methods of sample description and logging, the interpretive system and the percentage system. The interpretive log is preferable but its accuracy depends in some measure on the quality of the samples, and the surface data logger’s familiarity with the local stratigraphic section of the area. Slougcuttings must be disregarded, and only the lithology felt to be represent the interval drilled is to be logged. If several different rock types are present in thsample, all are assumed to be derived from the drilled interval, they are loggdiscrete beds, interbeds, intercalations, lenses, or nodules, rather than as percentages. The interpretation in this case is based on the surface data logknowledge of the area. On interpretive logs, lithologic contacts are drawn shaand the entire width of the log column is filled with the suitable lithology plot types. Two hazards in this form of logging are unexpected recurrence of litholtypes and wildcat wells where there are no lithologic histories available for comparison.


Sample ExaminationCollecting Cuttings Samples

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Experience and good training are essential for making a good interpretive log. Generally the surface data logger examining the samples is best qualified to recognize lithologic and formational contacts. Although formation contacts should be picked on the basis of sample data rather than on mechanical logs, the latter, as well as the drill rate, can also be useful in defining boundaries of specific lithologic units, and zones of interest.

In percentage logging, the surface data logger, after eliminating the obvious foreign matter and unquestionable sloughed cuttings, logs each rock type with the percentage of that rock type that is present in the sample. This system of logging may be used to advantage in areas where:

1. The details of the stratigraphy are unknown.

2. The samples are of very poor quality.

3. No mechanical logs are available.

4. The sampled interval contains many thin beds.

5. The stratigraphic sequence is interrupted by structural complications.

6. The person studying the samples is inexperienced or is not an experienced surface data logger.

The principal disadvantages of this system are that lithologic breaks do not show up sharply on the log, and the logging of each rock percentage often gives a confused picture of the “in place” rock formation.

2.2 Collecting Cuttings Samples

First and most important step in evaluating any formation drilled is the collecof the drilled cuttings. If this step is not done properly, then, even if all the following steps are perfect, the information obtained is totally worthless to thegeologist and petrophysical engineer. Drilled cuttings are physical, tangible piof rock. It took the forces of nature millions of years to lay them down, and it cthe oil companies much time and millions of dollars to recover them. And, in span of just a few minutes, we can either save these cuttings (and the informthey carry) or lose them forever. Aside from their immediate value, the cuttingcan be saved and re-evaluated in the future using techniques and knowledgehave yet to be discovered. But if the cuttings simply fall overboard, then theirinformation is gone. The knowledge they carry is also lost when they becomemixed with other cuttings and we no longer know the depth of origin. Good cuttings and mud sample collection requires an accurate lag (indication of orof depth), a means of collecting representative samples, and efficient use of available time.



2.2.1 Shaker Samples

Almost every rig has a shaker screen for separating the cuttings from the mud when they reach the surface. Most shaker screens are of the vibrating type, but the cylindrical rotating type may be used in hard rock areas. When a shaker screen is used, the mesh size should be small enough to separate small cuttings from the mud. There must be a board or box placed at the foot of the shaker screen with the most cuttings coming over to collect the cuttings. The samples taken here will result in a composite sample that is representative of the complete sample interval (i.e., 10 feet, 30 feet). Cuttings caught directly from the shaker screens only represent a spot check of a couple of inches, and therefore, miss most of the cuttings from the sample interval. The board or box should be cleaned after each sample is caught so there will not be mixing of the cuttings from different depth intervals. It is important that if all the lagged intervals have been circulated from the hole, that the board or box be cleaned just before any new formation is due at the surface.

2.2.2 Settling Box Samples

Although the shaker screen cuttings sample retrieval method is the one most often used, another means of collecting samples is the settling box. A settling box should be rigged up in such a way that part of the mud from the flowline is diverted into the box (through a two inch line for example). The mud flows through the settling box, over a removable slide gate in the opposite end of the box, and into the mud pit. The flow through the settling box reduces the velocity of the mud, which permits the cuttings to settle to the bottom of the box where they can be scooped out with a sample spoon. After collecting a sample, the slide gate is lifted and the remaining cuttings are scraped and flushed away to prepare the box to collect the sample from the next sample interval. Using a settling box ensures that a composite sample is collected for each sample interval. A settling box employs the sluice box effect, and it provides the surest means of collecting small cuttings and fine grained sand. The settling box is practically the only means of catching samples in lost circulation zones when the shakers are being bypassed. Setting up a settling box before hand assures that no samples will be missed in the event circulation is lost, and that there will be uniform sample catching throughout the hole.

Hints and Precautions

1. The discharge from the settling box should go into the shaker pit or sand trap. Ask the tool pusher.

2. A small stream of water into the settling box will help cuttings to settle in heavy, viscous muds. (Check with the tool pusher or mud engineer before adding such a stream of water.)



3. If the amount of cuttings coming across the shaker decreases rapidly, or the cuttings disappear altogether, this could mean that a fine grained sand has been encountered. If this happens, you should check the sand content of the mud.

4. This same problem could also mean that a salt section has been encountered. Check the chlorides of the mud, and watch for deterioration of the mud properties.

5. Check the desander and desilter discharges for the possible presence of sample material which has gone through the shaker screens. A periodic check from these sources will provide a basis for comparison.

2.2.3 Collecting the Cutting Samples

The Sperry-Sun Surface Logging Systems Log is plotted on the basis of a sample interval that is specified by the customer. Surface data loggers have numerous demands on their time, there are many tasks to be accomplished and many pieces of equipment to operate. A logger should learn to establish an efficient work routine that makes provisions for collecting this important information in the time available.

Usually, fast drilling occurs at shallow depths and, occasionally, at greater depths through drilling breaks. On jobs where it is the policy to circulate out drilling breaks, fast drilling during these breaks can be handled by carrying out the following procedure: (1) the top of the drilling break is circulated out to examine very carefully for oil or gas; (2) when drilling is resumed, only the drilling rate needs to be logged until the cuttings from new formation are up. (Frequently, the fast drilling is over by the time the cuttings from new formation are up and the logging engineer can concentrate on the samples.)

When logging on shallow, very fast holes, it is best to have two surface data logging engineers on the job for the first day or two until one man can handle the logging. For a few days this could mean sixteen hour work days for a two man crew, but it is easier doing it this way, than trying to log a fast hole in a new location by one’s self. In a situation where two engineers are on duty at one time, it is usually the best practice to have one of them catch and analyze the samples while the other collects the data and takes care of the data sheets and logs.

Samples should be caught at more frequent intervals in a potentially productive zone. And, once a zone is found to contain a hydrocarbon show, samples should be caught even more frequently. The relative data analysis can be determined quickly since the surface data logging engineer knows what to look for.

When logging on deep, very slow wells, it is a good policy to collect samples even more often than the customer requires if possible (i.e., if the customer request



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30-foot samples and the drill rate is 30 ft/hr, then catch 5- or 10-foot samples). There is no such thing as too much information.

Hints and Precautions

1. If a sample is missed for any reason, mark the sample bag and the data sheet that it was missed. A missed sample is better than a “faked” sample.

2. During a potentially productive zone, or a known productive zone; catch tsamples as often as possible. This can be accomplished by placing the samples in suitable containers, marked with the correct lag depth, and seaside until there is time to examine them carefully. It is better to be late winformation than to be on time with very little information concerning the interval.

2.2.4 Collecting “Wet” Samples

A “wet” sample is an unwashed cuttings sample taken for paleontological anpetrological examination in the oil company’s laboratories. It can be a tinned sample, or just a sample put straight into a fine mesh cloth bag, labelled, andout in the sun to dry before tying it up into bundles and bagging it up into labesacks.

Note: To avoid loosing a sample take care in pen selection. Do not use washink. A bag of samples with the label missing is useless.

Care should be taken to adequately fill the sample sacks. The operating comusually requests that the wet samples be placed into plastic bags before theyput into cloth bags. If this is done, be sure that the top of the plastic bag and top cloth bag are both tied in such a manner that the samples will not be prefrom the bag during shipment to the customers laboratory.

It is a good procedure to collect a sample of all mud additives and their MSDsheets and ship them with the first set of samples that are shipped to the custlaboratory. Many of these mud additives can affect the rocks and the informathat they contain.


Sample ExaminationWashing the Cuttings

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2.3 Washing the Cuttings

2.3.1 Washing Cuttings From Water-Based Muds

Washing and preparing the cuttings sample for examination is as important as the examination itself. The technique must be adapted to the area and the type of material being examined. In hard rock areas the cuttings are usually easy to clean. Most of the time washing is just a matter of hosing the sample in a mud cup with a jet of water to remove the film of drilling mud from the surface of the cuttings.

Washing the cuttings from areas of recent geological age (cuttings that are less compacted and consolidated) is, however, more difficult, and requires taking several precautions. The primary concern is that the clays and silts that are present are often soft and dispersible in water. Indeed, they are often of a consistency that will disperse and “make mud.” When cuttings of this type are washed there istendency for the wash water to dissolve the clay and wash it away. This shoutaken into account. The surface data logger should always keep in mind thatclay that is washed away is not foreign material, but it is a part of the sampleshould be logged accordingly. The sample should be washed no harder thannecessary to remove the drilling mud.

Cuttings from zones of lost circulation are intermixed with lost circulation material. This material can usually be floated out of the sample container by flooding it with water, leaving only the cuttings. This method, however, is sometimes very time consuming. A settling box for catching the sample is anexcellent solution to this problem since it flushes most of the lost circulation material away from the cuttings. It is important for the surface data logger to recognize the difference between any lost circulation material and true formacuttings.

2.3.2 Cleaning Samples From Oil-Based Muds

In the case of oil based muds, the cuttings are quite representative of the formbecause this type of mud decreases sloughing so there is little dispersion of shales. At the same time, however, cuttings contained in oil based muds posproblem with washing and handling. They cannot be washed in water alone.necessary to use a detergent on the cuttings to clean off the drilling mud thatinterferes with seeing the cuttings fragments for description.


Sample ExaminationWashing the Cuttings

Method One

Set up two containers, such as two 5-gallon buckets. One should contain a non-fluorescent solvent (preferably Varsol or naphtha). This should be used for the first washing to remove the outer coating of drilling mud from the cuttings. In the other container, mix a solution consisting of a commercially available detergent into 5 gallons of water. Wash the cuttings in the detergent solution to remove the solvent. After this they can be washed in water as usual. To make a good inspection for lithology and staining, the cuttings must then be broken or crushed.

Sometimes, cuttings that have been subjected to oil-based mud turn to paste if any attempt is made to wash them with water as described in method one. Methods two and three can overcome this problem.

Method Two

Wash the cuttings in only a non-fluorescent solvent, such as Varsol or naphtha. One means of accomplishing this with a minimum use and waster of solvent is to prepare 3 or 4 baths for processing the samples. A closed container (without an internal lip, as some cuttings may hang up at this point) is ideal since this allows shaking of the solvent/cuttings mixture. First, dump the fresh cuttings into the first container containing solvent. Secure the lid on the container and agitate by shaking for approximately 30 seconds. Remove the lid and pour the solvent into another container for use again on the next sample. Refill the container with fresh solvent and repeat the entire process. When the solvent remains clear after agitation, the sample is clean. Again, pour off the solvent for later use and empty the cuttings into the perforated basket in the Sperry-Sun spin-dryer. Remove the solvent from the cuttings by spinning the assembly under the wall mounted motor for 30 seconds. Remove the perforated basket from the spin-dryer and empty the cuttings into a dry sieve assembly. Vigorously shake the sieves side to side to force cuttings through the various screens.

Method Three

Wash the cuttings in the base fluid of the mud (i.e., with Petrofree use Ester). Then wash the cuttings as described above until clean.


Sample ExaminationProcessing the Samples

2.4 Processing the Samples

2.4.1 Sieve Processing

The cuttings from newer, less compacted and consolidated formations need to be handled differently than the cuttings from older more compacted and consolidated formations. The following methods deal with the different types of formations.

Compacted and Consolidated Formations

After the cuttings have been washed to remove the drilling mud, they should be washed through a 5-mm sieve to remove sloughed shale and then into a 20-mesh, an 80-mesh sieve, and then into the sieve receiver assembly. It is generally accepted that the drilled cuttings will pass through the 5-mm sieve and the material that does not pass through is cavings. The 5-mm catch should be monitored closely even though these fragments are generally not generated by the bit. First of all, the amount of fragments in the sieve can indicate changing downhole conditions. An increase in the volume of these fragments can mean the hole is becoming near balanced pressure wise and formation is popping into the wellbore; these pieces are generally curved or splintery. It can also indicate that a water sensitive formation has been encountered and it is swelling due to the mud filtrate and sloughing into the hole. A sudden decrease in the volume of the 5-mm sieve chips can indicate an easily dissolvable formation has been cut and the chips are being reduced to very fine particles. Changing volume can also indicate mud problems (i.e., water loss, pH) or drill string problems (keyseating, doglegs, etc.)

The 20-mesh screen, with its .85-mm openings, is very helpful in many ways also in addition to merely holding cuttings washed through the 5-mm sieve. Generally, it will retain grains of very coarse size (1.0 mm) and fragments. This is where the bulk of your sample will occur normally and it should therefore be used to its fullest capacity. As the cuttings are washed down through the sieve assembly the cuttings segregate according to their density on each of the different screens. This means the denser fragments will go to the bottom of the sieve while the less dense fragments remain near the top. Reservoir rocks, namely carbonates (limestone, dolomite) and sandstone are much denser than shale and will settle to the bottom of the fragment assemblage in the sieve. Therefore, to ensure seeing the potential reservoir material we need to look at the bottom of the pile. After scooping some of the cuttings onto the stainless sample tray, quickly invert the 20-mesh sieve on the counter top with a firm slam. This will dislodge the cutting and after removing the sieve, the bottom of the assembly is now on top. Scoop these cuttings onto the sample tray for later study.


Sample ExaminationProcessing the Samples

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The 80-mesh screen, with.177-mm openings, will retain most grains of the fine size (.125 mm to .250 mm) and smaller cuttings. An increase in volume here may indicate a softer formation (which should be reflected in the drill rate) since most of the cuttings are generally in the upper 20-mesh screen. The same process of inverting this sieve after some of its catch has been slid onto the sample tray is also recommended.

The sieve receiver is an essential component of the sieve set because it catches everything that goes through all the screens. Generally, we would be looking for very fine grain sand in this portion of the sample. Experience should show that if you expect sand, due to a drilling break, but do not see much in the upper sieves, the sieve receiver will hold what you are looking for. This will also be where “dissolved” cutting would be collected.

After the sieving, a small portion of the washed sample should be put onto onthe trays provided for microscopic inspection and then drained. A larger samshould be placed on another tray, then drained and dried before it is placed ilabeled envelope and boxed for the oil company laboratory analysis. The trayimmediate examination should contain only a single layer of cuttings. This is important when considering the relative percentages of the different materialcontained in the sample.

Uncompacted and Unconsolidated Formations

Due to the nature of uncompacted clays and unconsolidated sands, the drillinmud on these cuttings is normally removed in the sieve assembly. They shouwashed through the 5-mm sieve to removed any sloughed formation into a 18200-mesh sieve. It is important that the cuttings not be overwashed as much formation will be washed away also.

After removing the 5-mm sieve, place the 200-mesh sieve directly under a gestream of water and vigorously shake the sieve from side to side. Do not spracuttings as this will tend to wash away the formation along with the drilling mContinue this until the cuttings appear clean. Then tilt the sieve and gently apstream of water to the bottom of the sieve and wash the cuttings onto a samptray.

Next, place the thumb of one hand across the opening of the sample tray anda gentle stream of water directly onto the thumb, allowing the water to run intosample tray. Gently agitate the sample tray until mostly clean water is runningof the tray. Drain the tray and then examine the cuttings under the microscopusing this method, most of the sand grains will be in one corner of the tray. Doscoop or scrap the sample tray across the sieve to obtain a sample. Most of finer sediments will be left on the sieve and not in the tray.


Sample ExaminationLogging While Coring

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2.5 Logging While Coring

In general, because coring ROPs are slow, oil companies will require more frequent samples in the event that the whole core is not removed.

When coring is in progress, the cuttings (which will be smaller than normal) should be carefully examined just as in normal drilling. This will help locate cores in cases of incomplete core recovery. For instance, in a 10-foot section of cored hole only 5 feet of core is recovered. The question as to which 5 feet of the core was recovered: the top, middle or bottom needs to be answered. Matching of the cuttings samples, correlated as to depth, with the 5 feet of core can “place” thorigin of the 5-foot section within the 10-foot interval. Obviously, the core itseshould be the basis of the lithological description when it is available. For thisreason, a complete description of the cores, the footage cored and footages recovered should always be kept.

Particular effort should be put into making a good sample collection of cuttingbecause this is the only permanent proof to the oil company of what was actudrilled. The log and the bagged samples are a lasting reminder to the customour association with the job.

2.5.1 Sidewall Coring

Sidewall coring is a supplementary coring method used in zones where corerecovery by conventional methods is small or where cores were not obtainedthe drilling progressed. Sidewall coring is useful in paleontological work, becait is possible to obtain shale samples for micropaleo analysis at definite depth

The sidewall coring device, a Chronological Sample Taker (CST) tool, is loweinto the hole on a wireline cable and a sample of the formation is taken at thedesired depth. This is done by shooting a hollow “bullet” into the wall of the hand then pulling it out. Usually there are as many as thirty bullets per gun. Sitwo or more guns can be used, up to ninety cores can be obtained during onIf an electric log has been obtained, a spontaneous potential (SP) or gamma(GR) curve run in conjunction with the sample can position the sample by dirlog correlation.

Sidewall cores taken with CSTs are small (1 inch × 21/2 inches), and in some casethe recovered material consists largely of mud cake. Sidewall coring is usualunsuccessful in very hard rocks. Nevertheless, cores of this type provide a mof examining the rock in portions of the hole on which information may be extremely scanty. Sidewall cores are sometimes taken with the intention of evaluating the porosity, permeability, and saturation characteristics of the roc


Sample ExaminationSample Description

However, because compaction occurs as the bullet enters, the results are inevitably less reliable than those from a conventional core.

Examining the Core

After the core has been frozen with dry ice, a geological description can be performed. This is mainly the responsibility of the wellsite geologist, but the logging engineer is advised to make a description also to be included on the mud log and/or attached to the bottom of a supplemental log.

Gross characteristics such as dip, fractures, bedding irregularities, mottling, etc., should be noted first, along with the thickness of each bed measured to the nearest millimeter. A more detail description is made from examination under the microscope for lithological alterations and under ultraviolet light for evidence of oil fluorescence. No more of the core should be removed than is necessary for sample examination (approximately 1/16 inch).

2.6 Sample Description

2.6.1 Sample Quality and Examination Techniques

The quality of a mud log is a direct measure of the quality of the samples that were collected and prepared. Clean, good quality samples are exceptions rather than the rule. The surface data logger describing the samples must learn to make his interpretations from samples of widely varying quality. Cavings and other contaminants must be recognized and disregarded.

Several methods of examining samples are in use throughout the industry. Some surface data logger examine one sample at a time; others lay out the samples in compartmented trays so that a sequence of from five to ten samples may be examined at one time.

The following procedure is recommended: the samples are laid out in a stack of five-cell trays with the depths marked on the trays. The cuttings should just cover the bottoms of the trays. It is desirable to separate the obvious cavings by sieving the samples. Attention should generally be focused on the smaller cuttings with angular shapes and fresh appearance.

A standard practice is to scan 100 or more feet of samples, observing the lithologic changes. The samples can then be re-examined for more detailed study, the samples should be dry for porosity estimates, wet for all other properties. Wet



samples bring out rock characteristics that are not apparent in dry samples. Leave the samples covered by a thin film of water. After the cuttings have been logged, they are set aside to dry and then placed in dry sample envelopes.

The technique of scanning samples before logging them in detail has many advantages. In addition to helping the surface data logger pick tops and lithologic changes it may also aid him in determining the extent of porous and hydrocarbon bearing intervals. However, the principle advantage of this technique is that it provides the surface data logger the opportunity to observe and interpret depositional sequences. When sample intervals are laid out in sequence subtle changes in texture, mineralogy, color and facies often become apparent even before microscopic examination. Thus the surface data logger is alerted to look for these changes when making the detailed sample examination. This method of examining samples encourages surface data logger to observe and log lithologic rather than sample interval units. It is still important that the surface data logger do a complete and thorough description of each sample.

Textures in carbonate rocks can be clearly observed with the aid of wetting agents such as mineral oil, glycerine, clove oil, etc. A further improvement of this technique is the use of transmitted light as described below.

2.6.2 Use of Transmitted Light

Textural and structural details often become evident when light is transmitted through thin slivers of carbonate rock. This technique is particularly useful for the routine examination of drilled cuttings.

Cuttings selected for their thin, platy shape are etched lightly in dilute HCl, placed in a clear Pyrex spot plate, and then completely covered with a wetting agent. Light is then transmitted through the chips by the use of a substage mirror, or a small reflecting mirror placed directly on the stage and underneath the plate.

A mixture of water and glycerine is recommended as the wetting agent because (1) it evaporates slowly, and (2) chips may be washed clean with water after examination.

2.6.3 Abbreviations

Abbreviations should be used for all descriptions recorded on surface data logs. Appendix A contains a list of the recommended abbreviations from the SPWLA manual.



2.6.4 Order of Written Description

Written descriptions are required in a standardized order of description because of the following: (1) it reduces the chance of not recording all important properties, (2) increases the uniformity of description among surface data logger, and (3) saves time in obtaining information from descriptions.

The following order is used:

1. Rock type - followed by classification

2. Color

3. Texture - including grain size, roundness, and sorting

4. Cement and/or matrix materials

5. Fossils and accessories

6. Sedimentary structures

7. Porosity and oil shows

2.6.5 Rock Types

The recording of rock type consists of two fundamental parts: the basic rock name (e.g., dolomite, limestone, sandstone), and the proper compositional or textural classification term (e.g., lithic, oolitic grainstone).

2.6.6 Color

Color of rocks may be a mass effect of the colors of the component grains, or result from the color of the cement or matrix, or staining of these. Colors may occur in combinations and patterns, e.g., mottled, banded, spotted, variegated. It is recommended that colors be described on wet samples under ten-power magnification. If is important to use the same source of light all the time and to use constant magnification for all routine logging. General terms, such as dark grey and medium brown, generally suffice.

Ferruginous, carbonaceous, siliceous, and calcareous matter are the most important staining or coloring agents. From limonite or hematite come yellow, red, or brown shades. Gray to black color can result from the presence of carbonaceous or phosphatic material, iron sulfide, or manganese. Glauconite, ferrous iron, serpentine, chlorite, and apatite impart green coloring. Red or orange mottlings are derived from surface weathering or subsurface oxidation by the action of circulating waters.

Bit or pipe fragments in samples can rust and stain the samples. Drilling mud additives may also cause staining.



2.6.7 Texture

Texture is a function of the size, shape, and arrangement of the constituent elements of a rock.

2.6.8 Grain or Crystal Sizes

Size, grades and sorting of sediments are important characteristics. They have a bearing on the porosity and the permeability of the rocks and may be a reflection of the environment in which a sediment was deposited. Size classifications are to be based on a Wentworth scale. The surface data logger should not try to record size grades without reference to a standard comparator of mounted sieved sand grains. Other comparators are photomicrographs of thin sections showing both grain size and sorting. Both simple and useful is a photographic grid of half-millimeter squares which may be placed near the microscope.

2.6.9 Shape

Shape of grains has long been used to decode the history of a deposit of which the grains are a part. Shape involves both sphericity and roundness.

Sphericity refers to a comparison of the surface area of a sphere of the same volume as the grain, with the surface area of the grain itself. For practical purposes, distinction is usually made in large particles on the basis of axial ratios, and in grains by visual comparison with charts.

Roundness which refers to the sharpness of the edges and corners of a fragment, is an important characteristic that deserves careful attention in detailed logging. Five degrees of rounding are described as follows:

Angular edges and corners sharp, little or no evidence of wear.

Subangular faces untouched but edges and corners rounded.

Subrounded edges and corners rounded to smooth curves; areas of original faces reduced.

Rounded Original faces almost completely destroyed, but some comparatively flat faces may be present; all original edges and corners smoothed off to rather broad curves.

Well rounded no original faces, edges, or corners remain; entire surface consists of broad curves, flat areas are absent.



2.6.10 Sorting

Sorting is a measure of the size frequency distribution of grains in a sediment or rock. It involves shape, roundness, specific gravity, and mineral composition as well as size. A classification given by Payne (1942) that can be applied to these factors is:

Good: 90% in 1 or 2 size classes

Fair: 90% in 3 or 4 size classes

Poor: 90% in 5 or more size classes

More precise values may be determined by direct comparison with sorting comparators.

2.6.11 Cement and Matrix

Cement is a chemical precipitate deposited around the grains and in the pore spaces of a sediment as aggregates of crystals or as growths on grains of the same composition. Matrix consists of small individual grains that fill the pore spaces between the larger grains. Cement is deposited chemically and matrix mechanically.

The order of precipitation of cement depends on the type of solution, number of ions in solution and the general geochemical environment. Several different cements, or generations of cement, may occur in a given rock, separately or overgrown on or replacing one another. Chemical cement is uncommon in sandstone which has a clay matrix. The most common cementing materials are silica and calcite.

Silica cement is common in nearly all quartz sandstones. This cement generally occurs as secondary crystal overgrowths deposited in optical continuity with detrital quartz grains. Opal, chalcedony, and chert are other forms of siliceous cement. Dolomite and calcite are deposited as crystals in the pore spaces and as aggregates in the voids. Dolomite and calcite may be indigenous to the sandstone, the sands having been a mixture of quartz and dolomite or calcite grains, or the carbonate may have been precipitated as a coating around the sand grains before they were lithified. Calcite in the form of clear spar may be present as vug, or other void filling in carbonate rocks. Anhydrite and gypsum cements, are more commonly associated with dolomite and silica than with calcite. Additional cementing materials, usually of minor importance, include pyrite, generally as small crystals, siderite, hematite, limonite, zeolites, and phosphatic material.

Silt acts as a matrix, hastening cementation by filling the pore spaces, thus decreasing the size of interstitial spaces. Clay is a common matrix material, which



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may cause loss of porosity either by compaction, or by swelling when water is introduced into the formation. Argillaceous material can be evenly distributed in siliciclastic or carbonate rocks, or have laminated, lenticular detrital or nodular form.

Compaction and the presence of varying amounts of secondary quartz, secondary carbonate, and interstitial clay are the main factors affecting pore space in siliciclastic rocks. While there is a general reduction of porosity with depth due to secondary cementation and compaction, ranges of porosity vary considerably due primarily to extreme variations in amounts of secondary cement. For instance, coarse-grained sandstones have greater permeability than finer ones when the same amount of cementing material is available to both. However, the same thickness of cement will form around the grains regardless of their size, therefore the smaller pore spaces, which occur in finer grained sandstones, will be cemented earliest.

2.6.12 Fossils and Accessories

Microfossils and some small macrofossils, or even fragments of fossils, are used for correlation and may also be environment indicators. For aiding in correlation, anyone making mud logs should familiarize himself with at least a few diagnostic fossils. The worldwide Cretaceous foraminiferal marker, Globotruncana, for example, should be in every surface data logger’s geologic “vocabulary.” Anysurface data logger who examines samples should be able to distinguish sucforms as foraminifera, ostracods, chara, bryozoa, corals, algae, crinoids, brachiopods, pelecypods, and gastropods so as to record their presence andrelative abundance in the samples being examined. More detailed identificatwill probably have to be made by a paleontologist. Fossils may aid the surfacdata logger in judging what part of the cuttings is in place and what part is caFor example, in the Gulf Coast region, fresh, shiny foraminifera, especially wbuff or white color, are usually confined to the Tertiary beds; their occurrencesamples from any depth below the top of the Cretaceous is an indication of tpresence of caved material. It would be helpful to each surface data logger toavailable one or more slides or photographs illustrating the principal microfoswhich might be expected to occur in each formation he will be logging. Eventhe surface data logger cannot recognize the various fossils, it is important thnotes them on the logs, noting also if there is an increase or decrease in the amount present in the samples.

Accessory constituents, although constituting only a minor percentage of a rocmay be significant indicators of environment of deposition, as well as clues tocorrelation. The most common accessories are glauconite, pyrite, feldspar, msiderite, carbonized plant remains, heavy minerals, chert, and sand-sized rocfragments.


Sample ExaminationSedimentary Structures

2.7 Sedimentary Structures

Most sedimentary structures are not discernible in cuttings. On the other hand, one or more of them can always be found in any core, and they should be reported in the description thereof. Structures involve the relationship of masses or aggregates of rock components. They are conditioned by time and space changes; e.g., stratification may result from discrete vertical (time) change in composition, as well as changes in grain sizes or of fabric. In time of origin, they are formed either contemporaneously with deposition (syngenetic), or after deposition and burial (epigenetic). Syngenetic structures are often very important indicators of the environments of deposition of sediments.

2.8 Porosity and Permeability

Among the most important observations made in the course of sample examination are those relating to porosity and permeability.

A number of classifications considering various aspects of carbonate porosity and permeability have been developed, including those by P. W. Choquette and L. C. Pray (1970) and by G. E. Archie (1952).

2.9 Hydrocarbon Shows

The recognition and evaluation of hydrocarbons present in well samples is another of the more important responsibilities of the surface data logger. He should be familiar with the various methods of testing for and detecting hydrocarbons, and should use them frequently in the course of routine sample examinations. Cuttings with good porosity should always be tested for hydrocarbons.


Sample ExaminationSome Criteria and Procedures For Rock and Mineral Identification

nd,

2.10 Some Criteria and Procedures For Rock and Mineral Identification

2.10.1 Testing Methods

Tests with Dilute HCl (10%)

There are at least four types of observations to be made on the results of treatment with acid:

1. Degree of effervescence: limestone (calcite) reacts immediately and rapidly, dolomite slowly, unless in finely divided form (e.g., along a newly made scratch). While the effervescence test cannot yield the precision of chemical analysis or X-ray, it is generally adequate for routine examination. Unless the sample is clean, however, carbonate dust may give an immediate reaction that will stop quickly if the particle is dolomite. Impurities slow the reaction, but these can be detected in residues. Oil-stained limestones are often mistaken for dolomites because the oil coating the rock surface prevents acid from reacting immediately with CaCO3, and a delayed reaction occurs. The shape, porosity, and permeability will affect the degree of reaction because the greater the exposed surface, the more quickly will the reaction be completed.

2. Nature of residue: carbonate rocks may contain significant percentages of chert, anhydrite, sand, silt, or argillaceous materials that are not readily detected in the untreated rock fragments. Not all argillaceous material is dark colored, and unless an insoluble residue is obtained, light colored argillaceous material is generally missed. During the course of normal sample examination in carbonate sequences, determine the composition of the noncalcareous fraction by digesting one or more rock fragments in acid and estimate the percentage of insoluble residue. These residues may reveal the presence of significant accessory minerals that might otherwise be masked.

3. Oil reaction: if oil is present in a cutting, large bubbles will form on a fragment when it is immersed in dilute acid.

4. Etching: etching a carbonate rock surface with acid yields valuable information concerning the texture, grain size, distribution and nature of noncarbonate minerals, and other lithologic features of the rock.

Etching is accomplished by sawing or grinding a flat surface on a specimen, which is then submerged for a short time (10 to 30 seconds) in dilute acid with the flat surface parallel to the surface of the acid. After etching the surface is carefully washed by gentle immersion in water, care being taken not to disturb the insoluble material adhering to the surface of the specimen. Limestone specimens etched in HCl usually develop and “acid polish.” Insoluble materials such as clay, silt, sa



chert, or anhydrite will stand out in relief against the soluble matrix. Dolomite crystals usually stand out also, inasmuch as they are attacked by the acid more slowly than is calcite. The internal structures of fossils, oolites, and detrital fragments are commonly revealed on an etched surface. If the appearance of the etched surface is so diagnostic that permanent record is desired, an acetate peel can be made, or the surface can be photographed.

Hardness

Scratching the rock fragment surface is often an adequate way of distinguishing different lithic types. Silicates and silicified materials, for example, cannot be scratched, but instead will take a streak of metal from the point of a probe. Limestone and dolomite can be scratched readily, gypsum and anhydrite will be grooved, as will shale or bentonite. Weathered chert is often soft enough to be readily scratched, and its lack of reaction with acid will distinguish it from carbonates. Caution must be used with this test in determining whether the scratched material is actually the framework constituent or the cementing or matrix constituent. For example, silts will often scratch or groove, but examination under high magnification will usually show that the quartz grains have been pushed aside and are unscratched, and the groove was made in the softer matrix material.

Parting

Shaly parting, although not a test, is an important rock character. The surface data logger should always distinguish between shale, which exhibits parting or fissility and mudstone, which yields fragments which do not have parallel plane faces.

Slaking and Swelling

Marked slaking and swelling in water is characteristic of montmorillonites (a major constituent of bentonites) and distinguishes them from kaolins and illites.

Thin Sections

Certain features of rocks may not be distinguishable even under the most favorable conditions without the aid of thin sections. Thin sections adequate for routine examination can be prepared without the use of the refined techniques necessary to produce slides suitable for petrographic study.

Some of the questions of interpretation which might be clarified by the use of thin sections include the following: mineral identification, grain-distribution, grain



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are

s of een

and , and o ing, alcite ion.

d, ck le

g d ite.

ate

sizes, source rock quality. Although wetting the surface of a carbonate rock with water, or mineral oil, permits “in depth” observation of the rock, some particlesparticle-matrix relationships still remain obscure until the rock is examined bytransmitted light, plane and/or polarized. Once these features have been recognized in thin sections, they are frequently detectable in whole fragmentsonly a few thin sections may be needed in the course of logging a particular interval. It is important to have polarizing equipment available for use in thin section examination - many features of the rock texture, and some minerals,most readily recognized by the use of polarized light.

Staining Technique for Carbonate Rocks

The distinction between calcite and dolomite is often quite important in studiecarbonate rocks. For many years several organic and inorganic stains have bused for this purpose, but with varying degrees of success.

One stain that is applicable to routine sample examination and is both simplerapid, is Alizarin Red S. This stain can be used on any type of rock specimenit has proved especially useful in the examination of cuttings. The reactions tacid of chips of dolomitic limestone or calcareous dolomite are often misleadand the rapid examination of etched chips does not always clearly show the cand dolomite relationships. Alizarin Red S shows clearly the mineral distributCalcite takes on a deep red color; other minerals are uncolored.

Insoluble Residues

Carbonate rocks may contain significant percentages of chert, anhydrite, sansilt, or argillaceous materials that are not readily detected in the untreated rofragments. The study of cherts and associated residues has been a commonpractice for many years in certain areas. For routine logging of micro-insolubresidues, symbols for accessory minerals, should be used.

Versenate Analysis

Versenate analysis is a relatively fast and inexpensive method for determininquantitatively the calcite/dolomite ratios of given carbonate rocks. The methohas shown merit in the mapping of intimately associated limestone and dolomIt is based on the color reactions of a reagent on crushed and sieved carbonsamples.



Heavy Mineral Studies

Heavy mineral studies are used today primarily when a geologist is seeking information concerning the source areas and distribution patterns of siliciclastic sediments. Their use as a correlation tool is limited.

2.10.2 Test for Specific Rocks and Minerals

Many of the more perplexing problems of rock and mineral identification can be solved by use the thin sections. However, certain simple and rapid tests are discussed as follows.

Clay

Shales and clay occur in a broad spectrum of colors, mineral composition, and textures. Generally, their identification is done with ease; however, light colored clay is commonly mistaken for finely divided anhydrite. The two may be distinguished by a simple test.

Anhydrite will dissolve in hot dilute hydrochloric acid and, when cooled, will recrystallize out of solution as acicular needles. Clay remains insoluble in the hot dilute acid.

Chert

Recognition of the more common varieties of chert and siliceous carbonates generally is not a problem. Weathered chert, however, is often found to be soft enough to be readily scratched and mistaken for clay or carbonate. Lack of reaction with acid generally distinguishes this type of chert from carbonates. Clay and tripolitic chert may require petrographic techniques for differentiation. In thin sections under polarized light, chert commonly has a characteristic honey-brown color.

Evaporites

1. Anhydrite and gypsum are usually readily detected in cuttings. Anhydrite is more commonly associated with dolomites than with limestones, and is much more abundant in the subsurface than gypsum. At present, there appears to be little reason to distinguish anhydrite from gypsum in samples. Anhydrite is generally harder and has a pseudo-cubic cleavage; the cleavage flakes of



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gypsum have “swallow-tail” twins. Anhydrite can be readily recognized inthin sections by its pseudo-cubic cleavage, and under polarized light, by bright interference colors.

The dilute hydrochloric acid test is a valid and simple test for anhydrite orgypsum in cuttings. Place the cuttings in a watch glass and cover with acHeat on a hot plate to ±250oF (±120oC) and wait for the sample to start dissolving. If anhydrite or gypsum is present, acicular gypsum crystals wiform around the edge of the acid solution as it evaporates. If the sample contains much carbonate, a calcium chloride paste may form and obscuracicular gypsum crystals. Dilute the residue with water, extract and discathe solution and report the test.

A simple method of distinguishing finely divided anhydrite from silt is a scratch test. This can be done by two methods:

a Rub a glass rod on the residue in the bottom of a glass test plate and for a gritty sound.

b Place a drop of liquid containing the residue on a glass cover-slip, ancover it with another slip. Rub them together between the thumb and forefinger. Examine the slips under the microscope for scratch markslisten for a gritty sound.

2. Salts are rarely found at the surface and generally do not occur in well samples. Unless a salt-saturated or oil-base mud is used, salt fragmentscrystals dissolve before reaching the surface. The best criteria for detectisalt section are: (a) the occurrence of “salt hoppers” (molds of dissolved crystals in other rock fragments), (b) marked increase in salinity of the drilmud, (c) a sudden influx of abundant caved material in the samples, (d) asharp increase in the drilling penetration rate, and (e) mechanical log character, particularly the sonic, density, and caliper log. Cores are the mdirect method of determining whether salt is present, but they are not usucut in salt sections.

Salts are commonly associated with cyclical carbonate sections and masred bed sequences. In the former, they are usually thin bedded and often above anhydrite beds. Potassium-rich salts, the last phase of an evaporacycle, are characterized by their high response on gamma ray log curves

Phosphate

Place on the suspected mineral (either on the hand specimen or on an uncovthin section) a small crystal of pure white ammonium molybdate. Allow one otwo drops of dilute nitric acid to fall on the crystal. If the rock contains phosphthe crystal rapidly takes on a bright yellow color.


Sample ExaminationPorosity and Permeability

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e of

e of

Siderite

Siderite is usually readily distinguished by its characteristic brown color and slow rate of effervescence with dilute HCl. The mineral often occurs as buckshot-sized pellets. The presence of siderite or iron dolomite in the same rock with calcite may be difficult to recognize and the following stain procedure is recommended for use when such cases are suspected.

The polished face of the chip is immersed for 5 to 10 minutes in a hot, concentrated solution of caustic potash to which a little hydrogen peroxide is added at intervals during treatment. The surface is finally washed and dried in the air. Siderite is stained brown while ferrous dolomite (ankerite) takes a weaker stain and ordinary dolomite remains colorless; calcite is roughened but is not destroyed and chamosite retains it green color unless carbonate of iron is present. This method is equally applicable to powders.

Feldspar

The presence, quantity and type of feldspar constituents can be important in the study of reservoir parameters in some sandstones, particularly the coarse arkosic sands or “granite washes.” Staining techniques, operationally applicable to ralarge etched core (or surface) sample surfaces, allows a better estimation ofamount and distribution of feldspar grains. The use of sections to make theseestimates is expensive, and often difficult because of the small surfaces prov

Bituminous Rocks

Dark shales and carbonates may contain organic matter in the form of kerogbitumen. Carbonates and shales in which the presence of bituminous mattersuspected should be examined by thin section and pyrolysis-fluorometer metfor possible source rock qualities. Dark, bituminous shales have a characterichocolate brown streak which is very distinctive.

2.11 Porosity and Permeability

2.11.1 Detection and Types

The detection and evaluation of porosity and the inferred presence or absencpermeability in the course of rock examination is one of the most important responsibilities of the surface data logger. Porosity is a measure of the volum



the void space in the rock; permeability is a measure of the capacity of a rock for transmitting a fluid. Permeability is dependent on the effective porosity and the mean size of the individual pores; it has a direct bearing on the amount of fluid recoverable, whereas porosity determines the amount that is present. Generally the smaller the grain or crystal size, the lower the permeability.

The ability to estimate porosity accurately comes through practice and experience in examining samples. Although magnification of about 10X is frequently adequate to detect porosity, higher magnification is often necessary. Pores are easier to recognize in dry samples than in wet ones. Qualitative estimates of the pore size range and mean should be made for all porous intervals. Quantitative permeability measurements are not possible by microscopic examination, but qualitative indications often may be seen. The speed with which water is absorbed by a rock fragment is an indication of its relative permeability. Conversely, water will stand up in a bead on a completely impermeable fragment.

If porosity of any category is observed, it should be thoroughly described using the proper symbols to denote its relative quality. Additional comments about it should be made in the remarks column. Samples with porosity should always be checked for hydrocarbons regardless of whether or not staining is observed on the rock surface. High gravity oils may leave little or no visible staining on the rock. A chlorothene or other nontoxic solvent cut should dissolve any trapped hydrocarbons from the inner pores that have not been previously dissipated.

In siliciclastic rocks three types of porosity are common: intergranular, moldic and fracture. Intergranular is by far the most common type and the most readily seen in cuttings. Normally it is difficult to detect moldic or fracture porosity in cuttings. Moldic porosity, the result of leaching of soluble grains is often difficult to differentiate from plucked grains. The presence of fragments of coarsely crystalline vein calcite in cuttings is often the only indication of the occurrence of fractures.

Porosity in carbonate rocks is generally classified in one of the following categories: interparticle, intercrystal, vuggy, moldic and fracture. These broad categories can be further subdivided into such specific types as inter-oolitic, leached fossil, pel-moldic, etc. These have genetic significance and should be described in detail on the log. Interparticle porosity, the pore space between particles of the rock, and intercrystal, that between crystals, usually is not larger than the particles or crystals. Vuggy porosity, comprising pore space equal to or larger than the particles of the rock, commonly results from the leaching of particles, and may have the form of irregular shaped voids.

It is important to record the sizes of vugs, as well as their presence. Where vugs are as large as, or larger than, the cuttings, the only evidence of their presence may be the occurrence of crystals, either free, or cemented to a surface which is actually a portion of the wall of a vug. In this situation it may be impossible to differentiate vuggy from fracture porosity in carbonate rocks.



Two carbonate porosity classifications are listed below. One developed by Choquette and Pray emphasizes geologic or genetic interpretation. The other by Archie deals primarily with physical properties used for evaluating or exploiting the fluid content of a rock.

2.11.2 Choquette and Pray’s Carbonate Porosity Classification

This is one of the best and most widely used carbonate porosity classifications and was published in the AAPG Bulletin in February 1970. The authors recognize that carbonates are generally complex in their geometry and genesis, and their classification is designed to aid in geologic description and interpretation of pore systems and their carbonate host rocks.

Although fifteen basic pore types are listed. It should be emphasized that differentiation of all these pore types from cuttings is impossible. Generally, both interparticle and intercrystal porosity are recognizable in cuttings. Often moldic porosity is identifiable, but the larger the pores the more difficult it becomes to distinguish among moldic, vuggy, intraparticle, fenestral and shelter porosity. In logging samples it is best to consider these voids as vuggy porosity if the pore space is larger than the size of the supporting particles or larger than the cuttings.

It is recognized that in some instances more precise identification of pore type can be made. In these situations, if appropriate symbology is not provided in the legends, descriptive comments should be made in the remarks column of the log.

2.11.3 Archie's Classification of Porosity in Carbonate Rocks

This classification was published in the AAPG Bulletin in February 1952. The scheme emphasizes the features of the pore structure in carbonate rocks that control fluid flow and fluid distribution without regard to the rocks genetic or diagenetic history. Carbonates are described according to matrix texture, including size and fit of individual grains, crystals or particles and size and amount of visible pores.

A comparison between lithic descriptions and an Archie classification description are shown below.

1. Genetic or descriptive classification

Sample 1 - limestone, oolitic grainstone, fine grained, well sorted with interparticle porosity

Sample 2 - dolomite, finely crystalline, sucrosic, porous


Sample ExaminationHydrocarbons

f and ence

ence cases,

ve. that

w s and

2. Archie - III FB10

a III = sucrosic or granular texture

b F = fine grain size

c B = visible pores less than 0.125

d 10 = 10% porosity in B pores

e B size pores with 10% porosity + A size matrix pores with 7% = total 0 17%.

The Archie terminology defines both lithic rock types as having identical potential as reservoir rocks although the stratigraphic implications as to the origin of the rocks are entirely different.

Data emphasizing the petrophysical characteristics of carbonates derived from Archie’s classification can be included on sample logs in conjunction with lithologic descriptions.

2.12 Hydrocarbons

Although petrophysical analysis may give conclusive determination of the presence of commercial quantities of oil, it is the surface data logger’s responsibility to report and log all shows, and to see that good shows are evaluated. Positive indications of hydrocarbons in cuttings can be a decisive factor in the petrophysicist’s evaluation of a well.

Unfortunately, no specific criteria can be established as positive indications owhether or not a show represents a potentially productive interval. The color intensity of stain, fluorescence, cut, cut fluorescence and residual cut fluorescwill vary with the specific chemical, physical, and biologic properties of each hydrocarbon accumulation. The aging of the shows (highly volatile fractions dissipate quickly), and flushing by drilling fluids or in the course of sample washing, also tend to mask or eliminate evidence of hydrocarbons. The presor absence of obvious shows cannot always be taken as conclusive. In many the only suggestion of the presence of hydrocarbons may be a positive cut fluorescence. In other cases, only one or two of the other tests may be positiHence, when the presence of hydrocarbons is suspected, it is very importantall aspects be considered: the porosity and thickness of the interval, the petrophysical evaluation, and the quality of the hydrocarbon tests. Listed beloare some of the most common methods of testing for hydrocarbons in samplecores that should be used by the surface data logger during routine sample examination.



2.12.1 Routine Hydrocarbon Detection Methods

Odor

Odor may range from heavy, characteristic of low gravity oil, to light and penetrating, as for condensate. Some dry gases have no odor. Strength of odor depends on several factors, including the size of the sample. Describe as oil odor or condensate odor. Depending on the strength of odor detected, report as good, fair, or faint, in the remarks column. Faint odors may be detected more easily on a freshly broken surface or after confining the sample in a bottle for 15 to 20 minutes.

Staining and Bleeding

The amount by which cuttings and cores will be flushed on their way to the surface is largely a function of their permeability. In very permeable rock only very small amounts of oil are retained in the cuttings. Often bleeding oil and gas may be observed in cores, and sometimes in drill cuttings, from relatively tight formations.

The amount of oil staining on ditch cuttings and cores is primarily a function of the distribution of the porosity and the oil distribution within the pores. The color of the stain is related to oil gravity; heavy oil stains tend to be dark brown, while light oil stains tend to be colorless.

The color of the stain and bleeding oil should be reported. Ferruginous or other mineral stain may be recognized by lack of odor, fluorescence, or cut.

Reaction in Acid of Oil-Bearing Rock Fragments

Dilute HCl may be used to detect oil shows in cuttings, even in samples that have been stored for many years. This is effected by immersing a small fragment of the rock to be tested (approximately 1/2 to 2 mm in diameter) in dilute HCl. If oil is present in the rock, surface tension will cause large bubbles to form, either from air in the pore spaces or from CO2 generated by the reaction of the acid with carbonate cement or matrix. In the case of calcareous rock, the reaction forms lasting iridescent bubbles large enough to raise the rock fragment off the bottom of the container in which the acid is held, and sometimes even large enough to carry the fragment to the surface of the acid before the bubbles break and the fragment sinks, only to be buoyed up again by new bubbles. The resulting bobbing effect is quite diagnostic. The bubbles which form on the surface of a cutting fragment of similar size which contains no oil do not become large enough to float the fragment before they break away, and the fragment, therefore, remains



on the bottom. In the case of oil-bearing noncalcareous sandstone, large lasting bubbles form on the surface but may not float the fragment. The large bubbles result from the surface tension caused by the oil in the sample, which tends to form a tougher and more elastic bubble wall.

It should be pointed out that this test is very sensitive to the slightest amount of hydrocarbons, even such as found in carbonaceous shale; therefore, it is well to discount the importance of a positive test unless the bobbing effect is clearly evident or lasting iridescent bubbles are observed. The test is very useful, however, as a simple and rapid preliminary check for the presence of hydrocarbons. A positive oil-acid reaction alerts the observer to intervals worthy of more exhaustive testing.

Fluorescence

Examination of mud, drill cuttings and cores for hydrocarbon fluorescence under ultraviolet light often indicates oil in small amounts, or oil of light color which might not be detected by other means. All samples should be so examined. Color of fluorescence of crudes range from brown through green, gold, blue, yellow to white; in most instances, the heavier oils have darker fluorescence. Distribution may be even, spotted, or mottled, as for stain. The intensity range is bright dull, pale, and faint. Pinpoint fluorescence is associated with individual sand grains and may indicate condensate or gas. Mineral fluorescence, especially from shell fragments, may be mistaken for oil fluorescence, and is distinguished by adding a few drops of a solvent. Hydrocarbon fluorescence will appear to flow and diffuse in the solvent as the oil dissolves, whereas mineral fluorescence will remain undisturbed.

When using the Sperry-Sun API gravity chart to determine the API gravity from the fluorescence, it must be taken from the unwashed cuttings mixed with water. By washing the drilled cuttings, some of the oil is washed from the cuttings, resulting in a brighter and lighter color fluorescence than the actual formation. With sidewall cores and conventional cores this problem is not as pronounced.

Reagent Cut Tests

Oil-stained samples which are old may not fluoresce; this failure to fluoresce should not be taken as decisive evidence of lack of hydrocarbons. All samples suspected of containing hydrocarbons should be treated with a reagent. The most common reagents used by the surface data logger are chlorothene, petroleum ether, and acetone. These reagents are available at most drug stores and give satisfactory results. The use of ether gives a more delicate test for soluble hydrocarbons than chlorothene or acetone, however, the ether being used should be tested constantly, for the least presence of any hydrocarbon product will



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itive ich ce

ate ured

olor

contaminate the solvent and render it useless. Chlorothene is recommended for general use although it too may become contaminated after a long period of time. Acetone is a good solvent for heavy hydrocarbons but is not recommended for routine oil detection.

Caution: Carbon tetrachloride is a cumulative poison and should not be used for any type of hydrocarbon detection.

To test cuttings or cores, place a few chips in a white porcelain evaporating dish or spot plate and cover with reagent. The sample should be dried thoroughly at low temperature, otherwise water within the sample may prevent penetration by the reagents, thus obstructing decisive results. The hydrocarbon extracted by the reagent is called a “cut.” It is observed under normal light and should be descon the basis of the shade of the coloration, which will range from dark brownno visible tint. A faint “residual cut” is sometimes discernable only as an amber-colored ring left on the dish after complete evaporation of the reagentvery faint cut will leave a very faint ring, and a negative cut will leave no visibcolor. The shade of the cut depends upon the gravity of the crude, the lightescrudes giving the palest cut, therefore, the relative darkness should not be takan indication of the amount of hydrocarbon present. A complete range of cutcolors varies from colorless, pale straw, straw, dark straw, light amber, ambevery dark brown to dark brown opaque.

The most reliable test for hydrocarbons is the “cut fluorescence” or “wet cut” tIn this test the effect of the reagent on the sample is observed under ultraviolight, along with a sample of the pure solvent as control. The sample should thoroughly dried before applying the reagent. If hydrocarbons are present, fluorescent “streamers” will be emitted from the sample and the test is evaluaby the intensity and color of these streamers. Some shows will not give a noticeable streaming effect but will leave a fluorescent ring or residue in the after the reagent has evaporated. This is termed a “residual cut.”

It is recommended that the “cut fluorescence” test be made on all intervals inwhich there is even the slightest suspicion of the presence of hydrocarbons. Samples that may not give a positive cut or will not fluoresce may give a pos“cut fluorescence.” This is commonly true of the high gravity hydrocarbons whgive a bright yellow “cut fluorescence.” Distillates show little or no fluorescenor cut but commonly give positive “cut fluorescence,” although numerous extractions may be required before it is apparent.

Generally low gravity oils will not fluoresce but will cut a very dark brown andtheir “cut fluorescence” may range from milky white to dark orange. An alternmethod involves picking out a number of fragments and dropping them into aclear one or two ounce bottle. Petroleum ether, chlorothene, or acetone is poin until the bottle is about half full. It is then stoppered and shaken. Any oil present in the sample is thus extracted and will color the solvent. When the cof the cut is very light, it may be necessary to hold the bottle against a white



acity

ed.

background to detect it. If there is only a slight cut, it may come to rest as a colored cap or meniscus on the top surface of the solvent.

Caution: Proper ventilation is important when using petroleum ether as it may have a toxic effect in a confined space. In addition, petroleum ether and acetone are very inflammable and must be kept away from open flames.

Wettability

Failure of samples to wet, or their tendency to float on water when immersed, is often an indication of the presence of oil. Under the microscope, a light-colored stain which cannot be definitely identified as an oil stain may be tested by letting one or two drops of water fall on the surface of the stained rock fragment. In the presence of oil, the water will not soak into the cutting or flow off its surface, but will stand on it or roll off it as spherical beads. Dry spots may appear on the sample when the water is poured off. This, however, is not useful in powdered (air drilled) samples which, because of the particle size and surface tension effects, will not wet.

2.12.2 Other Hydrocarbon Detection Methods

Acetone-Water Test

If the presence of oil or condensate is suspected, and provided no carbonaceous or lignitic matter is present in the rock sample, the acetone-water test may be tried. The rock is powdered and placed in a test tube and acetone is added. After shaking it vigorously it is filtered into another test tube and an excess of water is added. When hydrocarbons are present, they form a milky white dispersion, inasmuch as they are insoluble in water, whereas acetone and water are completely miscible.

Hot-Water Test

Place 500 cc’s of fresh, unwashed cuttings in a tin or beaker which has a capof 1,000 cc’s. Pour in hot water with a temperature of at least 170oF (77oC) until it covers the sample to a depth of 1 cm. Observe the oil film thus formed underultraviolet light and record the amount of oil released using the scale illustrat



Figure 2.1 Determination of Oil Shows by the Hot Water Method

Iridescence

Iridescence may be associated with oil of any color or gravity, but it is more likely to be observable and significant for the lighter, more nearly colorless, oils where oil staining may be absent. Iridescence may be observed in the wet sample tray. Iridescence with oil coloration or staining may indicate the presence of light oil or condensate.

Pyrolysis Test

When well samples of kerogen-rich rock are pyrolyzed in a thick walled test tube placed over a propane torch, oily material may be generated and condensed as a brown residue around the walls of the tube. This simple technique may be used to identify source rocks capable of generating liquid oil. However, the pyrolysis technique cannot distinguish between oil source rocks and those sediments rich in humic matter (carbonaceous shales and coals) which are considered to be dominately sources for gas. This test is also not responsive to post mature source rocks. The artificial test-tube generating process is believed to be similar to that associated with natural time-temperature dependent processes accompanying rock burial in depositional basins.

Hydrocarbons in organic rich sediments may be determined semi-quantitatively with a Turner fluorometer. One hundred milligrams of rock is pyrolyzed as above and the resulting condensation is diluted with 3 milliliters of chlorothene. The fluorescence of the solution thus produced is recorded in fluorometer units. For a more



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ed to by

r the

or ould

ns

ns.

ons.

comprehensive discussion of pyrolysis and pyrolysis techniques, refer to R. L. Heacock and A. Hood (1970).

2.12.3 Solid Hydrocarbons and Dead Oil

There has been much confusion, inconsistency and misunderstanding about the usage and meanings of these two terms. They are not synonymous.

Solid hydrocarbons refers to hydrocarbons that are in a solid state at surface conditions, usually brittle, and often shiny and glossy in appearance. There are a wide variety of substances called solid hydrocarbons with variable chemical and physical properties. The most significant of these variations is that of maturity. Some solid hydrocarbons, like gilsonite, are immature or barely mature oils, while others like anthraxolite represent the carbonaceous residue left after hydrocarbons have been overheated and thermally cracked. Anthraxolite is considered a thermally dead oil. Gilsonite, on the other hand, is certainly not a dead oil. It is a substance from which high-quality gasoline, industrial fuel oils and an endless list of other products are produced.

The term “dead oil” has been used indiscriminately in the industry to describethat are either (1) solid, (2) nonproducible or (3) immobile. All of these definitioare deceptive and misleading. Some solid hydrocarbons are not dead oil. Macalled “non-producible oils” are now productive because of improved recovertechnology, and there are numerous examples of “immobile oil” at surface conditions that are fluid and mobile at depth. Other factors that have been usdistinguish them are extremely variable and have lacked general agreement industry. For example, whether or not positive indications of fluorescence, residual cut, and/or cut fluorescence are considered requirements, or whethephysical state of the oil is solid or tarry.

In view of the above it is recommended that usage of the term “dead oil” be applied only to thermally dead solid hydrocarbons that will not fluorescence, give a cut or cut fluorescence. Whenever the term is used, qualifying data shbe listed.

2.12.4 Generalizations

No “rules of thumb” can be used to relate the evidences of the presence of hydrocarbons to potential production. However, there are some generalizatiothat are worth noting.

1. Lack of visible stain is not conclusive proof of the absence of hydrocarbo(Gas, distillates and high gravity oils ordinarily will have no visible stain.)

2. Lack of fluorescence is not conclusive proof of the absence of hydrocarb


Sample ExaminationProblems in Interpreting Drill Cuttings

3. Bona fide hydrocarbon shows will usually give a positive cut fluorescence (wet cut). High gravity hydrocarbons will often give a positive cut fluorescence and/or residual cut, but will give negative results with all other hydrocarbon detection methods. (Minerals which fluorescence will not yield a cut.)

4. The oil acid reaction test will give positive results when oil is present, but it is very sensitive and may give positive results in the presence of insignificant amounts of hydrocarbons.

2.13 Problems in Interpreting Drill Cuttings

2.13.1 Contamination from Previously Penetrated Beds

Cavings

Cavings may often be recognized as material identical to what has already been seen from much higher in the hole. This spalling of previously penetrated rocks into the ascending mud stream is particularly pronounced after trips of the drill stem for bit changes, drill stem tests, coring operations or other rig activities. It is suppressed by good mud control, but most samples will contain caved material. (Soft shales, thinly bedded brittle shales, and bentonites cave readily and may be found in samples representing depths hundreds of feet below the normal stratigraphic position of those rocks.)

Owing to differences in the hardness of rocks, the type and condition of the bit, and the practice of the driller, one cannot set any hard and fast rule for the size of true cuttings. Caved fragments tend to be larger than fragments of rock from the bottom of the hole, and they are typically rounded by abrasion. Flaky shape, freshness of appearance, sharp edges and signs of grinding by the bit may be used as criteria for the recognition of fresh cuttings.

Recirculation

Recirculation chiefly refers to sand grains and microfossils from previously drilled rocks which re-enter the hole with the mud stream and contaminate the rising sample.



2.13.2 Other Contaminants

Lost Circulation Material

A large variety of substances may be introduced into the hole to combat lost circulation difficulties. These include such obviously foreign materials as feathers, leather, burlap sacking, or cotton seed hulls, as well as cellophane (which might be mistaken for selenite or muscovite), perlite, and coarse mica flakes which might be erroneously interpreted as formation cuttings. Most of these extraneous materials will float to the top of the sample tray when it is immersed in water, and so can be separated and discarded at once. Other substance may need more careful observation. Generally the sudden appearance of a flood of fresh-looking material, which occupies the greater part of a sample, is enough to put the sample logger on his guard. As a check, he can consult the well record for lost circulation troubles, and the kinds of materials introduced into the hole.

Cement

Cement fragments in cuttings are easily mistaken for sandy, silty, or chalky carbonate. However, most cements are of an unusual texture or color, frequently have a glazed surface, tend to turn yellow or brown when immersed in dilute HCl, and are usually full of fine black specks. The latter are sometimes magnetic, in which case the fragments of cement can be removed from the cuttings with the aid of a small magnet. If the identification of cement is questionable, the well record should be examined to determine where the casing was set or cement plugs were set.

Drilling Mud

In examining unwashed or poorly washed cuttings, it is often important to be able to recognize the drilling muds which were used. An inexperienced surface data logger may confuse drilling mud with soft clay, bentonite, or sometimes gypsum or a carbonate. Thorough washing and rinsing in a pan of water will generally remove most mud contamination. If necessary, lithic fragments can be broken open to see if the interior (fresh) differs from the surface (coated).

Oil-base and oil-emulsion muds coat the cuttings with oil, and care must be taken to distinguish such occurrences from formation oil. They are generally recognized because they coat all cuttings regardless of lithology, rather than being confined to one rock type. Such contamination can sometimes be removed by washing the samples with a detergent or with dilute HCl. Ligno-sulfate muds may present problems in samples used in palynological studies.



Oil Contamination, Pipe Dope, etc.

Foreign substances, such as pipe dope or grease, from the rig operations sometimes enter the mud stream. Most pipe dope and grease will normally appear in the cuttings after a trip out of and into the hole has been made. Usually these contaminations will disappear after one or two complete circulations are made.

Pipe Scale, Bit Shavings, and Casing Shavings

Scale shavings of metal may also contaminate the samples, but they can be readily removed with a small magnet. They are usually rusty and rarely present a logging problem. Bit shavings are shiny as opposed to pipe scale. Casing shaving will also be very shiny and the shape will usually be curved or spiral. The drilling foreman on location should be notified immediately when bit or casing shavings are found in a sample.

Miscellaneous Contaminants

Other lithic materials which may be present in cuttings samples and obscure their real nature, or might be logged as being in place, include rock fragments used as aggregate in casing shoes.

2.13.3 Miscellaneous Interpretation Problems

Rock Dust

If samples are not washed sufficiently, a fine dust composed of powdered rock or dried drilling mud may cover the chips with a tightly adhering coat. In such cases, care should be taken that a fresh surface of the rock is described. Wetting the samples will tend to remove this coating, but if the chips are saturated with oil, the powder may still adhere to the surface even after immersion in water, unless a wetting agent or ordinary household detergent is used. These comments are particularly applicable to limestone and dolomite where the powdered rock film tends to be in the form of crystals which may mask the true texture of the rock. In this case, the best procedure is to break a few chips and obtain fresh surfaces for description.



ith es

o s of nto

Powdering (Bit Spin and Percussion Chalkification)

Powdering is the pulverization of the cuttings by regrinding (failure of the mud to remove cuttings from below the bit), or by crushing between the drill pipe and the wall of the borehole. It can result in the disappearance of cuttings from some intervals, and the erroneous logging of chalky limestone where none exists.

Fusing

Shales drilled by a diamond bit may be burned and fused, resulting in the formation of dark gray or black hard fragments that resemble igneous rock.

Air-Gas Drilling Samples

Cuttings from wells drilled with air or gas instead of mud are usually made up of small chips and powder, which makes sample examination difficult. Often a sample screening of the cuttings to eliminate the powder will facilitate the sample study. When the cuttings are entirely of powder, little can be done beyond describing basic rock types and colors. When the cuttings are carbonates, the basic rock type will be difficult to determine because dolomite powder effervesces as readily as limestone powder.

Where well-indurated shale sections are air drilled, the samples can be cleaned conveniently by washing them with care on a 60- to 100-mesh screen. This cleaning procedure should be required, where feasible, as the dust coating on the particles will mask the true color, texture and even the basic lithology of the drilled section. When “mist” drilling is done, particles can become plastered wfine mud which is removable only by a washing process; simple screening donot suffice.

Spread

Spread is the separation of large from small cuttings by relative slippage (alscalled elutriation or differential settling) in the mud stream, so that the cuttinga rock drilled up into fine chips may overtake the cuttings of a rock drilled up icoarse chips during their journey up the borehole. This results in the wrong sequence of rock types or very mixed sample being recovered.


Sample ExaminationGeological Notes

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2.14 Geological Notes

2.14.1 Unconformities

Notation on a sample log of any data which suggest the presence of an unconformity is important, even though the evidence is inconclusive. Supporting evidence may be found in nearby wells. In cuttings, the following criteria may indicate the presence of an unconformity:

1. Concentrations of minerals, e.g., phosphate, pyrite, glauconite, calcite, manganese nodules.

2. Abrupt changes in mineral assemblages, fauna, lithologic character, or cementing material.

3. Iron oxide stains or manganese coatings.

4. Corrosion surfaces, as developed on conglomerates (e.g., blackened limestone pebbles).

5. Desert varnish, as polished surfaces on pebbles.

6. Basal conglomerate - generally more heterogeneous and weathered than other conglomerates.

7. Bone and tooth conglomerate - accumulated as a “lag zone” overlying anunconformity.

8. Siliceous shells with beekite rings - small, bluish grey to white doughnut-lrings occurring on siliceous shells below some unconformities.

9. Weathered chert - a definite indication of an unconformity, providing the chis residual and not reworked.

10. Asphaltic residues can be present at unconformities at which oil seeped othe surface. In the case of cherts, the oil or asphaltic residue may be in thresidual chert and not in the overlying reworked material.

11. Porous zones in limestone, caused by solution by ground water, may be evidence of unconformities, but porous zones can develop for considerabdistances below the surface. The porosity may not be in contact with the unconformity, but the erosional interval is the cause of it. Limestones thatunderlie unconformities should be more deeply leached than similar limestones which do not underlie conformities. Other porous zones may oat unconformities in various types of lithology because of the occurrence there of coarser material and the effects of weathering. An unconformity sestablished may be traced from well to well by recognition of the porous zones.

12. Caliche and vadose pisolites, may form in carbonate rocks exposed to suweathering.


Sample ExaminationGeological Notes

The presence of two or more associated criteria greatly increases the chances that an unconformity is present.

2.14.2 Environments

Environments of deposition may be interpreted from (1) geometry and distribution of depositional units, (2) sedimentary structures and lithologic associations, (3) fossil assemblages. Information from drill cuttings, excepting fossil assemblages, is often insufficient to allow interpretation of environments. When a number of control wells are available in a region and sedimentary units can be traced, it is often possible to interpret at least generalized environments on geometry and distribution of units, lithologic associations, and in some cases, electric log shapes. Sedimentary structures and fossils observed in slabbed cores are the principal physical basis for identifying specific sedimentary environments, and determining sediment genesis.

Environments are classified with respect to sea level: continental, coastal, marine; and on the basis of physiography: shelf, slope, basin. Clastic sediments are controlled by the source of transported materials and the currents which disperse them; therefore, it is necessary to distinguish between coastal and continental environments in order to differentiate sand bodies which were formed by different processes and so have very different shapes and characters. The physiographic distinction between shelf and basin is important to the understanding of sandstones which may have been deposited in submarine fans and canyons. Carbonate sediments are generally best understood in terms of physiography. Tabular units may be expected to be present on the shelf, and lenticular units, such as mounds or reefs, form at the loci of major changes in slope; e.g., the shelf margin. The constituents of carbonate sediments are usually generated locally and not derived from external sources as are those of siliciclastics, so they may be found to change character abruptly in response to inherited or constructed topographic features anywhere in shallow marine environments. The distinction between continental, coastal, and marine is of lesser importance; most genetic units in carbonates are marine, although the landward limits of carbonate deposits may be within the coastal realm. Carbonates formed under subaerial conditions in a continental environment may not be volumetrically important but they demand particular attention as indicators of periods of exposure and thus of the intensive diagenesis which may occur under such conditions.

Description and logging of drilled cuttings and cores is an essential step in providing data which will contribute to the interpretation of the environment of deposition and genesis of a sedimentary unit.

Environmental interpretation from cuttings is extremely difficult and more often than not is impossible. However, in certain exploration areas even gross designations of basin, shelf, or continental is useful information. More specific


Sample ExaminationEquipment, Special Techniques and Procedures

environmental interpretations can be very helpful in establishing local facies variations and sedimentologic sequences and should be recorded on the sample log along with qualifying data.

2.15 Equipment, Special Techniques and Procedures

2.15.1 Equipment and Supplies for Routine Sample Examination

The following is an alphabetical listing of the principal items needed for sample examination in a well equipped logging unit. This list is not intended to include all items needed for specialized stratigraphic studies.

1. Acid, hydrochloric; 10% or 20% solution

2. Alizarin Red S dye

3. Beakers (50 ml)

4. Bottles, dropper or wash. Use for acid, chlorothene, mineral oil, or glycerine

5. Brush (paint brush) for cleaning sample trays

6. Carborundum stone (paper or powder) or silicon carbide grit

7. Cement: Lakeside 70 plastic cement, or Canada balsam

8. Comparators for size, sorting, roundness, sphericity and percentage

9. Chlorothene

10. Ultraviolet box

11. Glycerine

12. Hot plate (electric)

13. Lamp for microscope, with frosted and blue filters

14. Magnet (pocket size)

15. Manual (standard sample logging manual)

16. Mineral oil (Nujol)

17. Microscope, binocular, with polarizing attachment desirable

18. Plate (glass)

19. Probes

20. Sieves (5 mm, 20 mm, 80 mm, 120 mm, and 200 mm)

21. Slides (glass, 1 inch × 3 inches or 1 inch × 2 inches)

22. Spot plates (porcelain)

23. Streak plate



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ta rtition m a

24. Trays, sample (metal)

25. Tweezers or forceps

26. Water (distilled)

27. Wetting agent (or household detergent) for wetting powdered or contaminated samples

Binocular Microscope

The lens magnification should range from approximately 9 to 50 diameters. Magnification should be great enough to reveal the essential structure and texture of the sample. It should be low enough to reduce eyestrain and to provide a sufficiently wide field of view for estimating percentages of the rock samples. A magnification of approximately 9 to 12 diameters is best for routine sample examination, and 27 to 50 diameters for more detailed study. To reduce eyestrain, microscopes should be kept clean, properly focused, and in good condition. Lenses should be cleaned with lens paper; facial tissue, or a very soft, clean cloth may be used if lens paper is not available. A polarizing attachment for thin section study is a desirable accessory. Microscopes should be kept lightly lubricated.

Light

Natural or artificial light may be used; however, samples are usually examined under artificial light produced by one of several types of lamps. A Nikon, Bausch & Lomb, Zeiss, or American Optical illuminator is recommended, but any lamp with a blue bulb or blue filter plate may be used. A lamp that produces a “rainbow” of colors should not be used as it will tend to mask or distort the trucolors of the sample and will cause eyestrain. Not only should sufficient lightapplied to the sample itself, but the work area around the microscope shouldwell illuminated to prevent excessive eyestrain. A gooseneck desk lamp withblue bulb produces an excellent light, if a conventional microscope lamp is navailable.

Sample Trays and Dishes

Several types of trays and dishes may be used for examining the sample undmicroscope. A small flat tray made from wood, tin or other durable material mbe used. Compartmented trays with partitions dividing the trays into five compartments are particularly useful. They are available commercially and usually made of black plastic varying in size from 81/4 inches by 4 inches to 83/8 inches by 27/8 inches. Samples are poured into the trays for the surface dalogger and the depth of the sample is recorded on the side, or an elevated paof each tray. This method enables the surface data logger to have cutting fro



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ore

large interval of the well poured into trays for study; in addition, it facilitates the picking of sample breaks, inasmuch as gradations and variations in lithology are often readily visible and may be recognized before the samples are subjected to detailed examination under the microscope.

Ultraviolet box

Surface data loggers should have access to an ultraviolet light box at all times while examining samples. All porous intervals should be thoroughly checked for hydrocarbons with this device.

Acid and Solvents

Acid is used at all times in the running of samples; a dilute hydrochloric acid of 10% or 20% is recommended.

Various chemical solvents can be used for testing for hydrocarbon shows. It is recommended that chlorothene be used for this purpose because of its nontoxic qualities. Ether can be used also but is less desirable.

2.15.2 Thin Sections from Drill Cuttings

Preparing thin sections of cuttings on an operational level is a relatively simple process. They may be prepared in the following manner:

Equipment

1. Hot plate

2. Glass slides

3. Lakeside #70 thermoplastic cement (broken to approximately 1/8 inch pieces)

4. Glass grinding plate, 1/4 inch × 10 inches × 10 inches, carborundum stone o#300 or #400 grit (fine) silicon carbide paper

5. Carborundum loose grain abrasive (#240, #400, #600 grit)

6. Tweezers

Procedure

1. Melt the cement on a glass slide on the hot plate and drop into it one or mcuttings.



2. Remove the slide from the hot plate and allow the cement to harden by cooling.

3. Wet the grinding surface and hone a flat surface on the chips. Keep the grinding surface thoroughly wet by either dipping the slide in a water pan or by sprinkling additional water on the surface. The glass plate and loose abrasive method, the wet stone or the carbide paper may be used to make the thin section.

4. Dry the slide and place it back on the hot plate.

5. Using tweezers or a probe, turn over the honed surface of the chip when the cement melts.

6. Remove the chip from the hot plate and press the chip (honed surface down) against the slide as the cement hardens.

7. Hone the chip down to the desired thinness on the glass plate, wet stone, or carbide paper (as in Step 3).

Caution: Take care in Step 7 not to grind away the mounted chip entirely. It is not necessary to achieve any critical thinness. All that is necessary is to make the rock reasonably transparent. Therefore, check frequently by examining under the microscope. With a new stone, and especially with silicon carbide paper, the small chips will grind down quickly.

This process is simple in practice, and reasonable proficiency can be achieved with very few attempts. Using a carborundum stone, the whole procedure takes less than 10 minutes; when using silicon carbide paper, even less time is required. Better quality sections result from using a glass plate with abrasives. Covering the finished section is unnecessary; simply wet the surface while examining.

2.15.3 Staining Techniques for Carbonate Rocks

Preparation of Alizarin Red S staining solution. The staining solution is prepared by dissolving 1 gram of Alizarin Red S in 998 ml of distilled water and 2 ml of concentrated hydrochloric acid.

Preparation of the Samples for Staining

1. The samples must be clean and dry before the stain is applied.

2. The stain boundaries are intensified by polishing the sample with 1,000 grit and on a felt lap with stannic oxide.



3. Samples containing a high density of pores less than 1/2 mm in diameter do not stain well because the solution soaks in, coating the walls of the pore with stain, and pore differentiation is difficult. This type of rock is best stained if impregnated with plastic first. In this case, the matrix is stained and the pore space is void of stain.

4. If the sample does take a good stain with the first application, repeat the procedure for sample preparation.

Procedure

1. Immerse the chips to be stained momentarily in acid, then briefly rinse in distilled water. (Dipping the chips, held in tweezers, in a spot dish depression filled with acid then one filled with distilled water is an effective way.)

2. Apply a drop of two of Alizarin Red S to the chip on a spot plate or impervious surface (or place the chip in the stain) for 45 seconds.

3. Remove the chip and wash off the excess staining solution with distilled water. Let stand until dry.

4. Examine the chip under the microscope. Calcite will stain red, dolomite and other minerals will not be stained.

Note: The stain will come off if mineral oil, clove oil, or glycerine is applied to the samples. It may be removed from samples or thin sections by scrubbing with warm water and mild soap.

The concentration of HCl in the staining solution is extremely critical. Variations of a few tenths of a percent will give different contrasts between stained and unstained areas. It is recommended that each time a new solution is mixed, it has exactly the same HCl concentration as the solution being replaced. 0.2% HCl gives a good contrast between stained and unstained areas.

2.15.4 Detailed Insoluble Residue Studies

The procedure used in making detailed insoluble-residue analysis is described below.

Preparation of the Samples

Materials used in the study of detailed insoluble residues may be obtained from well cuttings, sidewall cores, or core samples. When sidewall cores or core samples are used, a small chip should be taken at regular intervals. It is usually desirable to group these fragments into 5- or 10-foot intervals. The fragments should then be crushed and a cut made of the crushed material in order to obtain a



more representative sample. However, since well cuttings are generally the only source of material available, it is from them that most residues are prepared.

In the preparation of insoluble residues, a measured sample (approximately 10 grams by weight) is placed in a 200-ml beaker to which dilute (12% to 15%) HCl is added. The first application of acid should be done slowly, to prevent foaming and overflow caused by rapid effervescence. A few minutes after the initial application, additional acid may be added. After several hours of digestion, the samples should be washed once or twice to remove the spent acid, then a second application of acid should be made. If the sample has only a small percentage of carbonates, a single application of acid will suffice for total digestion. Evidence of incomplete digestion will be the presence in the samples of dolomite fragments with rough surfaces, dolomite rhombs, or rounded limestone fragments. Finally, the sample should be washed to remove all traces of acid and prevent scum and caking of the residues.

Examination and Description

The percentage of insoluble material remaining after acidization is determined by visual measurement and plotted on an insoluble-residue strip log.

Residues are examined under a binocular microscope at magnifications ranging from 9X to 50X. The observed material can be classed in one or more of the following groups: (1) cherts, (2) clastics, including argillaceous material, shale, silt, and sand, and (3) miscellaneous or accessories, which include minerals and siliceous fossils or, more frequently, fossomolds. The terminology used in describing these residues is based on morphology rather than genesis, as described by Ireland (1977).

Cherts are generally the most important constituent and are distinguished by their texture, color, and diaphaneity. The various textural types, which are frequently gradational from one to another are plotted in different colors. The cavities, oolites, and other structures of the cherts also serve to characterize them as being derived from a particular zone or formation. The clastic material, minerals, and fossils found in residues vary in quantity and importance, but are generally subsidiary to the chert.

The extensive use of insoluble residues involves expensive and time-consuming operations. Frequently it is more practical for the surface data logger to prepare on-the-spot residues during routine study of well cuttings. However, caution should be observed, for seldom is a single constituent diagnostic of a particular zone or formation. Instead, an association of types of residues, or the relative abundance of a particular type and its position in the section are more significant criteria.



2.15.5 Versenate Analysis

The versenate analysis is a relatively fast and inexpensive operational method to determine the exact calcite/dolomite ratio of a carbonate rock. The method is a color-reaction experiment which employs the use of a reagent and a crushed and sieved sample.

Pure dolomite samples are readily identifiable with 15% dilute HCl acid, but the quantitative interpretation of mixtures of calcite and dolomite in well cuttings based on their reaction with acid is subjective and therefore variable between individuals. The versenate method has shown merit when limestone-dolomite stratigraphic traps are under investigation.

Due to variations in the chemicals employed in the reagent solution, it is necessary to test known calcite/dolomite mixtures and to plot a reaction time versus calcite/dolomite ratio curve, since the pH of the buffer solution affects the reaction time.

Preparation of the reagent

A single reagent solution is prepared by mixing the proper volumes of three solutions: a solution of sodium ethylenediaminetetraacetate, a buffer solution, and an indicator solution. To prepare the ethylenediaminetetraacetic acid solution, dissolve 4.0 grams of disodium dihydrogen ethylenediaminetetraacetate dihydrate, Na2H2Y. 2H2O, in 750 ml of distilled water. To prepare the buffer solution, mix 6.75 grams of ammonium chloride and 57.0 ml of concentrated ammonium hydroxide and dilute to 100 ml with distilled water. The pH of this solution is just over 10. To prepare the indicator solution, dissolve 1.0 gram of eriochromeschwartz T (F241) in 100 ml of methyl alcohol. To prepare the final reagent solution, mix 50 ml of the sodium ethylenediaminetetraacetate solution, diluted with 50 ml of distilled water, 12.5 ml of the buffer solution and 0.25 ml of the indicator solution. To prepare the Aerosol solution, a commercial agent, dissolve 0.1 grams of Aerosol in 100 ml of distilled water.

Testing procedure

1. Crush the sample and collect the portion that passes through a 150-mesh sieve.

2. Place approximately 0.02 grams of the sample in a 10-ml beaker and wet the sample with one drop of Aerosol solution.

3. Place the beaker under a mixer with a glass stirring rod and start the mixing motor.

4. Add 3 ml of the reagent solution to the beaker and start a stopwatch when the solution comes in contact with the sample.



5. When the solution turns from blue to pink, stop the watch and record the time on the Versene Analysis data sheet in the Reaction Time column.

6. The calcite/dolomite ratio is obtained from the accompanying chart. Silica and argillaceous impurities of less than 30% have no effect on the reaction time, but the presence of +15% anhydrite decreases the reaction in both limestone and dolomite.

/ /Dolo Calc/Dolo Time

Table 2.1 % Calcite/Dolomite vs. Reaction Time Chart

Calc/Dolo Ratio

Time(sec)

Calc/Dolo Ratio

Time(sec)

Calc/Dolo Ratio

Time(sec)

100/0 29 57/43 54 32/68 100-106

99/1 30 56/44 55 31/69 107-110

95/5 31 55/45 56-57 30/70 111-114

90/10 32 54/46 58 29/71 115-119

89/11 33 53/47 59 28/72 120-124

87/13 34 52/48 60-61 27/73 125-131

84/16 35 51/49 62 26/74 132-137

80/20 36 50/50 63 25/75 138-146

79/21 37 49/51 64 24/75 147-156

77/23 38 48/52 65-66 23/77 157-168

76/24 39 47/53 67-68 22/78 169-182

75/25 40 46/54 69-70 21/79 183-198

72/28 41 45/55 71-72 20/80 199-218

70/30 42 44/56 73-74 19/81 219-237

69/31 43 43/57 75-76 18/82 238-258

68/32 44 42/58 77-78 17/83 259-285

67/33 45 41/59 79-80 16/84 286-318

66/34 46 40/60 81-82 15/85 319-355

64/36 47 39/61 83-85 14/86 356-402

63/37 48 38/62 86-88 13/87 403-462

62/38 49 37/63 89-90 12/88 463-537

61/39 50 36/64 91-92 11/89 538-630

60/40 51 35/65 93-96 10/90 631-703

59/41 52 34/66 97-99

58/42 53 33/67 100-103



ion

2.15.6 Limestone-Dolomite Differentiation Using Fairbanks Solution

Procedure

Drop a fragment of unknown rock into the Fairbanks solution and wait 30 seconds.

Result

If the rock turns purple, it is calcite or limestone. If the rock remains unchanged, it is dolomite.

Caution: Exercise close attention in applying this test to dolomite or calcareous shale.

2.15.7 Sperry-Sun Calcimeter

The following is the procedure for using the Sperry-Sun Calcimeter for the determination of alkaline earth carbonates such as calcium carbonate and dolomite.

Equipment

1. Plexiglass CO2 cell fitted with one of the following:• Marsh Instrument Co. Type 11 pressure gauge (0-15 psi)• Marsh Instrument Co. Type 28 pressure gauge (0-30 psi)• Rustrack Model 2162 pressure recorder (0-15 psi or 0-30 psi)

2. (Optional) Wrist-Action shaker or equivalent shaker capable of mild agitatwith the complete CO2 cell.

3. Analytical balance (o.1 mg precision for calibration) or a portable balance(10 mg precision for field use).

4. 10 ml graduated pipette and aspirator bulb or equivalent

5. Mortar and pestle

6. Glazed paper or equivalent

7. Vacuum grease or lubriseal

8. Graph paper

9. Small brush



rl” l. If a

acid

.2)

Reagents

1. Dilute Hydrochloric acid solution. Dilute the concentrated reagent grade HCl with distilled water (20% HCl by volume).

2. Calcium carbonate - reagent grade (laboratory standard).

Procedure

Construction of the calibration curve

1. Weigh exactly.20,.40,.60,.80, 1.0, and 1.2 grams of reagent grade CaCO3 onto six pieces of glazed paper.

2. Remove the top and acid cup from the CO2 cell.

3. Inspect the CO2 cell to ensure that it is clean and dry.

4. Slide the paper and sample to the bottom of the cell by holding the cell in a horizontal position. Raise the cell to vertical and dump the sample onto the cell bottom. Brush the paper with the small brush to remove traces of the sample.

5. Measure and pour 10 ml of 20% dilute HCl into the acid cup and lower it into the cell. Be careful not to spill the acid and get any of it on the bottom of the cup.

6. Be sure the cell O-ring seals and pressure connections are in good condition. Use a light coating of vacuum grease on the O-ring seals.

7. Tighten the cell cap being careful not to splash acid onto the sample.

8. Open the bleeder valve until a “0” pressure reading is obtained.

9. Close the bleeder valve tightly.

10. Tip the cell and allow the acid to run out of the cup onto the sample. “Swithe acid and sample gently. Keep the reactants in the lower part of the celmechanical shaker is available, agitate for 20 minutes. If not, swirl continuously by hand until a constant pressure is obtained. (Avoid getting into the pressure gauge.)

11. Plot the grams of CaCO3 versus pressure on regular graph paper. Figure 2



Figure 2.2 Sample Calcimeter Calibration



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te.

ure 0 rom

12. Compute the average slope of the calibration curve by obtaining from the curve two high pressure readings (P2 - P1) and corresponding weights (W2 - W1). Compute the slope using the following formula:

Slope =

Repeat the slope calculation for two low pressure readings and corresponding weights. Finally, using the two slopes just computed, compute the average slope using the following formula:

Average Slope =

13. The cell should be calibrated monthly.

Testing of drill cuttings

1. Dry the cuttings on a hot plate or under a heat lamp.

2. Grind the cuttings with the mortar and pestle to at least 200 mesh.

3. Sieve the cuttings through a 200-mesh sieve onto glazed paper.

4. Weigh 1.0 gram of grounded cuttings (if available) to the nearest 10 mg or better, depending on the type of balance available.

5. Follow Steps 2 through 11 in the above “Construction of the Calibration Curve” procedure.

6. For interpretation of the pressure readings, refer to Figure 2.3 and FigureThese figures are representative of the CaCO3, dolomite and combined CaCO3/dolomite pressure versus time graphs as they would appear on thpressure recorder model.

7. Pressure gauge models

Note: As soon as the cell is tipped to start the reaction, observe and recordrapidly rising pressure at its peak reading. Record this as the CaCO3 pressure. If dolomite is present there should be a slight pause, then asecond rise in pressure. Keeping in mind that the dolomite reaction isslow, swirl the cell and allow sufficient time for the reaction to compleThe reaction is assumed to be complete when the pressure stops increasing and remains constant (approximately 15-20 minutes). Thisfinal pressure value is the total CaCO3 plus dolomite pressure.

8. Pressure recorder models

Note: Allow sufficient time for the reaction to complete (i.e., when the pressstops increasing with time and remains constant, approximately 15-2minutes). Refer to Figure 2.3 for interpretation of the recorded data. FFigure 2.3, the first pressure peak is due to CaCO3 and the final pressure is the total CaCO3 plus dolomite pressure. The CaCO3 pressure peak is not as well defined for higher dolomite concentrations (for dolomite

P2 P1–

W2 W1–--------------------

Slope1 Slope2+

2----------------------------------------



concentrations approaching 100% the Figure 2.3 curve begins to look like the Figure 2.4 (b) dolomite curve). Take care in determining CaCO3 pressure when dolomite concentrations are high. Use the following formulas for calculating the CaCO3 and dolomite percentages.

% CaCO3 =

% dolomite =

Figure 2.3 CaCO3 and Dolomite Pressure Versus Time Graphs

Pressure reading in psi × 100

Sample weight × average slope

Sample weight × average slope

(Total pressure - CaCO3 pressure) × 100 × .92



Figure 2.4 Combined CaCO3/Dolomite Pressure Versus Time Graph

Troubleshooting

Leaks in the pressure system are probably the greatest source of potential trouble. Periodically inspect and replace if necessary, the CaCO3 cell, O-rings, and seals. On models with pressure recorders, also check the fittings and tubing CaCO3 cell to the recorder. A serious leak will show up during a test as a decay in pressure after the normal pressure build up from the CaCO3 reaction. To check for leaks, pressure the instrument up to 10 to 12 psi (use the CaCO3 and HCl reaction), and let the instrument stand at least one hour. Pressure should not decease unless leaks are present.

The second source of potential trouble is lack of agreement with the Calibration Curve or degrade performance. Tests conducted in the laboratory on the CaCo3 cell with the recorder indicated an overall accuracy of +/= 5% even with a portable balance (10 mg precision). If there are no leaks in the system, but performance is questionable with the following:

1. Check for a sticking pressure gauge or recorder malfunction, consult the Rustrack manual for the recorder.

2. Make sure the balance is clean and free of corrosion on the weighs and pan. Shield the balance from any air currents and vibrations as much as possible.

3. Check the CaCO3 cell for contaminants. Be sure the cell is clean and dry.

4. Check for impurities in the reagents. Moisture in the CaCO3 standard will introduce an error.



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2.15.8 Shale Factor

Shale factor is a technique for the determination of the clay content or “shalinof a sand/shale sample with a standard methylene blue dye. Plots of Shale Fmade at the well site during drilling are used to assist in pressure detection fobalanced pressure drilling. Also, Shale Factor logs have been used to locateformations which cause serve borehole instability.

Clays are sensitive indicators of environment and geologic history because trespond to slight changes in composition, temperature, and pH of the surrounthrough geologic time. Examples of this sensitivity are evident in the acousticelectrical log analysis wherein certain subsurface conditions such as formatiopressure can be inferred. The word infer should be qualified to mean that theinference is relative to each particular borehole and does not bear an absoluquantitative unit of measure.

The basis of Shale Factor is the assumption that the cation absorptive capacthe cutting is in itself a significant number and there is not the necessity of thhaving to correlate with any other measurements for arriving at a parameter.cation absorption has a direct relationship only to the type of clay and the perclay content.

An analytical technique has been developed for measuring the cation exchancapacity for as little as a fourth of a gram sample (often a single cutting). Themay be done rapidly, simply, and with expectation of reasonable accuracy fopurposes of optimizing the drilling process while in progress.

As do all cation exchange methods the methylene blue test measures the totexchange capacity of the sample system and is, therefore, dependent upon thand extent of clay minerals present. Only the reactive portion of the cuttings involved. Finely grounded minerals, such as ilmenite, limestone, or sand do absorb methylene blue. The test is somewhat unique in that a direct reading exchange capacity of the formation is obtained. This reading or Shale Factorresult is expressed as milliequivalents per hundred grams of sample.

The Shale Factor is interpreted to mean an equivalent amount of montmorillowhich is equivalent to the water holding capacity of the shale.

Clay plates have a tremendous water holding capacity, even after the free wahas been expelled by compaction, several molecular layers of bound water remain. It is the mechanism of the release of this bound water, associated wichanges in clay mineralogy, which gives the Shale Factor technique its' originThis release is a step in what is called diagenesis.

Water expelled from clay sediments smoothly and continuously with the increin burial depth, as the clay and the clay minerals are altered from montmorillotowards illite with time given the gradual releasing of the bound water for



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expulsion through a sufficient permeability pipeline and the time for this escaping to take place. In this case, the shales will become compacted and firm, and the pore pressure and matrix stress will be “normal.” Except for abrupt changes insand/shale lithology, a plot of Shale Factor versus depth in the ideal situationshow a continuous decline in montmorillonite with depth and the age of the formation.

It is the departure from the “normal” water squeezing with depth and time trethat gives Shale Factor it potential. Wherever completion of this phase of diagenesis has been slowed or interrupted for whatever reason and is not stioccurring, generally a higher than normal montmorillonite content is encounteand its corresponding higher than normal water content. This condition has itattendant drilling problems associated with the abnormal pore pressure or subnormal matrix stress. Rather than over-simplify the situation by alluding toimpermeable “seal” or “cap,” it seems more reasonable to picture this as a dynamic situation with diagenesis still occurring releasing new fluid but fastethan the fluid can escape. This fundamentally, makes the Shale Factor technan abnormal pressure detecting scheme. So, “abnormal” montmorillonite for given depth must first be present for abnormal water content to exist. Furtherprevent rapid leak-off, there must be an absence of permeable lithology whicalso verified by Shale Factor. (Other methods of pressure detection are all baon indirect measurements or secondary properties that occur as a result of thincomplete and presently occurring diagenesis; and these include increasingconductivity, decreasing resistivity, increasing sonic travel time, decreasing density, increasing drillability, increasing gas content, increasing temperaturegradient, and decreasing salinity. These are not independent and are alteredmasked by minor changes in lithology.)

This is not meant to imply the other parameters are not useful. However, ShaFactor has its greatest value in correctly interpreting this other data in the lighits more positive identification of clay mineralogy and shale versus sand litholoAlso, Shale Factor is one of the few properties of the formation or cuttings thanot altered by exposure to the drilling fluids.

Shale Factor logging experience indicates that there are few “pure shales” or“clean sands” in the formations that are drilled. There are instead sandy shalshaly sands, and it is next to impossible for even an experienced geologist osurface data logger to correctly identify cuttings as one or the other by lookingrains under the microscope. Attempts to correlate drilling breaks with litholoby calling a drilling break a sandier section can be wrong about half the time these drilling breaks also occur in wet shalier sections. Shale Factor providesmore precise number for this shaliness versus sandiness of a formation. A wclay might have a Shale Factor as high as 15 to 20, whereas a relatively cleasaltwater sand might have a Shale Factor as low as 5.



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Equipment

• Mortar and pedestal• Methylene blue solution (3.74 per 1000 cc)• Dilute sulfuric acid (approximately 5N)• Hydrogen peroxide (3% solution)• Distilled water • Erlenmeyer flask, 250 ml• 10-ml pipette• 1-ml pipette• glass stirring rod• hot plate• filter paper• 200-mesh sieve• small magnet• portable balance or scale

Procedure

1. Wash and screen sloughings from a shale sample from the shale shaker.

2. Place the shale samples on the hot plate and cook off all the water from tsample.

3. Grind the dry sample in the mortar and pedestal until it is a fine powder.

4. Run the magnet through the sample to remove any metal particles whichbe in the sample.

5. Sift, do not force, the sample through a 200-mesh sieve.

6. Measure 1 gram of sifted cuttings.

7. Add the 1 gram of sifted cuttings, 10 ml of distilled water, 15 ml hydrogenperoxide, and 0.5 ml of sulfuric acid to the Erlenmeyer flask.

8. Boil gently for 10 minutes.

9. Dilute the solution to about 50 ml with distilled water.

10. Add methylene blue solution to the flask in .5 ml applications. After each addition, swirl the contents of the flask for about 20 seconds, and while thsolids are still suspended, remove one drop of fluid with the glass stirringand place the drop on the filter paper. The end point of the titration is reacwhen the dye spreads as a greenish-blue ring or tint around the spot of dsolids.

11. When the blue ring or tint is detected around the spot, shake the flask anadditional 2 minutes and place another drop on the filter paper. If the blueis again evident, the end point has been reached. If the ring does not appcontinue as before until a drop taken after shaking for 2 minutes shows thblue tint.



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12. Report as follows:

Methylene blue used (ml) × 1.425 = Methylene blue capacity (FMBT)

2.15.9 Shale Density

The density gradient column is a partial mixture of two fluids in a graduated cylinder such that the density of the fluid varies smoothly from top to bottom.Calibration beads of various densities suspended in the mixture permit the usprepare a calibration graph of the density of the fluid with respect to column height. Thus, when a small shale sample is dropped into the column it comesrest at the level corresponding to its density. A density reading in grams per ccentimeter is then determined from the calibration graph of column height vedensity. These readings are used to plot a shale density log.

The density gradient column is used to measure the relative density of varioushales being drilled as represented by bottom hole cuttings. The values are incorporated into the main computer, and thus into the database computer bsurface data logger and used to plot a shale density log. Since shale compaca function of pressure, this log indicates bottom hole pressure during drilling operations. Because this method is independent of drill rate it serves as an especially important tool in predicting abnormally pressured zones.

Equipment

• Sodium polytungstate (density 2.89 g/cc)• Distilled water• 350 ml graduated cylinder with stopper• Calibration beads

2.14 g/cc white cylinder2.22 g/cc clear bead2.27 g/cc pale yellow bead2.34 g/cc gray bead2.41 g/cc gray/clear bead2.47 g/cc blue bead2.56 g/cc maroon bead2.70 g/cc black/maroon bead2.85 g/cc black beadlow range calibration beads (optional)1.80 g/cc green bead1.90 g/cc orange bead2.00 g/cc bright yellow bead

• cleaning basket• stirring rod



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• graph paper (10 × 10 divisions per inch)• wall mounting bracket containing a light source

Gradient Column Set Up

1. Pour 200 ml of sodium polytungstate, the heavy solution, into the graduacylinder.

2. Add the distilled water very slowly, decanting it onto the inside wall of thecylinder, until a total volume of approximately 330 ml is reached.

3. Slowly lower the cleaning basket, containing the beads, until the sample retriever rests on the bottom of the cylinder. (Drop in the beads if the cleabasket is already in the cylinder.)

4. Slowly lower the stirring rod to a point about two inches below the beads. the rod quickly about three inches. Wait for the beads to stop moving.

5. Slowly lower the rod to a point no closer than three inches to the bottom ocylinder. Lift the rod quickly to a point no closer than two inches from the tWait for the beads to stop moving.

6. If the beads span less than three 20 ml graduations, mix again in the abofashion.

Note: Use only upward strokes to mix. Always wait for the beads to settle between strokes. Never mix the top and bottom ends of the column

It is very easy to mix too much rather than too little. Be sure not to mithe bottom three inches or the top two inches of the column with the stirring rod. Be patient. Time is very effective at smoothing out an initially uneven density gradient.

7. Add the extended low range beads now if desired.

8. Slowly add distilled water, decanting it against the cylinder wall as beforereach a total of 350 ml.

Column Calibration

1. Prepare a piece of graph paper with 10 × 10 divisions per inch for use ascalibration graph.

a If using the regular set of calibration beads, along the long edge of thpaper mark out a suitable span of 100 ml of column height, using a sof one inch per 10 milliliters. Start with the 10 ml division below the lowest bead at the left margin of the graph.

b Along the width of the paper graph 2.15 - 2.85 g/cc, using a scale of inch per 0.1 g/cc. See Figure 2.5.



c If using the extended set of beads, prepare the graph paper as shown in Figure 2.5. Along the side, mark off 1.6 - 3.0 g/cc using a scale of one inch per 0.2 g/cc. Along the bottom edge mark from 20 to 340 ml as shown in Figure 2.6, using a scale of one inch per 40 milliliters.

2. Draw guidelines, if desired, opposite the density of each bead to be used. This will aid in quick plotting of the calibration graph. See Figure 2.5.

a Draw the guidelines for the lighter beads along the left margin.

b Draw the guidelines for the heavier beads along the right margin.

c The densities of the calibration beads are given on the envelope in which they are contained. They may vary slightly from those given in Section 6.20.2.

Figure 2.5 Graph Paper Prepared for Plotting Calibration Curve



th

ror in

d

e.

Figure 2.6 Sample Plotted Calibration Curve

3. Plot the height of each bead in column milliliters using the markings on the cylinder.

a Read the height of the middle of the bead.

b Read the height with your eye at the same height as the bead to avoid parallax error.

c Plot the graph in pencil so that you can replot the same graph as the column shifts.

d Plot each point as a dot and circle it. “X” out any point improperly plotted. See Figure 2.6.

4. Draw a smooth curve through the points.

a This curve need not be a straight line; it should, however, be a smoocurve.

b Your shale densities will be more accurate if you draw a smooth line instead of just connecting the points. This is because there is some erthe density of the calibration beads.

c Typically the line should flatten out at one or both ends and be fairly straight throughout the middle section.

5. If the points do not make a suitable curve, slowly insert the stirring rod anmake one or two strokes upward through the uneven areas.

a Remember the curve will become smoother and more stable with timTry to leave it alone.



b Remember the beads will usually not move upward and they will usually not move closer together.

c If a single bead is too high a short stroke downward, beginning above the bead and pushing down on it, will cause it to move downward in the column.

Gradient Column Clean Up

1. Pour 30 ml of solvent in the cylinder. Chlorothene is an effective solution for rinsing the graduated cylinder, calibration beads, and rods.

2. Lower and rinse the sample retriever with the beads.

3. Rinse the stirring rod.

4. Swab the cylinder with a paper towel, being careful not to scratch the graduated cylinder.

Gradient Column Maintenance

1. Replot the calibration graph whenever there have been noticeable changes in the positions of the beads. It is a good practice to replot the calibration graph every two days during continuous drilling.

a Erase the penciled curve and plotted points, and reuse the same prepared graph paper.

b Do not plot beads resting at the bottom or floating at the top of the gradient mixture.

c Write the date and time on the new plot each time one is made.

2. Remove the accumulated shale every two days of normal drilling, or whenever the equivalent amount of shale samples have accumulated. This prevents the premature contamination of the column by the absorption of the water contained in the shale.

a Lift the cleaning basket very slowly. Plan to take almost a minute to lift the basket from the bottom to the top of the column.

b Remove the shale and beads, clean the beads, and replace the beads in the cleaning basket.

c Just as slowly, lower the basket back to the bottom of the column.

d Replot the calibration curve.



Mixing a New Column

When to mix a new column is up to the discretion of the surface data logger. Generally the stability of an old column must be balanced with the ease of reading a new column. The following conditions are indications that a new column might be needed:

1. The shale densities, for any reason, can no longer be discerned.

2. The beads no longer form a smooth curve.

3. The column is too dirty or too discolored to be useful.

4. There are more than two beads on the bottom.

5. There are more than three beads on the top.

Beads on the top or bottom of the column cannot be graphed. And, if shale floats or sinks, its density cannot be measured in the gradient column. The areas above the highest suspended bead and below the lowest suspended bead cannot be used.

Remember that a new column is not stable so you should plan ahead. Mix a new column when first arriving on the site, before it is needed, and if it is necessary to replace an old column, plan to do it, whenever possible, while the bit is off bottom for at least a few hours.

Technical Tricks

1. Avoid unnecessary exposure of the column to ultraviolet radiation and vibration. Keep the column out of the sun and cushion it from vibrating machinery. In the logging unit, if light is a problem, shape a cardboard tube from a paper towel roll so that you can put it around the graduated cylinder when it is not in use.

2. Avoid inferior quality cuttings such as so-called gumbo shale. Not only will these give unreliable readings, but they will hydrate and clog up the column. Any time scum builds up in the column, the surface data logger should make sure, when making density readings, that the shale particles have freely found their own level without sticking to other material.

3. It is theoretically possible to raise the column by adding sodium polytungstate to the bottom of the column. To do this use at least 16 inches of Tygon tubing and a Sand Content Funnel to afford sufficient hydrostatic pressure to raise the column.

Cuttings Selection and Preparation

Using Cuttings Recovered from Water-Based Mud

For the most consistent density readings when the drilling mud system is using a water-based mud, follow these recommendations.

1. Use normally washed and screened cuttings.



Caution: Do not handle the cuttings with your fingers. The oils in the skin will contaminate the density readings. Use tweezers to handle the individual cuttings.

2. Under the microscope, select suitable bottom hole cuttings. See Figure 2.7.

a Select sharp, angular cuttings. Avoid smooth cuttings.

b Avoid cutting sloughed from the sides of the hole. These may appear smooth on one side or be flat rather than angular.

c Avoid cuttings which are cracked or have discernible crevices. These often contain trapped gas which would alter the density reading.

d Select bottom hole cuttings. They may appear slightly changed in color, if the bit is drilling a new formation.

e Pick cuttings of average size.

f Pick at least five good samples for each logging interval.

Note: Do not attempt to measure the density of very porous shale (so-called gumbo shale). Such shale absorbs the gradient fluid very quickly and thus no true density can be determined. The high water content of the shale also quickly contaminates the gradient solutions.

3. Use the cuttings as soon as possible.

a Maintain a consistent routine.

b Pat the cuttings dry with a paper towel.

c Do not air dry, spin dry, or force dry the cuttings.

d If waiting time must be inserted at this stage, leave the cuttings submerged in water during the waiting period. Keep this period to a minimum.

Note 1: Select sharp, angular cuttings. Avoid smooth cuttings.

Note 2: Avoid cuttings sloughed from the sides of the hole. These may appear smooth on one side or be flat rather than angular.

Note 3: Avoid cuttings which are cracked or have discernable crevices.



Figure 2.7 Suitable Bottom Hole Cuttings

Using Cuttings Recovered from Oil-Based Mud

This procedure is basically the same as when using water-based drilling fluid, although oil-based mud allows more consistent readings. The extended low range calibration beads may be needed since samples become available at shallower depths.

1. Use normally washed and screened cuttings

2. Select suitable cuttings as with water-based mud.



puter.

3. Use the cuttings as soon as possible.

Note: If waiting time must be inserted, leave the cuttings submerged in the base oil of the mud during the waiting period.

Using Dry Cuttings A good shale density gradient can be obtained using dry cuttings so long as dry cuttings are consistently used. It is much harder to select suitable cuttings once the shale has been dried. Cracks and crevices become a major difficulty.

The density readings are harder to make since the cuttings absorb the gradient fluid after they have reached a first equilibrium. Hence, unless unavoidable, the use of dry cuttings is not recommended.

Reading Shale Densities

Basic Procedure 1. Using tweezers, release one cutting immediately above the surface of the mixture and wait for it to come to rest in fluid of the same density.

Note: The cuttings will normally fall quite rapidly at first, then begin to slow as it nears fluid of the same density. It will have carried a halo of less dense fluid with it, which will disperse in a few seconds.

2. Read the level of the midpoint of the cutting about four seconds after it has slowed to near motionlessness. Immediately use the calibration graph to figure the density.

3. Do not record unreliable readings. The following are such indications:

a There are observable air bubbles released from the cutting.

b The cutting adheres to the column wall or another cutting.

4. After recording the densities of at least five cuttings in an interval (normally 30 feet), compute the average density.

a Discard the highest reading and the lowest reading, and average the middle three.

b If you vary this procedure, note the variation in writing on the data sheet.

c Note any known changes during the interval which could affect shale density readings as comments on the data sheet. Include changes in lithology which affect density readings.

5. Record these average densities on the standard Sperry-Sun Surface Logging Systems data sheet as “shale density.” Then enter the density in the com

Dealing with Inconsistencies

If you vary the above procedures, do so consistently and note the variation inwriting on the data sheet.



Replot the calibration graph whenever there have been noticeable changes in the positions of the beads. It is a good practice to replot the calibration graph every two days.

Do not attempt to second-guess your results. Make predictions, but remain objective by following the established procedures.

Note: The accuracy and reliability to the shale density graph is directly determined by the consistency and careful method of the surface data logger.




Show EvaluationGas Determination from the Drilling Mud

Chapter 3 Show Evaluation

When an oil or gas reservoir is drilled, a drilled interval of rock fragments and the formation fluids that it contains are carried to the surface. If it was possible to reconstruct these fragments and fluids at reservoir temperature and pressure, and if the fragments and fluids were the only source in the borehole, it would be possible to determine, the quantity, type and productivity of the fluids contained in the reservoir.

This highly desirable hypothesis remains beyond practical achievement. A reservoir is a highly complex system whose stability is distorted even prior to being drilled. The addition of material from the borehole wall and radical changes in temperature and pressure in transit to the surface will change the composition of the sample. At the surface, variable efficiencies and characteristics of the surface extraction and analytical equipment will lead to further compositional and concentration changes as the sample proceeds to final analysis.

Quantitative determination using Mud Log gas shows is, and will remain, an impossibility. On the other hand, when used as qualitative formation evaluation tool, the Mud Log is essential and irreplaceable. It is not the intent of this manual to propose changes in surface data logging technology or procedures, but to examine the physics and chemistry underlying the basic gas extraction and analysis process.

3.1 Gas Determination from the Drilling Mud

As the drill bit breaks loose the formation, cuttings and gas in the formation are transferred to and entrained in the drilling mud and transported to the surface. With this in mind, the surface data logger hypothesizes the existence of a direct relationship between the kind and amount of gas and/or oil in the drilling mud arriving at the surface, and the gas and/or oil that was in place in the formation being drilled at the time that particular mud was passing by the bit at the bottom of the hole. It may be an over simplification at this point, but this represents the situation in general and the description of the gas parameter.

The gases, if present, are assumed to be released by the formation and cuttings into the mud stream to be entrained in solution in the mud. The concentrations or amount of this entrainment normally encountered is on the low order of less than 5%. This entrainment is also influenced by pressure, temperature, etc.



All that remains now is to convert this parameter to a meaningful representation of the character of the formation before being disturbed by the bit. This conversion is accomplished by three parts of the gas detector and related equipment. These parts are:

1. The gas trap, which is the device for removing gases from the drilling mud.

2. The transporting equipment, consisting of a sample pump, pumping the gas-air mixture to the gas detector, the hoses, the plumbing, and flow regulation equipment.

3. The gas detectors proper (Total Hydrocarbon Analyzer and Gas Chromatograph). These detectors are the Flame Ionization Detectors, see the Sperry-Sun Drilling Services Gas Systems Manual for detailed information on these detectors and flow conditioners.

3.1.1 Aeration Gas Trap

The gas readings from the drilling mud as related to fluids and gases in-place in the formation must be interpreted with the following consideration in mind:

The extraction of this gas from the drilling mud must be done in a manner that is independent of variables such as density, viscosity and gel strength of the mud; in a manner independent of the flow rate of the mud through the whole mud system; in a manner so that all the gases as completely possible may be extracted even from a high gel strength mud, and in a manner which would be considered reliable around drilling rig conditions which tend to be destructive of sensitive equipment.

Sperry-Sun currently uses two types of gas traps. These are air powered and electrically powered.

In operation, the bottom of the trap lies submerged about two inches under the surface of the returning mud stream. The mud, tending to seek its own level, flows in the inlet in the bottom of the trap canister. Rotation of the motor-driven impeller blade causes this mud to whirled around rapidly. The centrifugal force of this whirling action causes the level of the mud to be raised around its periphery inside the canister until it flows out the discharge on the side of the trap. See Figure 3.1. The depth to which the trap is lowered into the mud should be adjusted to give a continuous sample of 3 gallons per minute (1 quart in 5 seconds) of mud flowing through the trap.



Figure 3.1 Mud Gas Trap

Simultaneously, as the sample of mud is being pumped through the trap, the whirling action of the impeller whips air from the atmosphere inside the canister into the mud. These bubbles of air tend to become united with the tiny molecules of gas entrained in the mud and being much larger, develop a size having a surface tension sufficiently low to be released from bondage by the drilling mud. These bubbles of air thus serve as a carrier by going into the mud, uniting with the gas and carrying the gas out of the mud into the atmosphere of the canister.

Hints and Precautions:

1. The trap should be located as near as possible to the discharge of the flowline, or at least in a way so that it will have immediate access to the mud returning to the surface. See Figure 3.2.

2. The trap should be located in an open atmosphere. The trap discharge must have immediate access to fresh air. This may not always be possible on some rigs.

3. If difficulty is experienced with lost circulation material, removing the flange on the trap bottom sometimes helps maintain a steady flow of mud.

4. Keep the locking screw on the adjustment jack tight after adjustments are made.

5. Mud should not be discharging from the trap in an intermittent manner but should exit in a continuous flowing manner.

Gas rises and escapesvia exhaust line to analyzer.

Mud enters trap.

Mud exits trap.



Figure 3.2 Gas Extraction at the Ditch

3.1.1 Transportation Equipment

After the mud has been sampled and the gases removed from it, these gases must be transported to the gas detectors in the logging unit. This is accomplished by a small motor-driven compressor which is connected to the trap by a length of rubber hose. The compressor pulls a continuous stream of fresh air in through the discharge of the trap. As the gases, if present, are being continuously extracted from the mud in the trap, they will be continuously mixed with this stream of air and carried with the air into the logging unit through the connecting hose. There, the flow of air, or air-gas mixture, passes through additional flow regulation equipment, plumbing and instruments and finally arrives at the detector element for continuous detection and monitoring. See Figure 3.3.

Air Port

Agitator MotorVacuum Line

To MudLoggingUnit

Return Flowline

Ditch(Possum Belly)

Desander Settling Pit

Shale Shaker

Gas Trap

To Mud Pit



Figure 3.3 Gas Analysis System

In the logging unit, the flow is kept constant by the Total Hydrocarbon Conditioner, and the flow rate is read on the flowmeter. The flow is split either two or three ways, and the majority of the flow is discharged back to the atmosphere.

The optimum flow of air from the trap is 6 to 8 cubic feet per hour (cfh). The total flow meter is a small flowrater, calibrated to read directly in cfh of 0 to 10 cfh. The flow is adjusted by an adjustment knob in the flowrater and should be kept at 6 to 8 cfh which will be maintained at this constant by the regulator. More volume of the air-gas mixture than is necessary for detection is drawn from the trap in order to minimize the lag time between the arrival of a show at the surface and its detection.

It now becomes apparent that a reliable gas detecting technique demands that the number of influencing variables be kept in control. Ideally, only the amount of gas in the mud and its corresponding reading should be variable. For this reason, it is important that the trap consistently pump a constant volume of mud, that the amount of air drawn through the trap be maintained at a constant, that there be no leaks or restrictions in the flow system.

InputFromDitch

Vacuum Pump

Pressure Regulator

Detector

Exhaust

Filterand

DryerFlowmeter

Milliameter

Chart Recorder


Show EvaluationOrigins of Gas Shows

r,” of a tion

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3.1.2 Gas Detection Equipment

See the Sperry-Sun Drilling Services, Surface Logging Systems, Gas Systems Manual for the detailed operation of the Total Hydrocarbon Conditioner, Total Hydrocarbon Analyzer, and Gas Chromatograph and the peripheral equipment related to these instruments.

3.2 Origins of Gas Shows

A gas show can be defined as a significant occurrence of hydrocarbons gases detected from the mud stream and identifiable as being the result of the drilling of specific interval of formation. This definition is apparently very simple and readily understood. It is in fact ambiguous and if taken literally, can lead to confusion.

The magnitude of a gas reading seen at the surface is not a true mark of its significance. Nor is the fact that a gas reading can be identified as coming from a volume of formation quantitative evidence of the volume of gas in place in that formation or even liberated from it while drilling.

The object of good mudlogging is to plot those gas readings produced by gases liberated from drilled formation in conjunction with the data relevant to their interpretation. The object of mud log analysis is to reconstruct from these the composition and mobility of reservoir hydrocarbons. In performing these tasks it is necessary to appreciate the physicochemical processes active in the formation, the mud circulation system, the gas sample extraction and analysis equipment. The amount of gas, i.e., the number of “gas units” or “percentage of gas in aidetected by the gas detection equipment from a given formation is the resultcomplex of interacting variables. These factors begin to act before the formahas been drilled and continue their effect until the gas sample enters the gasdetectors.

In order to reconstruct a picture of the fluids in place in a formation and the tyof fluid the formation may produce, it is necessary to study gas magnitude ancomposition in the mud stream and cuttings, oil and water themselves, and changes in the drilling process and circulation system which may affect or beaffected by formation fluid behavior.


Show EvaluationOrigins of Gas Shows

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3.2.1 Definitions

Prior to considering these complex factors, it is necessary to define the usage of the term “gas show” as it is to be used in this manual. To do this it will be necessary to define also the terms “background gas” and “circulation gas.” Although apparently self-explanatory, these terms are commonly given multipuses in the industry.

Circulation Gas

This is the value of gas seen by a gas detector when circulating under normaconditions, meaning a clean, balanced borehole with drill pipe in the hole androtating but with the bit off bottom and with no vertical movement. Under succonditions some gas will be present in the sample drawn from the mud streamit will represent only contamination or recycled hydrocarbons in the mud.

Background Gas

When drilling through a consistent lithology, it is common for a consistent gasvalue to be recorded. Certain lithologies (for example, overpressured shales)show considerable variation in the background gas. Background gas may beobserved to vary with drilling, mud or surface conditions without any change lithology or formation hydrocarbons. This should always be given consideratiin both formation and hydrocarbon evaluation.

Gas Show

This any deviation in gas, amount or composition, from the established background. This may or may not accompany a change in lithology, may or mnot indicate a significant or economic hydrocarbon accumulation. In other wo“Gas Show” is a term describing an observed response on the gas detector, hno causal or interpretive significance.

It is common for the surface data logger to be asked, “What is a good gas shThe answer to this is complex and relates to many factors beyond the simplenumber of gas units seen. To decide whether a gas show is “good” or “poor”,i.e., whether or not a significant hydrocarbon accumulation is indicated, requirtotal evaluation of all mudlogging parameters plus consideration of the manyvariable system conditions.

The manner and extent to which shows will manifest themselves varies so gramong the many different regions that it is impossible to set even a general srequirements which must be met to qualify a show for additional evaluation o


Show EvaluationSources of Gas in Mud

determine to what that evaluation should be. To a large extent, evaluation of interesting zones becomes a matter of comparison of likes and differences. Parameters of the log through the sections in question are compared with the same parameters in adjacent known barren zones for perception of the degree to which they changed or did not change. Generally speaking, the key to interpretation lies not in the magnitude of the reading reached, but in the extent to which it did change.

3.3 Sources of Gas in Mud

Gas detected in the mud stream may originate from the formation via a number of mechanisms. It is necessary for the surface data logger to isolate and attribute these causes in order to draw the appropriate conclusions. Gas originating from other sources or only indirectly from the formation will also be seen in the mud stream. This must, if possible, be recognized and removed from consideration. See Figure 3.4.

Figure 3.4 Sources of Gas in Mud



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rilling can

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nd rvoir. gas m the

and

oir has

oil as

3.3.1 Gas from Drilling

This is often referred to as “liberated” gas since it is liberated from the crusheformation produced by the drilling process. This should not be taken to imply the total volume of gas in place in the formation is liberated to the mud streamdetected at the flowline. As discussed below, not all of the gas seen at the suwill be present in the formation as free gas. Conversely, not all of the free gaplace in the formation will be liberated at the surface. Some free gas will remtrapped in the drill cuttings due to lack of permeability. Some gas, especially lighter hydrocarbons, will remain dissolved in the drilling fluid and not be released at the surface. Thus, though it can be said that the gas liberated by dreflects the composition and saturation of gas in place, no direct relationshipbe drawn.

3.3.2 Free Gas and Liquefied Gas

Methane and ethane, the two lightest paraffins, have critical temperatures of

-82.5oC and 32.3oC, respectively. Since most petroleum reservoirs will have temperatures in excess of this, the two will always exist in the formation onlygases. All other hydrocarbons and water may exist in both liquid and gaseouforms in equilibrium, dependent upon the temperature and pressure of the formation.

Since the vapor pressures and critical temperatures of all hydrocarbons are different, the composition of the free gas in the reservoir will differ from that othe oil with which it is associated. Similarly, the composition and volume of thgas detected at surface temperature and pressure will be different to that in p

3.3.3 Dissolved Gas

Much of the gas detected at the surface is present in place in solution in oil awater. This solubility depends upon the temperature and pressure of the reseOnly when the oil and water are fully saturated with dissolved gas will a free phase be present in the reservoir. Some gas will be liberated and detected frosolution when carried to the surface. Other gases will remain in solution in oilwater and be retained in the mud system.

The presence of gas as a liquefied, dissolved or free gas phase in the reservmajor influence on the relative permeability of the reservoir and its material balance, i.e., the type of production and productivity. Similarly, due to the differing solubilities of various hydrocarbons, the solution of gas in recoveredand water and mud filtrate will have an effect in reducing the amount of the gdetected at the surface and in changing its composition. See Figure 3.5.



Figure 3.5 Effects of Temperature, Pressure, and Salinity on the Solubility of Gas in Water

3.3.4 Effective Porosity and Permeability

It is important to relate the magnitude of a gas show to the fluids in place and hence to reservoir productivity. In order to do this the concepts of absolute and effective porosity and permeability must be taken into consideration. See Figure 3.6 and Figure 3.7.



Figure 3.6 Effect of Porosity on Gas Shows

Figure 3.7 Permeability and Effective Porosity



The imperfect gas law allows the computation of the volume occupied by a specific quantity of gas at varying temperatures and pressures (Figure 3.8). The converse of this would indicate that a fixed volume of pore space, as defined by porosity, hole diameter, and footage, would contain different quantities of gas at different depths, i.e., temperatures and pressures. The result will be that, with increasing depth, equal volumes of pore space, i.e., porosity and gas saturation, will produce greater volumes of gas into the mud stream. See Figure 3.9.

Figure 3.8 Gas Law

Figure 3.9 Effect of Depth on Gas Shows



Although the reservoir will contain a percentage of bulk volume as void space, only a proportion of these voids will be interconnected in such a way as to provide a flowpath, i.e., effective porosity. Permeability is related, since a lithology with zero effective porosity would also have zero permeability. However, the two are not directly related since one, effective porosity, is a measure of the quantity of connected voids whereas the other, permeability, is a measure of the quality of the interconnections. See Figure 3.7.

Nevertheless, where a formation lacks effective porosity and/or permeability, only a fraction of the pore fluids contained in it will be liberated to the mud stream during drilling, i.e., only those contained in pores exposed by the crushing process. If porosity is not effective, other pores within the cuttings will remain intact and retain their contained fluids. If permeability is poor, but the effective porosity is good, fluid will be lost from the pore spaces, but only slowly - some being retained even at the surface. In either case, analysis of the fluids retained in the cuttings is essential in estimating the total hydrocarbons in place and the ability of those hydrocarbons to flow out of the formation.

Evaluation of cuttings gas is also essential in determining the gas content of non-reservoir rocks which are known to have little or no permeability or effective porosity, e.g., shales and mudstones. Although such rocks are rarely of interest in terms of petroleum accumulation, they are known to be the source of most formation fluids, both water and hydrocarbons. This is due to their high initial content of water and organic debris which is lost in diagenesis due to compaction and thermo-catalytic degradation.

Analysis of hydrocarbon content in shale cuttings can be of value in determining the presence of both mobile and potential hydrocarbon sources. Enrichment of hydrocarbons will also occur in shales where rapid sedimentation has prevented dewatering and hence hydrocarbon displacement, resulting in abnormal formation pressures.

It should also be remembered that in a potential reservoir where a mixture of fluids is present, (water and/or oil and/or gas), the reservoir will have an effective permeability to each fluid less than that to each if present alone. Some attempt to reconstruct the character of the fluids in place will be advantageous in estimating the nature of eventual production from the reservoir.

Relative permeability can be defined as the effective permeability of a reservoir to a fluid (i.e., the actual rate at which that fluid will flow), when one or more other fluids are present, as a fraction of the permeability of the reservoir to that fluid when it is present alone under the same conditions. The effective permeability to each phase will be a function of the number of phases present, the proportion of pore volume occupied by each phase, the chemical composition and physical properties of each phase and the degree of continuity of each phase. See Figure 3.10.



Figure 3.10 Effective Permeability

3.3.5 Summary

It would appear that such complex interactive processes are at work as to hamper any estimate of quantity and type of fluids in place from a surface gas analysis.


Show EvaluationFactors Influencing the Amounts of Gas in Mud

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While it is true that no quantitative determination of either fluid in place or eventual production is possible from a surface analysis, it is also true that similar reservoirs can be generalized sufficiently to allow good qualitative correlations. Thus it may be possible to discriminate between a high gravity and low gravity reservoir or even to estimate an oil-water contact by distinctive gas composition. Such interpretations are an essential guide prior to running logs, a tool in the interpretation of those logs, and where control is good, may even prove to be a better means than logs in selecting productive intervals.

Most petroleum hydrocarbons originate from a similar organic source and proceed in their maturation via a similar temperature and pressure controlled physico-chemical process. For this reason, petroleum accumulations (although markedly different in composition) tend to show a spectral relationship to each other in terms of the type and amount of hydrocarbon species present. Therefore, though two crude oils may be extremely different in total composition, they will contain some similar components in similar compositional relationships to each other. Since petroleum maturation continues by the continuous “cracking” of complex branched molecules into simpler straight-chain molecules, these significant relationships are readily seen in the universal petroleum gases, methane through pentane. Thus, study of chromatographic analysis of thesemay often lead to a gross estimate of the type and quality of the reservoir.

Nevertheless, all of the factors explained above plus those to follow will contribute to the inaccuracy of such estimates and to the likelihood of some exceptional reservoir giving false indications. In addition, the gas analysis is one factor on the mud log. All others must be given consideration in evaluatinthe reservoir. Oil shows, water indications, lithology type, porosity and permeability are of equal or more importance in assessing potential productiv

3.4 Factors Influencing the Amounts of Gas in Mud

Although the interval of formation produced by drilling releases a quantity of which may be detected at the surface, this gas undergoes many influences bethe formation and the gas detector. There are also many other sources of gasborehole which must be isolated or eliminated before correct evaluation can made.

3.4.1 Flushing

It is well known that where the borehole pressure exceeds the formation presand permeability exists, the drilling fluid will tend to flush into the formation. Ithe solids diameter is sufficiently high, filtration will result. Mud filtrate will flush



into the formation, leaving a clay filter cake which eventually becomes dense and thick enough to be sufficiently impermeable to prevent further filtration (Figure 3.11). Such flushing commonly causes little formation damage since invasion takes place only a short distance into the formation. However, where effective porosity is low, only a small volume of flushing may give a large diameter of invasion. Displacement of gas some distance from the borehole in this way may so reduce the reservoir’s gas saturation and effective permeability to gas close to zero in the vicinity of the borehole. Thus a zone which gives good gas shows when drilled will appear water-bearing or recover only mud filtrate when logged or tested.

Figure 3.11 Flushing of the Formation



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This effect can be accentuated when dispersed clay or clay cement is present in a reservoir. If the clays are diagenetically immature, i.e., so-called swelling or mixed layer clays, invasion of mud filtrate may result in swelling or “recrystallization” of clays within the pore space, drastically reducing both permeability and effective porosity within the reservoir adjacent to the boreho

Flushing will also take place at the bottom of the hole when an overbalance e(Figure 3.11). In this circumstance no permanent mud filter cake can be formdue to the continuous action of the drill bit. Flushing below the drill bit will havmost effect when the reservoir has high permeability and effective porosity. Tdifferential pressure to the advantage of the borehole combined with high imforce due to the jet nozzle pressure drop will force mud filtrate into the formaahead of the bit. Dependent upon the relative horizontal and vertical permeabilities of the formation, the contained formation fluid may be displaceahead of or to the side of the bit's path.

When the formation is eventually drilled, little or no gas will be liberated. At thsurface a flat, unresponsive gas curve will be seen which may even indicate gas than in nearby formations. Since permeability is high, the reservoir will reto its natural state soon after drilling, and an apparently water-bearing reservmay later be logged or tested as productive.

Common good drilling practice in minimizing mud weight and water loss will advantageous in reducing flushing, but, to aid in the interpretation of such anomalies, the surface data logger should have sufficient information on the following:

1. Pump pressure

2. Jet nozzle sizes3. Mud rheology (Plastic Viscosity and Yield Point)4. Mud weight and ECD (Equivalent Circulating Density)5. Mud filtrate (water loss)

Evaluation of the flushing ability of the mud combined with the susceptibility othe formation to flushing should guide the surface data logger in the correct evaluation of the gas curves.

Compared with mud gas, high cuttings gas may indicative of poor permeabiliteffective porosity. The lithological description should indicate which. Where acombination of mud gas and lithology description indicate good permeability,flushing is to be expected. This may result in simple fluid displacement or mopermanent physical or chemical damage. (See Figure 3.12)



Figure 3.12 Reservoir Damage Due to Flushing

It is essential in assessing the possibility of formation permeability damage that the distribution of clays relative to porosity be determined and clay type identified on the log. For this reason clay ion exchange capacity (Shale Factor) should be determined and plotted on the log for the clay fraction of all samples. If this is not possible, the surface data logger should perform a wettability test on a fresh sample containing clay and report the water sensitivity of the included clays.

In addition to this it has been suggested that formation permeability damage may result due to the flushing and flocculation of mud clays in the formation adjacent to the borehole. This is difficult to verify, but reference to the base exchange capacity of the drilling mud may be of assistance in ascertaining the possibility of damage of this type, which in any case is likely to occur only where porosity is extremely large, i.e., where pore throats are capable of passing mud solids.

A formation indicating high porosity and permeability confirmed by a good rate of penetration, which shows little or no gas in either the mud or cuttings, should be strongly suspected of being flushed prior to drilling - especially where an overbalance exists. The occurrence of a clean, high porosity and permeability formation containing few or no hydrocarbons is in itself sufficient to lead to suspicion. However, the possibly does exist that the formation contains only water without even gas in solution. This possibility may be confirmed or rejected by monitoring mud salinity.



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Like the Shale Factor test, differential salinity is a tool which can be used. So long as a sufficient salinity differential exists between the drilling mud and the formation fluids, the drilling of a high porosity formation containing water should be indicated by a noticeable, though not extreme, change in mud salinity and hence resistivity.

3.4.2 Fluid Invasion

The invasion of formation fluids into the borehole may result from a number of causes, some but not all of which result from an underbalanced condition of either a temporary or permanent nature. If an underbalanced condition exists in the well, i.e., if a differential pressure to the advantage of the formation exists, there will be a natural tendency for fluid to flow from the formation into the borehole. Where a formation exists having good porosity and permeability, this flow will be massive and a kick will occur. Such a kick will be indicated by the invasion of formation fluid downhole, causing the expulsion of mud from the borehole at the surface. Were this to continue, a blowout would result. It is the surface data logger’s responsibility to monitor the mud pit level and report any unpredicted or unexplained level changes.

A massive invasion of fluid resulting in a well kick is unlikely to be misinterpreted as a gas show. In fact, if the hole is full, the kick should be recognized by a rise in the pit level long before the fluid causing it has time toappear at the surface (Figure 3.13).

However, minor invasions due to slight or temporary underbalance, or whereinsufficient permeability is provided a sustained kick exists and must interprecorrectly (Figure 3.14).

When an underbalance sufficient to cause a kick exists, but there is insufficiepermeability to sustain a massive fluid influx, a steady fluid “feed-in” may resIf this minor flow is from a discrete formation already drilled, it will be noticeable, producing a sustained minimum gas background even when circulating, but not drilling.

If the “feed-in” is from the formation currently being drilled, then as a greater agreater area of formation in the borehole wall is exposed by drilling, increasinflow will take place (Figure 3.15). If this is the case, the mud gas will exhibit asustained minimum when circulating as shown above, but will consistently risdrilling proceeds. Cuttings gas will inevitably be high relative to mud gas sincis only the lack of permeability which is preventing the feed-in from becomingkick.



Figure 3.13 Comparison Between a Gas Kick and a Large Gas Show

Oil inSandstone

Gas inSandstone

Casing

Drilling fluid isdisplaced by intrudingformation fluid (Oil,Gas or Water)

Gas inSandstone

Casing

Gas bearingcutings



Figure 3.14 Fluid Invasion into the Wellbore

Casing

Gas inSandstone

Oil inSandstone



Figure 3.15 Feed-in Due to Underbalanced Drilling

Where permeability is effectively absent, e.g., in clays or shales, even a minor feed-in cannot take place. Fluid pressure in the rock will gain access to the borehole by the opening of preexistent microfractures and partings in the rock. The result will be the caving or sloughing of rock fragments into the borehole, accompanied by a small amount of gas (Figure 3.16). As above, a minimum gas background and, in this case, cavings recovery will exist even when circulating without drilling.



Figure 3.16 Caving or Sloughing Shale Due to Underbalanced Drilling

Bottomhole pressure, when circulating is higher than when the mud is static. This is due to annular pressure losses when circulating. It is, therefore, possible for a feed-in, caving or even a kick, to result due to a resultant underbalance when circulation is stopped. Furthermore, pressure if further reduced due to the so-called swabbing effect when the drill pipe is moved upward, e.g., when making a connection. The literal meaning of swabbing is the pulling of a full gauge tool from the hole, acting like a plunger in a syringe and initiating fluid flow into the borehole. Swabbing by moving the drill string does work in this way. When the drill pipe is pulled upward, the high viscosity gelled mud will attempt to move with the pipe, thus reducing the effective hydrostatic pressure acting on the borehole wall. Pressure reduction is a function of pulling speed, mud rheology and annular diameter. The important consideration is that pressure reduction takes places not just below the bit but at all points in the open hole.

Downtime gas or connection gas is a gas show resulting from the momentary underbalance due to the pumps being shutdown and/or pipe movement. It can be recognized by the occurrence of discrete gas show appearance at, or slightly less than, the lag time after circulation recommences. This is gas actually being produced by the formation and the value should be reported on the log as it is indicative of formation permeability and fluid content. The surface data logger should also check a flowline mud sample when a connection gas occurs for evidence of produced oil or saltwater with the gas. The incidence of connection

ImpermeableWeak Matrex(Shale)

Permeable(Sandstone)



gas should also be reported to the drilling foreman who may choose to increase the mud weight in response to the indicated underbalance.

It is important to remember that the whole open hole section will be underbalanced by swabbing. The connection gas may not come from the bottom of the hole but from some horizon above. In fact, two or even more connection gases may result from a connection. For this reason, it is important that lag time and annular velocities should be accurately known by the surface data logger so that connection gases can be identified with the producing formation and the mud log annotated accordingly.

Drilling into a permeable reservoir with an underbalance is potentially dangerous, as a kick may result. Even if a kick does not immediately occur, the hazardous situation will be marked by an increasing feed-in as more formation is drilled, accompanied by progressively larger connection gases. This condition should be reported by the surface data logger and noted on the mud log. If increases in mud weight alleviate or remove the effect, this should also be noted on the mud log in explanation of the consequent reduction in gas.

Where a balanced or even overbalanced condition exists, it is still possible for formation fluids to move into the borehole. Normally, this will occur only where reasonable permeability exists in the formation. The mechanism involved is an interchange of fluids between the formation and the borehole, either by diffusion of lighter hydrocarbons or by the flushing of mud filtrate into the formation, displacing fluids out at some other point. Even though a permeable formation will be flushed with mud filtrate during and shortly after drilling, it is possible for some lighter gaseous hydrocarbons to move back into the flushed zone. This may be due to gaseous diffusion or to the mixing of mud filtrate with formation water containing dissolved gas. Where an impermeable mud filter cake has not yet formed or when the filter cake is removed by stabilizers, bit, or pipe movement, this gas-bearing mud filtrate may interchange with the mud in the annulus and be carried to the surface, resulting in a low, continuous gas background (Figure 3.17).



Figure 3.17 Gas Diffusion at a Permeable Formation

A more important incidence of fluid entering the borehole without an underbalance existing is in connection with flushing at the bottom as discussed above. It was shown how mud filtrate may flush into the formation ahead of the bit, displacing the original formation fluids before drilling takes place. Where a sufficient thickness of formation has been cut and vertical permeability exists, it is possible for these displaced formation fluids to be displaced back into the borehole at some point above the bit turbulence (Figure 3.18). The effect of this during normal drilling will be to effectively delay the appearance of a gas show until sometime after the formation is drilled. This may lead the inexperienced surface data logger to suspect some error in the lag time or even that the gas lag is somewhat longer than the cuttings lag.

Figure 3.18 Flushing from the Formation into the Borehole



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It should be remembered that the fluid contained in this influx may not be representative of the total fluids in place, but will be, in effect, produced fluids under a highly energetic water drive. In fact, depending upon mud rheology, hydraulics, overbalance and formation permeability and effective porosity, more fluid may be flushed from the formation in this way than would be produced by drilling it. If drilling stops and circulation continues, this formation “sweeping”effect will continue and mud gas will be seen to remain relatively constant, declining only slowly as the formation becomes depleted progressively furthefrom the borehole.

The effect would appear to behave very much in the same way as a bleed-inThere are, however, dissimilarities which indicate the presence of a different mechanism. Once sufficient exposed formation exists to allow sweeping, onlincreases in formation porosity, permeability or mud hydraulics will increase gas seen at the surface. The steady increase with drilling progress characteria bleed-in will not be seen, nor will a connection result in large or increasing connection gases. Most significantly, if the bit is lifted off bottom to a point abothe fluid invasion point to a position where normal flushing has produced an impermeable filter cake, the mud gas will show a rapid decline to normal withfurther circulation, i.e., sweeping no longer takes place.

Trip gas is a complex phenomenon. At best it can be said that it is a combinaof some or all of the above fluid invasion mechanisms. Nevertheless, regardlethe producing mechanism, it is true that one or more gas shows will be seen breaking circulation after a trip, coming from the bottom of the hole or the ophole section above it. This gas has been produced from the formation and thsurface data logger should report it on the mud log, and lag it back to the proboriginating formation and test mud samples coincident with the gas shows foproduced oil or water.

Care should be taken in anticipating “kelly cut” and recirculated trip gas. Kellcut is the result of air being pumped around from a partly empty drill string. Twill appear at the surface after the in/out lag (bottoms up plus down pipe voluhas passed from the time circulation commenced. Air will be compressed unborehole hydrostatic pressure, resulting in a slug of aerated mud being pumpfrom the bit and up hole. The increased tranmissivity of this aerated fluid will assist in any sweeping of diffusion processes active in the open hole especiasince immediately after a trip any mud cake stripped during the trip in will notbe fully reformed. The aerated mud will thus be enriched with formation hydrocarbons and produce a gas show at the surface. The presence and maof this indicate the presence of permeable hydrocarbon bearing formations downhole, but is of little diagnostic value beyond this.

In a dry hole, i.e., where the kelly cut picks up few or no hydrocarbons, confumay arise due to the arrival of the kelly cut, causing visible gas-cut mud at thflowline while the surface data logger reports no gas. An experienced surface



as

or at

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fully

ns

bit,

y me

logger will learn to anticipate arrival of the kelly cut and will report the fact to the driller.

Recycled trip gas, connection gas, or any other gas show will behave in a similar manner to kelly cut, producing an extended gas show. Similarly, oil accompanying a trip gas may, if not checked on its first occurrence, return and be incorrectly logged as a deeper oil show. The experienced surface data logger should anticipate gas show recycling by knowledge of the total circulation time of the circulation system.

3.4.3 Mode of Penetration

The amount of gas contained in a drilled formation will be controlled by the porosity and gas saturation of that formation. Since porosity also strongly influences the physical strength and “drillability” of the formation, it is to be expected that the rate of penetration will show a strong correlation with the gcurve. In combination these factors can be seen that comparison of rate of penetration with the total gas curve will permit gas saturation to be deduced,least qualitatively estimated.

Drillability depends both upon porosity and the strength of the rock matrix. Fothis reason the rate of penetration (ROP) will respond characteristically to chain both porosity and rock type. In fact, its response will be very similar to the Interval Transit Time from the Sonic Log, i.e., when the formation becomes harder or less porous both ROP and Delta T will fall, and they will rise with decreased rock strength or increased porosity. If the ROP scale used is carechosen, very close comparison is possible between the two logs and a goodcorrelation is possible.

ROP is therefore useful as a means of stratigraphic correlation, for picking lithological tops and for estimating formation porosity. Comparison of the porosity deduced in this way with the gas shows then allows further deductioabout formation fluid type and permeability.

Unfortunately, ROP is also affected by other factors, among them: weight onrotary speed, bit type, bit wear, drilling hydraulic, and most importantly, differential pressure between the borehole and formation pressures.

Assuming that all other formation, mud, and drilling considerations are held constant, the amount of gas liberated to the mud stream by drilling will be a function of the total volume of effective porosity exposed to the mud stream bthe cutting action of the bit. More simply, this will be dependent upon the voluof the cylinder of formation cut (Figure 3.19). It will also vary with bit selectionsince different bits provide different sizes of cuttings.



Figure 3.19 Volume of Gas Produced by Drilling

It would appear that the height of the cylinder of cut formation is not relevant since the mud log is a depth-controlled plot, and gas readings are plotted foot by foot as the well progresses. This is, in fact, a misapprehension and a formation identical in all ways will produce higher mud gas readings if drilled at a higher rate of penetration (Figure 3.20).

Figure 3.20 Effect of Rate of Penetration on Gas Shows



The reason for this is very simple and relates to the way in which the gas curve from the chart recorder is translated to a gas curve on the depth-based mud log. It is normal practice for the surface data logger to mark lagged depths onto the chart recorder; these depth marks will be more or less evenly spaced according to the uniformity of the ROP, i.e., the time/depth relationship. Slowly drilled intervals will be more spread out, quickly drilled intervals closely spaced.

It is mathematically provable that the amount of gas passing through the gas detector over any depth interval is equivalent to the area defined by the gas curve. Only if the interval is very small can it be said that the quantity of gas is proportional to the height of the gas peak, since the duration is so short. Thus, if a fixed quantity of gas is introduced into the gas detector over two differing time intervals, the high gas reading of short duration, (e.g., high ROP) and the low gas reading of long duration (e.g., low ROP) will define similar areas. If only the height of the gas curve is considered, the longer duration reading would be interpreted as a lesser quantity of gas. For this reason, the magnitude of a gas show should never be considered alone as an indication of reservoir quality without, at least, some reference to and consideration of the rate of penetration.

The second factor controlling the volume of the cylinder of formation cut is the hole diameter. Although this will not vary extremely over the commonly used bit sizes, it should be remembered that the volume of the cut cylinder will vary as the square of the hole diameter (Figure 3.21). It should also be remembered, in conjunction of the two factors, that in general, smaller diameter bits will drill less quickly than larger bits, thus reducing expected gas shows accordingly.

Figure 3.21 Effects of Hole Diameter on Gas Shows


Show EvaluationCirculating System

size the

o the g any 2). tracted de.

ed trap

and

not

The cylinder of rock cut by the bit is not cut as a “whole” but as cuttings. The of teeth on the bit, which is governed by both bit type and bit size, will controlsize of cuttings produced. Where cuttings are smaller and more numerous, formation fluids will be more easily liberated from non-effective porosity and inferior permeability, giving improved gas shows.

3.5 Circulating System

3.5.1 Recovery at the Surface

Produced, liberated fluids and those retained with the cuttings are released tmud stream and carried to the surface. The volume of gas or cuttings enterinvolume of mud passing bottom will be a function of mud flow rate (Figure 3.2Since surface data logging gas analysis depends upon the analysis of gas exfrom the mud, changes in flow rate will affect the apparent gas show magnitu

Figure 3.22 Effects of Mud Flow Rate on Gas Shows

As mud flow rate increases, the volume of gas and cuttings contained in a fixvolume of mud will decrease. Conversely, the volume of mud passing the gaswill increase. The net effect should be zero. In fact, the complex geometries variable efficiencies of the various parts of the system will introduce some variations, but the overall effect is probably not that great. Mud flow rate will


Show EvaluationCirculating System

vary greatly within any hole size or in relation to hole size within hole sections. This further removes the severity of this effect.

Upon entering the drilling fluid at bottom under high pressure, high temperature and the influence of the bit turbulence, the gas and oil which are still retained within the cuttings will be finely dispersed or dissolved in the drilling fluid. As the mud travels up the annulus and the temperature and pressure fall, gas will come out of solution, expand and be released from the cuttings and form larger bubbles. Droplets of oil will release dissolved gas and accumulate into larger globules in the mud. This process has its major effect in the final stage of travel, i.e., the top 500 feet of the borehole. Here, the temperature and pressure are at their lowest and falling fastest. Also, the mud is traveling more slowly and uniformly at the maximum annular diameter. This is especially true offshore where most or all of the 500 feet consists of a large-diameter marine riser subjected to seawater cooling.

As shown above, with increased depth, equivalent volumes of gas in place will result in increased volumes of gas to the surface. If hole size and mud flow rate are constant, the increased volume of gas on expansion will disperse through a greater length of borehole annulus. For this reason, although deeper reservoirs may liberate more gas into the mud stream, the net result may not be gas shows of higher magnitude but similar shows of longer duration.

Where permeabilities are high, escape and accumulation of fluids in this way is rapid and requires little time. However, in medium to low permeabilities, high annular velocities due to high flow rates or low annular diameters, especially when coupled with high mud viscosities, will reduce the time spent in this critical section and increase the degree of turbulence in it. The result of this will be increased retention of gas and oil in the cuttings, i.e., high cuttings gas analyses relative to mud gas, and greater retention of gas and oil in solution and fine suspension in the drilling fluid, lowering mud gas extraction and hence detection.

3.5.2 Borehole Contamination

Strictly speaking, produced, flushed and other forms of post-drilling gas are not contamination but other forms of formation gas which should be isolated and used as diagnostic evidence. Although not plotted on the mud gas curves, their occurrence and magnitude should be reported on the mud log. There are other types of gas detected in the mud stream which are of little or no diagnostic value. The objective of the good surface data logger should be to remove the effect of these from analysis or, if this is not possible, report them and estimate their effect (Figure 3.23). In either case, the presence of contaminants in the mud stream and samples should always be reported on the log.


Show EvaluationSurface Influences on Gas Shows

Figure 3.23 Contaminants in the Mud Stream

A common source of gas contamination is the degradation of organic-based mud additives, e.g., lignosulphonate dispersant. These will degrade due to the effect of hydrostatic head and with the catalytic support of the clay ion exchanges sites on the mineral matrix. The common product of the degradation is methane, although more complex hydrocarbons may also be present.

In order to determine only those hydrocarbons liberated by drilling, it is necessary to establish the amount of hydrocarbons detected from the gas trap when freshly circulated mud is present but drilling is not taking place. Ideally, to do this, it would necessary to circulate for several hours to establish complete consistency in the mud system, ensuring that a stable baseline above which all other readings could be taken. This is not only impractical and prohibitively expensive, but the system background established in this way would remain valid for only a short time, probably less time than is required to establish it.

3.6 Surface Influences on Gas Shows

Although as outlined above, there are many factors which can affect the liberation and transport of gas to the surface, it is readily observed that the most important factors controlling the final magnitude of a gas show are in the rig’s surface system and the extraction, pneumatic and detection systems of the surface data logging unit.



3.6.1 Flowline

It is well known that a high degree of degassing takes place in the conductor and flowline. In a good gas show with extensive gas cutting of the mud, gas-produced foam can often be seen bubbling at the bell nipple. Loss of gas from the mud to the atmosphere will also occur extensively in the flowline, especially where (Figure 3.24).

Figure 3.24 Loss of Gas from the Flowline

1. The flowline is not filled with mud.

2. Changes in the slope of the flowline cause turbulence.3. Sections of the flowline are open to the atmosphere.4. The flowline enters the possum belly above the mud level.

Geometry of the ditch will be of considerable effect in the volume of mud and gas available to the gas trap. Location of the flowline entry, direction of major flow and the degree of turbulence will all affect the efficiency of the gas collection system.

3.6.2 Gas Trap

The efficiency of a gas trap can vary between 20% and 50% depending upon design, location and mud properties, but most importantly upon careful

Losses from the Bell Nipple

Flowline Not Full

Turbulence inFlowline

Open Flowline

Entry Above Mud Level



maintenance and good operation. The trap and its immediate surrounding should be kept clear of cuttings, debris, settled debris or mud caking, all of which may restrict or modify the flow of mud and air through the trap (Figure 3.25).

Figure 3.25 Losses of Gas Trap Efficiency

Mechanical efficiency of the trap is controlled by the rotational speed and surface area of the trap impeller, strength of the sample pump vacuum and the flow rate of air from the trap. Physical condition and submersion depth of the trap and impeller should checked regularly. The surface data logging unit should be equipped to monitor continuously the current drawn by the impeller motor, vacuum and sample flow rate.

Even when installation and maintenance of the gas extraction system ensures maximum mechanical efficiency, there will be variations in the overall efficiency of extraction and the magnitude of gas shows. This will depend on the composition of gas present, distribution of gas in the mud, viscosity and gel strength of the mud, and the mud flow rate.

3.6.3 Gas Detection Systems

The Total Hydrocarbon Analyzer records the volume of gas entering the detector element as a proportion of the total volume entering the detector element; for example: percentage ppm, gas units. It must be remembered that whatever unit is used, it is only indicating what proportion of the total of the flow drawn from the gas trap is made up of the particular component we are investigating, such as total

MotorMalfunction

Weak VacuumAir Slot Plugged with Mud

Ditch Blockedwith Cuttings

Trap Blocked with Cuttings

Damaged Impellor


Show EvaluationShow Evaluation

tions

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ased en run e ud of the tted

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gas (all combustible fractions). However accurate the analysis, we are still dependent upon the same sample which, as has been seen, bears only indirect and unpredictable relationships with the volume of gas contained in the formation. The value of the “gas unit” as a quantitative measure is also reduced by limitaof the calibration technique commonly used.

The Gas Chromatograph is designed to analyze only for a specific group of compounds (methane through pentane). Calibration of the GC is therefore eaachieved by introducing a mixture of these compounds of known compositionthe chromatograph.

The Total Hydrocarbon Analyzer, on the other hand, is required to analyze a mixture of unknown composition and constitution. It is commonly the practicecalibrate the THA with a single gas standard (i.e., methane) of known composition.

Since only a small volume of gas actually passes into the detection systems,essential that this volume be maintained at a uniform rate to avoid fluctuationthe detected values. This is done by drawing a large volume of gas from the trap into the logging unit and diverting the excess needed by the detection systems.

3.7 Show Evaluation

Any evaluation of a gas show with Sperry-Sun Surface Logging Systems is bon gas-in-mud, thus mud samples must be caught at the possum belly and ththrough the Steam-Still prior to injection in the Gas Chromatograph (GC). Thpurpose of using gas-in-mud is so that the background gas entrained in the mthe suction pit can be subtracted from the gas readings of the mud caught atflowline. By using this procedure only the true formation gas readings are plofor show evaluation.

Catching the background suction pit sample and the flowline samples are theimportant steps in show evaluation. If these samples are not caught at the cotime and with the correct method, then all else that follows is totally worthless

3.7.1 Background Suction Pit Mud Sample

There must be a background suction pit mud sample caught prior to any showIdeally, this sample would be caught just before the interval is drilled. This wathe suction pit sample would be of the same mud that was at the bit when thinterval was drilled. This type of timing is next to impossible. So by taking the



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depth the ll. the very

suction pit sample when a drilling break occurs or during regular time intervals during the surface data logger’s tour is the best that can be done.

The sample must be taken from the suction pit, not the return pit since this pitcontain higher gas readings. It is a good idea to catch two samples each time

If the interval to be evaluated is thick enough that more than one complete circulation is completed before the bottom of the zone is encountered, then another set of background mud samples must be caught. After drilling any oiand/or gas zone, an additional amount of gas is entrained in the mud. Only tiand dilution will lower these gas readings.

3.7.2 Flowline Mud Sample

Before catching the mud samples, the surface data logger should have the dinterval of the zone written down and the number of bottles needed to cover interval ready to begin catching the samples. Five foot intervals are recommefor better coverage of the zone.

Ideally the flowline mud sample should be caught at the bell nipple, but sinceis impossible the sample should be caught at the point where the mud streamexits the flowline into the possum belly. This part of the mud stream will contathe most gas.

Places where the sample should not caught are as follows:

1. After the mud has past through the shale shaker.

2. After the mud has past through the gas trap.3. In the corners of the possum belly where there is little mud movement.

When catching the sample, the bottle must be submerged, mouth down, to a of approximately six to eight inches. Then with the bottle still mouth down in mud, the top is then screwed on. The sample bottles should be completely fuKeep the samples, top down, at all times until there is time to run the samplethrough the Steam Still. If not, some of the gas will escape around the top of sample bottle. The samples can be stored until there is time to run them withlittle loss of gas from the bottles if they are handled correctly.



3.7.3 Steam Still

Operating Principles

The Baroid Reflux Unit will strip the mud sample of virtually 100% of the dissolved light hydrocarbons through normal butane. In addition, with the proper technique, the surface data logger is able to collect a completely dry gas sample, free of liquid water and liquid hydrocarbons (Figure 3.26).

Figure 3.26 Reflux Steam Still Assembly

Within the mixing chamber the mud is swept with steam that carries gases and heavier hydrocarbons into the reflux unit. The steam then condenses on the water jacketed surface of the reflux unit. All the condensing water and oil rolls back into the mixing chamber; air, and other gases are swept to the top of the reflux unit and captured there. The inner surface of the condensing jacket is covered with a thin film of condensing water that flows back into the mixing chamber. Droplets of oil will condense and collect on this film of water and also flow back into the mixing chamber. The portion of the reflux unit above this water jacket will remain hot and the walls essentially dry. This distinct separation of condensing water and oil with

Water Resouvior

Coolant Water Pump

Water Level

Boiler

Water LevelGuage

Power Cord

PressureGuage

Water Feed Pump

Pop OffValve

ReturnWater Hose

CondenserWater Hose

Water Feed Line

Injection ScrewGas Removal Port



the gases in the top of the reflux unit eliminates the possibility of the gases redissolving in the condensing water and oil.

The hydrocarbons that are dissolved in the mud sample, are eluted by the steam and come off in the order of their vapor pressures. Only a small quantity of steam is necessary to strip methane from the mud sample; but, larger quantities are needed to strip heavier hydrocarbons. To strip heavier hydrocarbons the reflux unit condenses large amounts of steam which has passed through the mud sample. After reflux action has been carried out for at least four minutes essentially 100% of the normal butane and any lighter hydrocarbons will be stripped from the mud.

During the time that the reflux action is taking place, that is water is flowing through the condensing jacket, all gases will be swept to the top of the reflux unit. When the flow of water in the water jacket is stopped and the refluxing action ceases, gases that are trapped in the top of the reflux unit will disperse throughout the unit as the unit and mixing chamber all come to the same temperature.

Operating Procedure

1. Turn on the Steam Still and allow it to reach its working pressure (minimum of 10 psi, preferably 15 psi).

2. Start the water flowing though the water jacket.3. Insert a glass syringe, without the plunger, through the top of the reflux unit.

Allow all the excess air to be purged from the reflux unit. You should see water and air violently jetting from the syringe. This will take approximately 1 to 2 minutes. When air leaving the chamber is no longer audible, pull the syringe out. Then insert the syringe with the plunger, when air does not move the plunger, the chamber is properly purged.

4. While the reflux unit is purging, agitate the mud sample, by shaking the bottle or by tapping it on the heal of your hand.

5. Drain the excess water from the mixing chamber.6. Withdrawn 5 ml of mud from the sample bottle with a 5 ml syringe, ensure

that a full 5 ml of mud is withdrawn.7. Slowly inject the 5 ml mud sample in the injection valve.8. Set the timer and allow the reflux action to continue for 4 minutes, and do not

allow the boiler pressure to drop below 10 psi.9. Draw into a dry syringe, approximately 1 ml of air. Insert the syringe in the

top of the reflux unit. Force the air into the reflux unit and allow the pressure in the reflux unit to return the air and whatever gases are trapped in the top of the unit. The plunger will rise until steam in the unit begins to condense in the needle of the syringe. At this point, if the plunger does not read 5 ml on the syringe, tapped the plunger with your finger until more gas enters the syringe. This may take several taps, but eventually the syringe will have 5 ml of sample. Once 5 ml of sample is in the syringe, grasp the plunger and barrel of the syringe and remove it from the top of the reflux unit.



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10. Run the syringe under cool water for a minute to completely condense any water. With the needle down, tapped the syringe until all the water is at the bottom, then slowly eject all the water from the syringe.

11. Go to the LS-2000 command terminal and enter the volume factor and depth data (C C 10, 11, 12 and 13).

12. Inject the sample into the chromatograph. Start the chromatograph as soon as the sample is completely injected.

13. Drain the mixing chamber, purge the reflux unit and prepare the next sample.

3.7.4 Show Evaluation of Gas-In-Mud Chromatographs

While it was the development of the Steam Still Reflux unit that made possible the quantitative analysis of hydrocarbons in mud, it has become apparent that the composition rather than the magnitude of the gas in shows is the important factor in interpreting mud log in terms of formation productivity. The relationship of methane to the heavier hydrocarbon components - ethane, propane, butane and pentane, is indicative of gas, oil and water productive potential and, in some cases, the reservoir permeability. A comparison of the ratios of methane to the heavier hydrocarbons from producing wellheads and ppm logs produce striking similarity. In this similarity lies the evidence that the hydrocarbon ratio pattern can be used to predict the productive potential of a reservoir.

Despite the long accepted premise that formation fluids are partially flushed ahead of the bit, ordinarily when formation cuttings are drilled they still retain much of the formation pore fluid. This fluid is released to the mud column as the cuttings travel up the annulus. Most of the formation fluid in the cuttings will be “produced” into the drilling mud during the top 500 feet of hole travel. In the gtrap method of gas analysis the mud sample is diverted to the mechanically operated gas trap to obtain a sample of gas in the mud. The magnitude of thconventional gas show in this case is quantitative only to the gas-in-air sampobtained. The sample is accurately analyzed by the gas chromatograph, but because the sample furnished by the conventional gas trap represents only afraction of the gas present in the mud, and because that fraction is not representative of the total gases in the mud, the results are still only qualitativthe second method, when the Steam Still Reflux unit is used to obtain a gas sample, this analysis will represent almost 100% of the hydrocarbon fractionmethane through pentane that were in the mud sample. This enables the chromatograph analysis to be related quantitatively to the mud and the readinbe reported as parts per million of each hydrocarbon vapor to the mud volum

Because the cuttings from a particular formation “produce” approximately 70%100% of the producible gas they contain into the drilling mud, it is a reasonabassumption that this same formation, if completed, would produce gases of asimilar composition. This idea has led to the ratio plots of methane to each oheavier hydrocarbons from analysis of wellhead samples and ppm logs of



gas-in-mud when the well was drilled. A comparison of the plots led to two ideas: the first being that the magnitude of ratios of methane to each of the heavier hydrocarbons is essentially the same and the second is that the slope of the lines of these plotted ratios are nearly the same.

The similarity seen in the comparison of the plots of the ppm logs and wellhead gas analysis data show that a simple correlation could be made between the Steam Still Reflux samples and interpretation of the in place formation content.

A more detailed study of the correlations of the ratios has indicated the following principles:

1. Productive dry gas zones may show only C1 but abnormally high shows of C1 are usually indicative of saltwater.

2. C1/C2 ratios between 2 and 15 indicate oil.

a Values in the range of 2 to 4 indicate low gravity oil. (10-15 on the API gravity comparison scale.)

b Values in the range 4 to 8 indicate medium gravity oil (15-35 on the API gravity comparison scale.)

c Values in the range of 8 to 15 indicate high gravity oil (35 + on the API gravity comparison scale.)

3. C1/C2 ratios in the 15 to 65 range indicate gas.

a Values in the 15 to 20 range indicates gas rich in heavies, and would most likely be associated with condensate.

b Values in the 20 to 50 range indicates gas rich in mid-ranged hydrocarbons.

c Values in the 50 to 65 range indicates gas rich in the lighter fractions.

4. C1/C2 ratios less than 2 and greater than 65 indicate non-producible hydrocarbons.

a A hydrocarbon with a value less than 2 indicates an oil with a gravity so low that it cannot be produced.

b A hydrocarbon with a value greater than 65 indicates a light gas, most C1, but the low permeability nature of the formation makes it non-producible.

5. The slope of the line of all plotted ratios indicates if the zone will be produce hydrocarbons only or hydrocarbons and water. Line slope also provides some indication as to the formation permeability.

a An all positive slope, up and to the right, indicates hydrocarbons only.



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b If any of the line segments have a negative slope, down and to the right, hydrocarbons and saltwater is indicated.

c A steep line slope indicates reduced permeability and the steeper the slope the lower the permeability. Steep is a relative term but the dashed lines separating the gas, oil, and non-producible areas of the graph are there for comparison.

• Oil plots whose line slope is somewhat steeper than the middle dashed line indicates low permeability.

• Oil plots whose line slope is equal to or less than the middle dashline indicates good permeability.

• Gas plots whose line slope is somewhat steeper than the top dasline indicates low permeability.

• Gas plots whose line slope is equal to or less than the top dashedindicates good permeability.

Procedure for Completing the Zone of Interest Report

The following are the instructions for completing the Sperry-Sun Zone of InteReport (Figure 3.27).

1. “Zone of Interest Report No” - label this blank alphabetically if the report only a zone of interest.

a “Show Report No.” - label this blank numerically if this is a show repo

2. “Depth Interval (MD)/(TVD)” - enter the top and bottom depth values of thZone of Interest or Show, whichever is the case.

3. “Well Name” - enter the well name or OCS-G number if offshore.4. “Location” - enter the offshore block number 5. “Operator” - enter the name of the operating oil company.6. “Hole Diameter” - enter the current bit diameter.7. “Bit Type” - enter the current bit type; “X” the appropriate box.8. “Reported Prepared By” - enter the logger's name who logged the Zone o

Interest or Show.9. “Report Delivered To” - enter the person you delivered the report to. This

would be the geologist even if you verbally gave him the report over the phone.

10. “Date” - abbreviate or spell out the month rather than using a number val11. “Time” - enter the hours and minutes using a 24 hour clock.12. “New Orders” - what the rig operation was after detecting the show.13. “Max ROP @ _____ ft” - depth where the maximum ROP occurred.14. “Max Gas @ _____ ft” - depth where the maximum gas occurred.15. “Max Cl @ _____ ft” - depth where the maximum chlorides occurred.



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16. “MW in (before, during, after)” - suction pit mud weight.17. “MW out (before, during, after)” - flowline mud weight, including any cut.18. “Avg. WOB (before, during, after)” - average weight-on-bit.19. “Avg. ROP (before, during, after)” - average rotary speed.20. “Avg. GPM (before, during, after)” - average mud flow rate.21. “Avg. ROP (before, during, after)” - average rate of penetration, mark the

appropriate box for feet per hour or minutes per foot.22. “Max ROP” - the maximum rate of penetration during the interval.23. “Avg Gas (before, during, after)” - average gas reading, mark the appropr

box for either units or per cent gas.24. “Max Gas” - the maximum gas reading during the interval.25. “Avg Cl (before, during, after)” - the average chlorides (use K to indicate

thousands of ppm's)26. “Max Cl” - the maximum chloride reading27. “Avg. C1 (before, during, after)” - the average C1 readings from the

chromatograph.28. “Avg C2 (before, during, after)” - the average C2 readings from the

chromatograph.29. “Avg C3 (before, during, after)” - the average C3 readings from the

chromatograph.30. “Avg C4 (before, during, after)” - the average total C4 reading from the

chromatograph.31. “Avg C5 (before, during, after)” - the average total C5 readings from the

chromatograph.32. “PPM at Max Gas” - the parts per million of each gas component at the

maximum gas reading.

Note: If the gas readings do not contain a component, enter “NA” for thacomponent, do not leave it blank.

33. “At Max Gas, the visual sample percentages were: ____ % ____” enter tcuttings percentages and types seen in the interval (up to four types andpercentages).

34. “The reservoir rock was a ____” - enter the reservoir rock of the zone of interest or show.

35. “-colored ____” - enter the color or colors of the reservoir rock.36. “The gain (crystal) size was ____” - the size or sizes of the reservoir rock37. “and the grain shape was ____” - the shape of the grains of the reservoir38. “Approximate visual porosity was ____%” - estimate the visual porosity o

the reservoir rock.39. “and the visual permeability was ____” - estimate the visual permeability

the reservoir rock.40. “Grain sorting was ____” - enter the sorting of the grains or crystal (i.e., p

moderate, fair, well).



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41. “and the rock cement was ____” - if the reservoir rock was cemented, enthe type of cement holding the fragments together.

42. “The porosity type was ____” - enter the type of porosity of the reservoir r(i.e., intergranular, intraparticle).

43. “and the secondary components in the rock fragments were ____” enter the secondary components in the rock fragments of the reservoir rock, nosecondary rock types in the entire sample.

44. “The rock hardness was ____” - the hardness of the reservoir rock.45. “and the sample contamination was ____” any type of contamination of th

sample (i.e., metal filings, pipe dope).46. “Depth” - enter the depth of any gas-in-air chromatograph readings that w

taken during the interval.47. “Gas” - enter the mud gas reading for the above depth (mark the appropr

box for units or percent readings).48. “C1” - enter the C1 ppm reading (in thousands) for the above depth.49. “C2” - enter the C2 ppm reading for the above depth.50. “C3” - enter the C3 ppm reading for the above depth.51. “C4” - enter the total C4 ppm reading for the above depth.52. “C5” - enter the total C5 ppm reading for the above depth.53. “Oil Fluor y/n” - mark the blank with a yes or no if any oil fluorescence wa

noted in the sample for the above depth.54. “Cut Fluor y/n” - mark the blank with a yes or no if any cut fluorescence w

noted in the sample for the above depth. 55. “The liquid hydrocarbon was first detected at ____ ft” - the top depth that

liquid hydrocarbons were detected. 56. “and continued through ____ ft” - the bottom depth that any liquid

hydrocarbons were detected. 57. “The liquid phase of the mud was ____.” - enter the base of the drilling flu

(i.e., water, mineral oil).58. “The liquid hydrocarbon occurred in the form of ____” enter the type of

liquid hydrocarbon detected (i.e., gas condensate, oil).59. “and was present in the ____.” - was the liquid hydrocarbons detected in

mud, washed cuttings and/or unwashed cuttings. 60. “When the ____ (was/were) mixed with water and studied in the UV box,

enter which of the three above samples were mixed with water and studiethe UV box.

61. “the liquid hydrocarbon covered ____% of the surface of the water” - entewhat percent of the water fluoresced.

62. “The oil was ____ in color,” - enter the color of the oil as noted in unwashcuttings mixed with water.

63. “exhibited a ____ fluorescence” - enter the color of the oil fluorescence anoted in the unwashed cuttings mixed with water.

64. “and had an approximate API gravity of ____;” - enter the API gravity closto the color of the oil fluorescence as compared to the API Gravity Scale.



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65. “odor was ____ and staining (was/was not) present” - enter any hydrocarodor that was noted (i.e., none, very faint, faint, strong). Cross out the appropriate response pertaining to any staining that may have occurred isamples.

66. “The cuttings exhibited a ____ cut” - enter the type of solvent cut (i.e., streaming, blooming, crush).

67. “that was ____ in color” - enter the color of the solvent cut (i.e., clear, stralight brown, brown).

68. “with a ____ fluorescence.” - enter the color of the cut (i.e., cream/white, yellow/green).

Note: If no liquid hydrocarbons were detected in the interval, enter “NA”for each blank.

69. “Logger's Opinion of the Show Interval” - the logger should enter any othpertinent information concerning the interval at this point.

70. “100% Gas-In-Air = ____ units” - enter the gas scale for 100% gas, (i.e., 3000, 5000).



Figure 3.27 Sperry-Sun Surface Logging Systems Zone of Interest Report



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Procedure for Completing the Show Report

The following are the instructions for completing the Sperry-Sun Show Report (Figure 3.28).

1. “Show Report No.” - label this blank numerically

2. “Depth Interval (MD)/(TVD)” - enter the top and bottom depth values of thshow report.

3. “Well Name” - enter the well name or OCS-G number if offshore.4. “Location” - enter the offshore block number.5. “Operator” - enter the name of the operating oil company.6. “Report Prepared By” - enter the logger's name who logged the show.7. “Report Delivered To” - enter the person you delivered the report to. This

would be the geologist even if you verbally gave him the report over the phone.

8. “Date” - abbreviate or spell out the month rather than using a number val9. “Time” - enter the hours and minutes using a 24 hour clock.10. “the production of this zone is deemed to be ____.” based on your

interpretation of all Steam Still hydrocarbon ratio plots of the zone enter eigas, oil, water, non-producible hydrocarbons or any combination.

11. “At approximately ____ feet there is” - again referring to all the Steam Stihydrocarbon ratio plots in zone, enter the approximate measured depth wthe fluid content of the zone changed. If the zone was 100% gas or oil, e“NA” in all the blanks.

12. “a ____/____ contact” - if the zone contains gas and/or, oil and/or water, ethe type of contact.

13. “(and a ____/____ contact” - treat as above.14. “at approximately ____ feet)” - enter the measured depth of the second f

content change of the reservoir.15. “for a total of ____ feet” - enter the total footage of the first fluid type of th

reservoir.16. “of ____ show” - enter the first fluid type if the reservoir contains more tha

one fluid type.17. “(and ____ feet” - if the reservoir contains more than one fluid type, enter

total footage of the second fluid type. If the reservoir contains only one flutype, enter “NA”.

18. “of ____ show.)” - enter the second fluid type if the reservoir contains mothan one fluid. Enter “NA” if the reservoir contains only one fluid type.

19. “DEPTH” - enter the measured depth where the gas for this particular plooriginated from.

20. “GAS” - marked the appropriate box for either units or percent and enter value in this blank.

21. “MUD CHLORIDES (ppm)” - enter the mud chlorides for the plot measuredepth.

22. “FLOWLINE ppm” - enter the flowline ppm readings for the plot depth. If any components are not present, enter “NA”.



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23. “SUCTION ppm” - enter the suction pit ppm readings for the plot depth. Iany components are not present, enter “NA”.

24. “SHOW ppm” - subtract the suction ppm's from the flowline ppm's and enthe results here.

25. “HYDROCARBON RATIOS” - enter the C1/C2, C1/C3, etc. ratios here.26. “PRODUCTION ANALYSIS” - mark the appropriate box for the productio

type the ratios indicate.

Figure 3.28 Sperry-Sun Surface Logging Systems Show Report


Show EvaluationDetermination of Oil in the Cuttings

be

3.8 Determination of Oil in the Cuttings

Place about a tablespoon of the wet washed cuttings caught in the 80-mesh sieve plus some of the large sand or limestone chips remaining on the 5-mm sieve into a stainless sample tray. Drain off the excess water by tipping the tray and place the lip of the tray on the edge of the sink or place a finger on the lip of the tray to speed drainage. Next, place the tray containing the sample in the UV box for inspection. With the door closed examine the sample for fluorescence. Be sure to allow time for your eyes to become accustomed to the darkness of the box. Differentiate between oil and mineral fluorescence. Next, separate out the pieces exhibiting oil fluorescence and put them into one spot in the spot plate. If there is any doubt as to whether a new fluorescence is oil or mineral, place several of the fluorescent cuttings in a spot plate. Place the spot plate under a microscope and examine the cuttings as separated to learn the appearance of the mineral which exhibited various fluorescence. Place the spot dish into the UV box and cover the sample with chlorothene solvent. Use no more solvent than necessary to cover the cutting. In cross-examining the sample between the UV box and microscope, the logger should become aware of the relationship of the fluorescence and the type of material in the sample which is fluorescing.

In fast drilling areas where sand is likely to be the reservoir rock an alternative method of checking for oil in the sample of cuttings is to place a tablespoon of the cuttings in an evaporating dish, place this under the UV light, pour chlorothene over the aggregate sample and watch for cut. If a cut is obtained find the source of the cut and examine thoroughly. If fluorescence is found, first place the fluorescing piece on a spot plate and cover with solvent. This method has merit when looking for oil in carbonate rocks and should not be depended upon.

Oil has the convenient property of fluorescing under a UV light. The nature and porosity of sand makes sand an ideal holding medium for oil. Consequently sand cuttings can usually be depended upon to exhibit fluorescence if they contain oil. However, if they contain little oil, or the oil is of a very low gravity, this fluorescence may not be apparent. The use of a leaching agent on the cuttings serves to differentiate between oil and mineral fluorescence and to bring oil out of the cutting from which it would otherwise not be apparent.

In examining for an oil cut place the sample under the UV light and place the chlorothene on the sample while observing through the lens of the UV box. Oils will dissolve in the solvent, mineral fluorescence will not. Watch to see if the solvent takes on a fluorescent color from the cuttings or if stringers of fluorescing oil may be seen streaming from particular cuttings. If it does not, oil is not being “cut” from the cuttings by the solvent. Crush the sample to determine if oil mayliberated from the inner pores.


Show EvaluationEvaluation of a Cuttings Oil Show

Allow the solvent to evaporate; if oil was cut from the sample a fluorescent ring will be left in the dish. A blank solvent spot may be used for comparison. Samples should be checked again for fluorescence after they have dried. Some oils are more easily seen under the UV light in dry samples.

Examination of carbonate cuttings requires a somewhat different approach and additional considerations. Foremost is the fact that almost all limestones and dolomites exhibit some kind of mineral fluorescence. For this reason oil determination must depend almost entirely upon a fluorescent cut in a leaching agent rather than on fluorescence of untreated cuttings. The type of porosity usually found in carbonate rock is such that the cuttings themselves may be dense and have only one face that is part of the wall or a crystal-lined fracture that has been in contact with the oil. The cuttings in the sample tray should be studied for new and different types of fluorescence and these pieces picked out and placed in the spot plate. Under the microscope, pick out the cuttings indicating porosity and put them in the spot plate. Place the spot plate in the UV box and while observing, carefully spray chlorothene onto the cuttings. A strong cut should not be expected. In fact, an oil cut consists of no more than a flash or fluorescent leaching only immediately after application of the solvent. Add 10% hydrochloric acid to break down the cuttings and help liberate any oil present. Allow the solvent to evaporate and examine for a fluorescent ring.

Do not use solvent from rubber stoppered bottles or medicine droppers as the rubber will add fluorescence to the solvent, making it unfit for oil determination. A hypodermic syringe is best for dispersing the chlorothene, a glass dispensing bottle may be used. Periodically check the solvent for contamination.

Rig oils and greases must be examined for their fluorescence. Care must be exercised to determine that the fluorescence or cut is coming from within pieces of sample and not just from the overall surface. This will reduce chances of mistaking rig oil for crude oil. Before the oil in the cuttings evaluation entry is completed on the data sheet, the cuttings should also be examined under the microscope to obtain some idea of the sample porosity, staining and oil source.

3.9 Evaluation of a Cuttings Oil Show

Primarily, there are two main factors that should be taken into consideration in evaluating an oil show in the cuttings; the type of fluorescence and the percentage of the total cuttings sample which exhibit such fluorescence. The type of fluorescence gives some indication of the quality of the show and the type of formation from which the cuttings came, and the percentage of the cuttings exhibiting the fluorescence from a particular zone represent the massiveness and extent of the formation from which they came.



Qualifying factors with which the above results should be tempered would be dispersion of the analyzed sample in the mud column which is in itself dependent on depth, mud characteristics, actual grain size, density, hole conditions and the degree of cementation of the individual particles of the cuttings. In spite of the mechanical factors, the quality of the show and massiveness of the member containing the show are the important reservoir characteristics to be gained from this analysis of the cuttings.

Therefore, the evaluation of the show in the cuttings becomes a matter of first evaluating the show within individual cuttings which do exhibit a show and then interpreting that evaluation in the light of the factors affecting the percentage of these cuttings present in the sample. This allows the logger to arrive at the following table for evaluation or rating of the show:

The Table 3.1 is a chart that applies considerations of both quality and quantity as a guide for placing a rating on the above described oil show in the cuttings. It is conceded that specific knowledge of and experience in a particular area should supersede the application of this chart. However, in the absence of such information or any other circumstance surrounding the occurrence of the show, the logger should use the chart to arrive at a final evaluation to place the show of a cuttings sample. Also, he should take into consideration any extraordinary circumstances that temper his rating. Tar or deal oil alone should never be give a value greater than 1/2, regardless of the amount present. A TRACE of live crude oil should never be given a value less than 1.

Theoretically, if a 2-foot thick sand is drilled, the samples returning to the surface would contain 100% of this sand until the end of the interval passes over the shaker and then the samples would abruptly change to whatever follows the sand. Therefore, if the sand contained a GOOD SHOW it should be logged accordingly for two feet, though the formation might be barren above and below. In practice, however, zones are never this clearly defined even at a shallow depth. Actually, at a fairly shallow depth, the hypothetical sample above might indicate only 50% sand for the two foot interval with the balance of the sand from this interval

Table 3.1 Quality of Show in Those Cuttings Which Exhibit a Show

Percentage of show-containing cuttings in the sample

Little or no porosity, little or no staining, weak fluorescence, cuts only after crushing

Some visible porosity, fair visible porosity, fair fluorescence, cuts by discoloration

Good porosity, good visible, staining, good fluorescence, streaming cut

Few pieces - 25% Trace Trace-1 Show-2

25% - 50% Trace-1 Show-2 Show-3

50% - 75% Trace-1 Show-2 Good show-4

More than 75% Show-2 Show-3 Good show-4



trailing off showing decreasing percentages for the next several samples. In a deeper well, the sample from this same sand might indicate only 25% of the sand the balance will trail off over an even longer interval. Thus, it is easy to see that evaluations based on percentages alone will lead to an erroneous representation. More correctly, the quality of the show should be logged, letting the depth intervals delineate the thickness or extent.

Cuttings oil shows can be described using Table 3.2 below and the following guide:

1. Percentage stain and distribution

2. Color of the stain3. Intensity and distribution of fluorescence4. Color of fluorescence5. Type of cut

Table 3.2 Cutting Oil Show Descriptions

Stain Distribution

PoorFairGoodNo visible stain

pfrgn vis stn

UniformScatteredSpottyStreakedFracture

uniscatspstrfrac

Shade Hue

Very lightLightMediumDarkVery dark

v ltltmdkv dk

GreenYellowBrownBlack

gnyelbrnblk

Fluorescence intensity Distribution

FaintDullBrightNo fluorescence

fntdullbrin flor

UniformScatteredSpottyStreakedFracture

uniscatspstrfrac

Shade Hue

Very lightLightMediumDarkVery dark

v ltltmdkv dk

BlueWhiteYellowOrangeGoldBrown

blwhyelorgoldbrn


Show EvaluationDetermination and Evaluation of an Oil Show from Mud

Cuts fall into three categories:

3.10 Determination and Evaluation of an Oil Show from Mud

A small sample of mud should be caught at the same time as the cuttings sample. The sample should be caught as close to the discharge of the flowline as possible, the sample should never be taken from the discharge of the gas trap or after the mud has passed through the shaker screens. To prepare the mud sample for viewing under UV light, fill a pyrex sample dish about one third full of mud and add sufficient water to make the mud thin.

Oil shows may be found be examining the returning drilling mud under an ultraviolet light. In some cases this has resulted in the finding of new oil fields. It is possible to detect minute amounts of oil in drilling muds by this manner. In some experiments with known laboratory mixed samples, as little as 5 parts per

1 Streaming cuts These are the quickest to develop and are the ones in which the oil fluorescence can be seen to stream out of the cuttings.

ImmediateFastSlowLazy

immfstslwlazy

StreamingCut

strmcut

2 Discoloration cuts These are slower to develop than streaming cuts and are the ones where the solvent becomes discolored without any obvious source points for the producing the discoloration.

Very slowSlowModerateFast

v slwslwmodfst

MilkyHazy

mlkyhzy

3 Crush cuts These are the cuts produced by crushing the cuttings, either prior to adding the solvent or in the case of a very slow discoloration cut/no cut after the addition of the solvent. A sample with a good crush cut and a very slow discoloration may be interpreted as having a low permeability.

PoorFairGood

pfrg

Crush crsh



f the ud e

te or

the n

e

ur

de

t an ence

million (ppm) oil-in-mud were detected with UV light; 15 ppm oil-in-mud were easily detected.

The mud sample for study must be collected at the point of nearest access to the well head. Usually this point is at the flowline. This is necessary in order that the mud will have a minimum exposure to the atmosphere. The sample must never be taken from the discharge of the trap or after passing through the shaker screens. Fill a pyrex mud sample dish about one third full of mud. Add sufficient water (of no fluorescent impurities) to make the mud thin. Place the sample in the UV box immediately and with the door closed, look for distillate fluorescence which usually disappears almost as soon as it reaches the surface. Stir several seconds with a glass rod while examining the mud sample under the UV light. In stirring, be sure to stir around the edges of the dish near the surface of the mud as some crude oils tend to adhere to the dish. Be sure your eyes become accustomed to the darkness of the viewing box before stirring and examining the sample. This is especially important on bright, sunny days. The mud sample should be allowed to stand until the time for collecting the next sample and another examination of the sample made for any new fluorescence.

In many cases oil appears to blossom and spread on the surface of the mud. High gravity crude oil shows usually appear as droplets which seem to “pop out” omud followed by and leaving a flower of fluorescence on the surface of the msample. An approximation of the gravity of the oil comprising the show may bmade from the color and type of fluorescence. The color may range from whivery light blue for high gravity; dark yellow or almost brown fro that of low gravity crude. The fluorescence of paraffin base crude will usually fall more inblue range while that of asphaltic crude will exhibit more of the yellow to browcast.

Since rig oil and greases will fluoresce under the UV light, a collection of thesoils and greases on a small stick will help to identify fluorescence from thesesources. A white light is provided in the UV box to assist in identifying such contamination as well as to assist in the complete examination.

Each time the UV box is turned on, it should be checked to ensure that all fotubes are burning. The ultraviolet light in the UV box must be checked periodically and sufficient intensity maintained.

Because of contamination by rig oils and grease and by oil recirculated in themud, it is necessary to examine mud samples at regular intervals, even whilecoring, in order to locate any new fluorescence which might be caused by cruoil; otherwise, the new fluorescence might go unnoticed because of the contaminating fluorescence from oils and grease.

The use of different types of oils in the making of oil emulsion muds, makes iimperative that the mud be examined at regular intervals. Only by doing so cthe fluorescence from a new show be distinguished from the normal fluoresc



of the mud. Arrangements should be made with the mud engineer to notify the logger of any new additions of oil to the mud.

Sometimes, cuttings samples are not readily available because of sand reaching the surface being finely divided, lost circulation material, hole conditions or fast drilling rates. In such cases, it is necessary to rely more on mud samples and in order to do so, the logger must have been examining the mud samples regularly. Accurate and logical evaluation of oil shows in the drilling mud is realized mainly by experience. Numerical evaluation of the oil shows in mud is normally a matter of visual comparison of a particular show with the known results of other shows that have been observed. The logger should have previously gained as much information from those already observed within the same or closely related areas.

The oil shows are evaluated on the basis of the percentage of the mud covered by oil and tempered by such things as drilling rate, depth, gas readings, lithology, rate of mud circulation and mud properties. In the interest of maintaining as much uniformity as possible between various logging jobs and between individuals, the evaluation below should be used:

A TRACE of live crude should never be given a value of less than T. A rating of a GOOD SHOW will be rare, and should only be given to a show accompanied by a good drilling break, increase in gas readings, and a good show of oil in the cuttings. No more than a TRACE should be given a show accompanied by only a small amount of gas increase or no increase al all.

These suggestions are not intended as ironclad rules, since practices and greater knowledge of certain areas may dictate variations. They are intended to serve only as a guideline to standardization of the evaluation given to a show throughout all operating areas and as aids to the logger to serve in the gathering of information on remote wildcats where little previous information is known.

Table 3.3 Fluorescence Evaluation

% Surface Fluorescence

Trace Up to 25%

Show 25% to 50%

Good Show 50% to 75%


Well ControlCauses of Kicks and Warning Signs of Kicks

Chapter 4 Well Control

The control of formation pressure during drilling, completion and work over operations.

The loss of well control is often a subtle and unnoticed event until it has suddenly become a threat to life, property and environment. Today, wells are being drilled at faster penetration rates, with lower mud weights, deeper, and in deeper water than ever before. Your ability to recognize the warning signs of kicks and potential blowouts, and to assist with the execution of correct and safe well control practices is important. Your life, as well as the success of the operation in which you are involved, may depend upon your knowledge of well control technology.

4.1 Causes of Kicks and Warning Signs of Kicks

The control of kicks and blowouts is important, but our first consideration is to avoid a kick or a blowout situation. Some kicks and blowouts are inevitable, but a concerted effort needs to be made to minimize these occurrences. If a kick develops, it is imperative that it be detected early in order to minimize the amount of influx of formation fluids. The greater the amount of influx, the more difficult the well becomes to control. An understanding and a watchful eye towards the kick warning signal are essential.

In order to begin any meaningful discussion of the causes and warning signs of kicks, it is necessary to define the terms kicks and blowout.

A kick may be defined as a condition which exists when the formation pressure exceeds the hydrostatic pressure exerted by the drilling fluid, allowing an influx of formation fluids into the wellbore.

A blowout is an uncontrolled influx of formation fluids into the wellbore. A kick is not a blowout, but if it is improperly handled, it may become a blowout.

A condition which exists when the formation pressure is less than the hydrostatic pressure of the mud plus any pressure losses and imposed pressure is known as overbalance. When the formation pressure exceeds the total pressure exerted by the mud column, friction losses, and imposed pressures, then this condition is known as underbalance.

There are a number of factors which determine the severity of a kick. In order to allow fluid to flow from the formation into the wellbore, there must be sufficient formation permeability and porosity for this to occur. Permeability is a term used to describe the ability of a fluid to move through the rock, and porosity is a term



used to measure the amount of space in the rock that contains fluid. Sand generally has a greater potential for causing a kick than does a shale because, (1) the volume of rock occupied by fluid is greater than in a shale (porosity), and (2) the ability of the fluid to move through rock (permeability) is higher than it is for a shale. The third factor controlling kick severity is the amount of underbalance. The greater the amount of underbalance, the easier it is for formation fluids to flow from the formation into the wellbore.

Kicks are commonly labeled by several different methods. For instance, the same kick may be labeled at various times as a 20-barrel kick (the amount of influx that occurred prior to the time the well was shut-in), a gas kick (the type of fluid influx), or a 1 ppg kick (the increase in mud weight necessary to control the kick).

4.1.1 Causes of Kicks

Failure to Keep the Hole Full

A survey, which was taken in 1971, indicated that 44% of all blowouts occurred while pipe was being tripped, and about 41% of the blowouts occurred while drilling operation were progressing. Failure to fill the hole during a trip is a common occurrence. As pipe is removed from the well, the fluid level in the wellbore falls because the metal in the drill pipe has displaced a certain amount of mud. With the pipe no longer in the hole, mud itself must fill the void which has been created by removing the pipe. If no addition mud is pumped into the well, the volume of fluid in the wellbore remains constant. A volume of mud equal to the pipe displacement has filled the void created by removing the pipe, so that the fluid level in the hole must drop.

If the fluid level drops enough to decrease the hydrostatic head of the mud to a point where the formation pressure exceeds the mud hydrostatic pressure, influx of formation fluids into the wellbore will occur.

We need to see whether or not this drop in hydrostatic pressure is significant. Assume the following hole data:

TVD = 9,000 feet

MW = 10.0 ppg

Drill pipe dimensions = 4.5 inches × 3.826 inches

Hole Size = 8.5 inches

Formation pressure = 9.9 ppg equivalent

Drill collars = 7 inches × 2.5 inches



tion

Assume the driller wants to pull 5 stands (94 ft/stand) between hole fills. Can he do so safely?

Solution: In order to find the answer to this problem, it is necessary to compute the fluid level drop in the hole after he has pulled 5 stands with filling the hole.

1. Calculate the total fluid displaced by 5 stands of drill pipe. Drill pipe displacement,

bbl/ft = (OD2 - ID2) × .0009714= (4.52 - 3.8262) × .0009714= .00545 bbl/ft

The total amount of pipe being pulled is 5 stands.

5 stands × 94 ft/stand = 470 ft.

So the total pipe length being pulled between fills is 470 feet.

The total fluid displaced by 470 feet of drill pipe is:

470 ft × .00545 bbl/ft = 2.562 bbl.

2. How many feet does 2.562 barrels fill?

Annular capacity (bbl/ft) = (Hole ID2 - Pipe OD2) × .0009714

bbl/ft = (8.52 - 4.52) × .0009714= .0505 bbl/ft

Drill Pipe capacity (bbl/ft) = Pipe ID2 × .0009714

= 3.8622 × .0009714

= .0145 bbl/ft

Fluid level drop (ft) =

=

= 39.5 feet

3. What is the pressure reduction?

The fluid level has dropped 79 feet. Therefore, the hydrostatic head reducis:

Mud displaced (bbl)

Annular capacity (bbl/ft) + DC capacity (bbl/ft)

2.562 bbl

0.0144 bbl/ft +0.0505 bbl/ft



t.

ead

ot

s, d.

re,

s the

he

39.5 ft × .052 × 10.0 ppg = 21 psi

4. Compute the hydrostatic head of 9,000 feet of 10.0 ppg mud.

HH = .052 × 10.0 ppg × 9,000 ft= 4680 psi

The formation pressure has been previously given as a 9.9 ppg equivalenCalculate the formation pressure in psi.

Formation pressure (psi) = 9.9 ppg × .052 × 9,000 feet= 4633 psi

Since the driller pulled 5 stands without filling the hole, the hydrostatic pressure of the fluid in the hole was reduced by 21 psi. The hydrostatic hof the mud now in the hole is:

4,680 psi - 21 psi = 4,659 psi

The difference between the new hydrostatic head (HH of mud with hole nfull) and the formation pressure is:

4,659 psi - 4,633 psi = 26 psi

Twenty-six psi is the safety factor, working for the driller while pulling 5 stands between hole fills. Each set of conditions requires separate calculations, so this analysis must be carried out on a case-by-case basiconsidering each of the different pipe sizes and hole diameters to be use

Drill collars displace considerably more hole fluid than does drill pipe. Therefowhen drill collars (or Hevi-Wate) is being pulled, more frequent hole fills are required than for drill pipe. Assume the hole data being used in this example isame as that used in the previous example.

Assume the driller wants to pull 3 stands of drill collars between hole fills. Cando so safely?

Solution:

1. Calculate the total fluid displaced by 3 stands (90 ft/stand) of drill collars

DC displacement = (OD2 - ID2) × .0009714= (72 - 2.52) × .0009714= .0415 bbl/ft DC displacement

Total displacement = 90 ft/stand × 3 × .0415 bbl/ft= 11.2 bbl



p?

tic sed

2. Compute the feet filled (fluid drop) by 11.2 barrels.

Annular capacity (bbl/ft) = (Hole ID2 - DC OD2) × .0009714= (8.52 - 72) × .0009714= .0026 bbl/ft

DC capacity = ID2 × .0009714= 2.52 × .0009714= .006 (bbl/ft)

Fluid level drop =

= 11.2 bbl .0285 bbl/ft

= 392 ft

3. What is the hydrostatic pressure reduction as a result of the fluid level dro

The fluid level has dropped 293 feet. Hence, the hydrostatic pressure reduction is:

392 ft. × .052 × 10.0 ppg = 204 psi

The formation pressure is given as being a 9.9 ppg equivalent.

FP = .052 × 9.9 ppg × 9,000 feet

= 4,633 psi

The hydrostatic head of the mud in the hole is now equal to the hydrostahead of the mud when the hole was full minus the pressure reduction cauby the pipe displacement.

HH = .052 × 10.0 ppg × 9,000 feet

= 4,680 psi

The hydrostatic head of the mud with the hole not full is:

HH - pressure reduction (psi)

4,680 psi - 204 psi = 4,476 psi

Fluid displaced (bbl)

Annular capacity (bbl/ft) + DC capacity (bbl/ft)



Therefore, the hydrostatic head of mud in the hole after pulling 3 stands of drill collars is 4,476 psi, and our formation pressure is 4,633 psi. Thus, leading to an influx of formation fluids.

The lesson to this story is two-fold:

1. Frequent hole fills while pulling drill pipe is a good practice, especially when drilling close to balance. The MMS requires that the hole be filled with fluid before a bottom hole pressure reduction of 75 psi occurs or no more than 5 stands of drill pipe, whichever provides the least reduction.

2. Pipe which displaces a lot of mud due to its wall thickness (such as drill collars or Hevi-Wate) will demand more frequent hole fills, not only to comply with the law, but for personnel and rig safety as well. A good practice is to fill the hole every stand or continuously when pulling large drill collars or Hevi-Wate drill pipe.

The MMS requires that the hole be filled with accurately measured volumes of mud. This implies that two things must be done: (1) the pipe displacement must be calculated, and (2) a method must be devised to accurately measure the mud volume used to fill the hole. The two most common methods for doing this are trip tanks and pump stroke counters.

A trip tank is a small tank with an accurate calibration scale which can be used to measure the amount of mud entering and leaving the tank. On some trip tanks, the calibration scale is accurate enough to read mud volumes to the nearest tenth of a barrel. The trip tank may be placed at a height greater than that of the flowline to allow it to fill the hole by gravity feed. If the trip tank is not placed at the flowline height or higher, a centrifugal pump may be attached to the trip tank so that the pump can pump mud continuously through a fillup line. Another line is placed on the BOP stack at a height slightly greater than that of the fillup line. The trip tank pumps mud into the annulus continuously and any overflow is returned to the trip tank via the return line (Figure 4.1).

The volume required to fill the hole can be easily seen by using the calibration scale and recording the drop in the fluid level of the trip tank as pipe is removed from the well.

The second method commonly used is to periodically fill the well with mud using the rig pump and to count the number of strokes the pump runs while filling the hole. The number of strokes that will be required to fill the hole should be predetermined before a trip is begun by using the following formula:

Strokes to fill = Pipe displacement volume (bbl)pump output (bbl/stk)

Example: Suppose the driller wishes to pull 5 stands of drill pipe between hole fills. The pipe displacement volume for the 5 stands is 3 barrels, and



the rig pump output is .2 bbl/stk. How many pump strokes are required to fill the hole?

Strokes to fill = .3 bbl = 15 strokes.2 bbl/stk

Figure 4.1 Trip Tank

If the hole fails to take the calculated amount of mud (either by strokes or by level decrease in a trip tank), formation fluids are entering the well and corrective action should be taken immediately.

Swab Pressure

Swab pressure is pressure created by pulling the drill string from the hole. Swab pressure acts like a negative hydrostatic pressure, thus causing reduced bottom hole pressures (BHP). If the BHP becomes less than the formation pressure, an influx of formation fluids can occur. There are a number of factors upon which swab pressures depend. Some of these are:

1. Speed at which the pipe is pulled.



oint nt

ab

the us

s than

ore. ured

ource the or

2. Mud flow properties, especially the yield point and gel strength.3. Hole geometry.4. Balled-up equipment (bits, collars, stabilizers.

Hole swabbing is very easy to recognize. First a hook load indicator may show more drill string weight than what the string actually weighs. Although drag may depend on any number of factors, it is an immediate tip-off that potential hole swabbing can be taking place. Hole swabbing can be detected by watching the fluid level as pipe is pulled from the hole. If the fluid level does not fall enough or if the fluid seems to be following the pipe as the pipe is pulled, swabbing is taking place. Again some remedial action must be taken immediately. Swab pressures can become severe enough at times so that a BHP reduction of several hundred psi may occur. This is a very common phenomenon in gumbo shale and happens because some of the drilling assembly has become caked with gumbo. As the pipe is removed from the hole, the balling that has taken place on the drilling assembly acts like a piston, which impedes the flow of mud required to fill the void created as the pipe was pulled.

It is common practice to pull up into the casing, put the rig in “high-high gear”and gel that pipe “on the floor” in a hurry. Swab pressure is exerted at every pin the open hole below the bit. Pipe speed should only be increased if sufficieswab pressure versus pipe speed data is available with which to determine maximum safe pipe speeds. Remember bottom hole pressure is critical, if swpressure reduces it below formation pressure, a kick is eminent.

Lost Circulation

Lost circulation may be a cause of kicks. If lost returns occur, the fluid level inhole begins to fall. The length of the fluid column in the hole is decreased, thcausing the hydrostatic pressure of the mud in the hole to decrease. If the hydrostatic pressure of the mud decreases to the point where it becomes lesthe formation pressure, a potential kick situation exists. If the lost circulation problem goes undetected, a large amount of fluid influx can occur in the wellbIt is therefore a good practice to attempt to keep the annulus filled with measvolumes of water.

Gas Cut Mud

Gas cut mud may cause a kick, although it does not happen very often. The sof gas in the mud is generally the formation which the bit itself has cut up. In oil field, this phenomenon is variously referred to as “drill gas,” “cuttings gas,”“core volume cutting.”



Most gas expansion takes place near the surface of the well. If a large diameter hole is being drilled at a high rate of penetration (as in a 171/2-inch surface hole offshore), the amount of gas cut up by the bit itself can be considerable. Expansion of the gas occurs as the gas nears the surface, so the hydrostatic head of the mud is reduced. If the hydrostatic head is reduced to a value lower than the formation pressure, a kick can occur. However, the hydrostatic head reduction caused on bottom by gas cut mud is generally not a significant value. The surface indication of gas cut mud often cause more concern than the situation warrants. The main concern when dealing with gas cut mud should be to make certain that the surface facilities are adequate to keep cut mud from being pumped back down the hole. An operational degasser is a necessity when dealing with gas cut mud.

There are two major types of degassers. One is the atmospheric type, often called a gas separator or gas buster. Its construction is such that it can be constructed at the rig site and has a large mud handling capacity. It can handle the volumes of mud normally pumped in circulating the well or the volumes pumped during a well-kill operation. The atmospheric degasser is usually the first treatment which gas cut mud receives at the surface. In the atmospheric degasser, mud falls over baffles which tend to break the gas bubbles out of the mud. The gas is vented to the atmosphere through a 6-inch or larger gas outlet.

The second common type of degasser is the vacuum type. Mud enters one side of the degasser and is pulled up into a chamber in which a partial vacuum exists. The gas is forced out of the mud by gravity segregation in the chamber under a partial vacuum. The mud flows back into the pits and the gas from the mud is vented to the atmosphere. The vacuum degasser is more effective than the atmospheric degasser, but its construction complexity and maintenance requirements are higher than those for the atmospheric degasser.

Water and Oil Cut Mud. Water and oil cut mud can cause a kick. The mud weight reduction at the surface caused by an influx or other additions of water and oil considerably decreases hydrostatic pressure in the wellbore. A .5 ppg cut at the surface implies that all the mud in the borehole is cut by at least .5 ppg. A .5 ppg cut on a 10,000-foot well reduces the bottom hole pressure by 260 psi.

Insufficient Mud Density - Abnormal Pressure

Although most blowouts or kicks occur while drill pipe is being tripped, insufficient mud density is the second most common cause of a kick. About 41% of all blowouts occur while drilling ahead, which implies that the mud density in use at the time was not sufficient to control the formation pressure. In the Gulf Coast area, most wells are drilled with higher than a 9.0 ppg mud weight. The normal formation pressure in the Gulf Coast area is assumed to be 9.0 ppg. If a 9.0 ppg or greater mud density is insufficient to control formation pressure, then



d, it

ing

pipe ole.

ber,

ng a are

ay ens

abnormal formation pressures exist. Insufficient mud density and abnormal formation pressures often go hand-in-hand with one another.

There are a number of techniques available to aid in the detection of abnormal pressure. Among those which may provide prior information that abnormal pressure exists are:

1. Paleontology

2. Offset well logs and analysis of offset well histories3. Temperature changes4. Gas readings5. Formation resistivity6. Cutting appearance7. Hole conditions

Each of the above may be an indication that abnormal pressure exists, but there are also a number of techniques available which can be used to determine closely what the magnitude of the abnormal pressure actually is. Among these are:

1. “d” exponent

2. EWR resistivity plots3. Shale Density4. Shale Factor

The theory of detection of abnormal pressure will be dealt with in a separate section.

Since abnormal pressures and insufficient mud weights often go hand-in-hanwould seem that a solution to this problem would be to drill with high mud weights. However, high mud weights may exceed the fracture gradient, causstuck pipe, and lower the rate of penetration. The best practice is probably tomaintain enough mud weight to keep a slight overbalance and set additionalwhen the mud weight nears the fracture gradient in the weakest part of the h

4.1.2 Warning Signs of Kicks

There are a number of indicators that will warn of an impending kick. Rememthe earlier a kick is detected, the more easily the control of the well can be maintained. Early detection can keep a relatively minor problem from becomimajor catastrophe. It is the responsibility of the individual mud logger to be awof and on the lookout for any indicators of abnormal hole conditions which mbe noticed. Since most of the downhole information is inferred from what happto the drilling mud, most of the kick warnings also involve the drilling mud.



Pit Volume Increase

If fluid is leaving the well faster than it is being pumped into the well, there will be an increased volume of mud in the pits. Increased volume of mud in the pits means that the mud level in the pits will rise. For this to be an early indicator, changes made and additions to the surface mud system must be accounted for. Good communications are a necessity. Often times, adding treatment to the surface mud system causes a pit level increase which can cause a panic at other parts of the rig because no one was told beforehand that the mud was being treated. By the same token, the level in the pits could be rising due to a kick while everyone is attributing the level increase to mud treatment. Anything done to the mud system at the surface must be made known to those people on the rig who monitor the remote pit level indicators.

Well Flowing with the Pumps Off

When the rig pumps are not pumping mud into the hole, there should be no mud returning from the well. It usually takes a few seconds for flow to stop after the pumps have been shut down. A continued flow returning from the well after the pumps have been stopped is a very definite kick indicator. If the mud in the drill pipe is heavier than the mud in the annulus, the well will flow until the hydrostatic pressure in the drill pipe and the annulus equalize. Slugging is easy to differentiate from a kick because a kick will generally flow faster and faster while a slug in the drill pipe will cause a flow which decreases steadily as the drill pipe and annulus hydrostatic pressures equalize.

Pump Pressure Decrease and Stroke Rate Increase

A change in pump pressure may be a kick warning signal. As formation fluid first enters the wellbore, the mud may become flocculated (thick), causing an increase in pump pressure due to the increased mud thickness. This rise in pump pressure is momentary and may go entirely unnoticed in a normal drilling situation.

As influx fluid enters the wellbore, the fluid column in the annulus becomes lighter. This makes the mud in the drill pipe fall. The pump stroke rate will increase and the pump pressure will drop due to the falling mud in the drill pipe.

Pump pressure changes can be caused by several different things. Among these are plugged pump suctions, aerated mud at the pump suction, pump component failure, washouts in the drill string, washed out nozzles, lost circulation and others. Pump pressure decrease is not necessarily a kick indicator, but it is still good procedure to check for a kick if a pump pressure decrease is observed.



Improper Hole Fillup on Trips

As was previously mentioned, a predetermined number of pump strokes or barrels of mud is required to fill the hole on trips. If the hole takes less than the calculated amount of mud to fill, it is a fair assumption that formation fluid or gas has entered the wellbore, the well may not flow because not enough has gotten into the annulus to lighten the hydrostatic head of the mud in the annulus to a level below that of the formation pressure. However, corrective action should be undertaken immediately if the hole takes less than the calculated amount of mud on trips.

String Weight Change

A drill string weighs less when it is immersed in mud than it does in air because the mud provides a buoyant effect on the drill string. Heavy mud exerts more buoyant force on a string of pipe than light mud does. Formation influx lightens the mud column and results in decreased buoyancy acting on the drill string.

Drilling Breaks

It was stated previously that a rock must have sufficient permeability and porosity in order for a kick to occur. Increasing porosity will result in drilling rate increases because more of the rock itself is occupied by fluid and less space is occupied by the actual rock matrix. An abrupt change in the rate of penetration usually signals a formation change (as in going from a shale into a sand). The sand has a greater kick potential than a shale does, so it warrants stopping the pumps 3 feet to 5 feet into the sand and checking the well for flow. A gradual increase in the rate of penetration is not a drilling break, but it is an abnormal pressure detection device and may warrant flow checks if it persists.

Changes in Mud Gas Content

As a well is being drilled, gas enters the returning mud stream because gas is present in the formation actually being chipped loose by the bit. The gas trapped in the pore spaces of the drilled rock expands as it travels up the annulus. This gas can be detected at the surface with a gas detector. If the amount of gas in the mud is high enough, a mud weight reduction at the flowline is observable due to the gas bubbles present in the mud, and the mud is said to be gas cut.

Gas may also enter the mud stream as a result of the swab pressure created by pipe movement while making trips and connections. If the pump strokes to circulate bottoms up are known, connection gases and trip gases may be determined by counting the pumps strokes since a trip or connection and noting any increases or



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decreases in the gas level at the time that gas is due at the surface. Connection and trip gases must be evaluated by the amount of change from previous readings rather than by the readings themselves. If the trip or connection gases keep increasing with each trip or connection, there is a good chance that the formation pressure is increasing. However, increased connection or trip gases may also be caused by deteriorating mud flow properties or balled up equipment. These two factors must be considered before evaluating connection gases or trip gases.

Background gas is that gas which is encountered while actually drilling the well. If a gas bearing formation is being drilled, gas will breakout of the rock cuttings as it nears the surface. High gas readings do not automatically mean that an increase in mud weight is required, but simply that a gas bearing formation has been drilled. Of course, gas may enter the wellbore from the formation as a result of underbalance. In this case, the amount of gas entering the mud may not be sufficient to cause a kick or blowout because the volume of gas entering the mud stream is low (low rock permeability). However, if a zone of higher permeability is later drilled, a kick may occur. As a result, it often becomes necessary to determine whether the gas has been caused by core volume cutting or bleed-in from the formation. A common way of determining whether gas in the mud is caused by core volume cutting or formation gas influx is to circulate the cuttings from the wellbore. If the gas readings fall back to a low value (they will not generally reach “0” even if the hole is clean), the gas is probably a result of cvolume cutting. If relatively high gas readings persist, the gas may be a resubleed-in from the formation and an increase in mud weight may be necessarcorrect this condition.

Gas cutting increases are a better warning sign of impending abnormal pressthan they are of an impending kick. Caution must be used in evaluating gas readings, however, because of the variety of sources which may cause gas readings to change.

Water-Cut Mud

Water may enter the returning mud stream by the same mechanisms by whicenters the mud stream. If the density of the formation water is less than the deof the drilling mud, a reduction in flowline mud weight may occur.

Water does not expand as it travels up the annulus. As a result, any mud wecuts caused by core volume cutting are generally insignificant because the rathe amount of water in a given formation compared to the volume of mud intowhich the water can disperse is quite small. An influx of formation water into return mud stream can be detected by three methods which are (1) mud weigcut, (2) change in mud salinity, and (3) changes in mud viscosity.

In the Gulf Coast area, most formation water is saltwater. The salinity of the formation saltwater is generally higher than that of the water in the drilling mu



When this is true, formation water bleed-in can be detected by running a chloride ion test on the mud filtrate. If the chlorides keep increasing, the chances are good that formation fluid is probably bleeding into the return mud stream as a result of underbalanced conditions. The influx of saltwater in appreciable quantities will also cause viscosity increases in a freshwater mud system which uses bentonitic gel as a viscosifier. It is probably a good practice to check the chlorides in the mud anytime a sudden increase in viscosity is noted unless the exact cause of the mud thickening is known. If the mud in use at a particular time has a higher salinity than the formation water, the chlorides will decease.

Freshwater mud cutting can occur in the same way as saltwater cutting, but an influx of freshwater due to formation pressure will cause a weight reduction, chloride decrease, and thinning of a freshwater gel mud system. Freshwater cutting of a mud is not a common occurrence on the Gulf Coast.

Oil Cut Mud

Oil generally weighs less than water, so its potential to cause a flowline mud weight reduction is obvious. As in the case of water, oil does not expand as it makes its way up the annulus, so the amount of oil present in a mud due to core volume cutting is generally not enough to cause a measurable mud weight cut. This type of oil can be detected at the surface by examining the cuttings for fluorescence under an ultraviolet light and by gas chromatograph techniques. Oil blotches may also appear in the mud at the surface.

Crude oil from the formation which is present in sufficient quantities to cause a mud weight reduction is generally caused by bleed-in from the formation. However, caution should be used when evaluating the amount of oil in a drilling mud because oil is recyclable (it can be pumped back down the hole) and can be detected again at the surface. Also, significant oil cutting is rare in low permeability zones. If enough oil became entrapped in the mud as a result of bleed-in from the formation, the chances are good that the well would also be kicking and the kick would be easily detectable by other, more direct methods.

Conclusions

Flow rate increases, pit level increases, positive flow checks, decreases in pump pressure or increases in pump strokes, and improper hole fillups on trips are positive primary indicators which will generally manifest themselves at the time the well begins to kick. A drilling break may also be a good kick warning indicator and usually warrants a flow check. However, string weight changes, chloride changes, gas changes, and flowline mud weight changes generally take time to detect (usually the time to pump bottoms up). In most cases, the well would have kicked prior to any of these indications being manifested at the


Well ControlBasic Kill Operations

surface. Cut mud is a good indicator of developing abnormal pressure, but is only of secondary importance as a kick warning signal.

4.2 Basic Kill Operations

Early kick recognition and prompt execution of correct shut-in procedures is the key to successful kick control. Two primary objectives of well control operations are:

1. To kill the well safely

2. To minimize borehole stresses

A timely sequence of operations must be followed to achieve the main well control objectives. One of the most critical times in a well control operation is when the well is initially shut-in. After the well has been shut-in, the proper procedure for controlling the well must be used. A proper kill procedure is safer for the operation and personnel because it minimizes the stresses on both the wellbore and the surface equipment.

This section will be comprised of three parts. The first part will deal with proper shut-in procedures for both surface and subsurface blowout preventer stacks. The second part will deal with U-tubes and basic well control theory, and the third part will deal with proper kill procedures using both surface and subsurface blowout prevention equipment.

4.2.1 Shut-In Procedures

Flow Check

When a kick warning sign has been recognized, unless otherwise obvious, a flow check is made to determine is a kick occurring. A procedure to check for flow is as follows:

1. Pick up the kelly until the tool joint clears the blowout preventer.

2. Shut down the mud pumps.3. Observe for flow of mud at the flowline.

If mud continues to flow from the wellbore or if doubt exists as to the results of the flow rate check, the well should be shut-in immediately and check for shut-in pressure.



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Shut-in procedures are classified as either “hard” or “soft.” Each has primaryobjectives different from the other, and each is correctly applied in situations different from the other.

Hard Shut-In

The primary objective of a hard shut-in is to limit influx volume to a minimumWhen a hard shut-in is to be performed, the adjustable choke is closed befortaking a kick; and the wellbore is shut-in upon kick recognition by closing a blowout preventer. Influx is limited in volume to that which can flow into the wellbore during the time that the blowout preventer is closing. A hard shut-in dhave disadvantages. Erosion of blowout preventer elements can lead to the immediate or premature failure of the blowout preventer. The minimized surfapressure and wellbore stress can exceed what the wellbore can withstand caan underground or surface blowout.

Soft Shut-In

The primary objective of a soft shut-in is to control surface pressure during shand to minimize erosion of blowout preventer elements. When a soft shut-in be performed, the adjustable choke is open before taking a kick; the wellboreshut-in upon taking a kick by first allowing flow from the casing through the choke line; second, closing a blowout preventer; and third, closing the adjustchoke. Surface pressure is monitored and controlled if necessary while closinadjustable choke. Erosion of blowout preventer elements is minimized by diverting flow through the choke line while the blowout preventer is closing. Tsoft shut-in does have disadvantages. Subsequent well control operations, scirculating out the influx, are complicated by increased influx volume and surfpressure. Shut-in of the well may not be immediately possible. A dynamic kilprocedure may be required.

After a kick has been shut-in, and the shut-in pressure stabilized, (assumingunderground blowout has not occurred), no further formation fluid will flow inthe wellbore; formation pressure is balanced with a combination of hydrostatand shut- in surface pressure.



Figure 4.2 Typical Well Shut-In

A correct shut-in procedure will safely control surface pressure and wellbore stress while minimizing influx volume. Four different shut-in procedures will be discussed; each involves what to do when a kick occurs and one of the following conditions exist. A hard shut-in will be assumed for each.

Drilling Ahead with Surface Blowout Preventer Stack

1. When a kick is detected or suspected, raise the kelly immediately until the uppermost tool joint in the drill string is above the rotary table.

2. Shut down the rig pumps. Leaving the rig pumps on while the kelly is being raised helps to maintain extra mud pressure due to ECD and minimizes the possibility of additional swabbing. (Remember that the rate of fluid influx into the wellbore is a function of the amount of underbalance, and the permeability and porosity of the kicking formation. The circulating pressure helps to lessen the amount of underbalance.)

3. Check for flow.4. Close the annular preventer.5. Open the HCR valve.6. Notify the operator personnel.



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7. Read and record the shut-in pressures and the amount of pit gain.

Tripping with Surface Blowout Preventer Stack

1. Upon the detection of a kick, immediately set the slips just below the uppermost tool joint.

2. Install a full opening, fully opened drill pipe safety valve on the drill pipe and make it up properly. In federal waters, it is required that a full opening drill pipe safety valve in the open position be maintained on the rig floor for use at all times. Safety valves must be available which can be made up on any part of the drill string.

Note: Attempting to make up the valve when it is already closed can cause the installation of the valve to be difficult or impossible.

3. Close the drill pipe safety valve.4. Close the annular preventer.5. Open the HCR valve.6. Notify the appropriate operator personnel.7. Pick up the kelly and make it up on the drill string.8. Open the safety valve.9. Read and record the pressures. Note the amount of pit gain.

Special consideration is given to placement of tool joints and drill string movement for floating vessels and subsurface blowout preventer stacks. To ensure tools joints are clear of closing blowout preventers, the drill string is picked up to a predetermined, “space off,” height before closing the blowout preventer. Thcorrect space off height is determined from the pipe tally.

Uncontrolled vertical movement in a closed blowout preventer can separate drill string or damage the blowout preventer stack. Movement of the drill strinnormally minimized with a motion compensator, but when the motion compensators are ineffective, the drill string is hung off on a pipe ram in whacalled a hang off procedure. These considerations are included in the two following shut-in procedures.

Drilling Ahead with Subsurface Blowout Preventer Stack

1. Upon detection of a kick, immediately pick up the kelly to some predetermined height. This height has to be determined on the basis of thpipe tally. The kelly should be high enough so that the bottom kelly cock accessible and positioned such that no tool joints are positioned across frany preventer closing elements.

2. Shut down the mud pumps.



3. Check the well for flow.4. Close the annular preventer.5. Open the fail safe valve.6. Notify the operator personnel.7. Hang-off procedure:

a Reduce the hydraulic pressure on the preventer until a slight preventer leak can be observed at the flowline. This will help save the rubber when the drill pipe is stripped through the preventer.

b Slack the kelly down and close the bottom kelly cock.

c Set the slips just below the uppermost tool joint.

d Break the kelly off above the kelly cock valve.

e Rig up pump-in lines and reopen the bottom kelly cock.

f Pick up the pipe to the space off height.

g Close the top pipe rams and lock in position.

h Slack off until the string weight is held by the pipe rams. This should occur when the tool joint reaches the closed ram element.

8. Read and record the SIDPP, SICP, and the amount of pit gain.

It may not be necessary to hang off the drill string on the rams every time, but the procedure may be followed if a move off location is anticipated, the motion compensator is not working properly, or the weather is bad.

Tripping Pipe with Subsurface BOP stack

1. When a kick is detected, immediately set the slips just below the top tool joint.

2. Make up a full opening, fully opened safety valve on the drill string.3. Close the safety valve.4. Close the annular preventer.5. Open the fail safe valve.6. Notify the operator personnel.7. Make the hang-off decision.8. Pick up the kelly and make the kelly up on the drill string.9. Open the safety valve.10. Read and record pressures and the amount of pit gain. The sequence of steps

may again be altered to suit the operator preference. The hang-off procedure would probably not be followed if stripping back to bottom was anticipated.


Well ControlWell Control Theory

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4.3 Well Control Theory

In order to kill a well, the bottom hole pressure (hydrostatic pressures of the mud and gas plus any surface imposed pressures) must be maintained constant at a level greater than or equal to the formation pressure.

Well control is based on both sides of a U-tube being balanced (the pressures on both sides of the U are equal).

Consider a tube formed into the shape of a “U”. One side of the U would be equivalent to the drill pipe in the wellbore and the other side would be equivato the annulus (Figure 4.3).

Figure 4.3 U-tube with No Imposed Pressure

Assume both sides are filled with a 10.0 ppg mud, and that the system is closthe top on both sides. The bottom hole pressure (BHP) is equal to the sum ohydrostatic pressure exerted by the mud (5200 psi at 10,000 feet) plus any pressures imposed at the surface (0). Both sides of this system exert the samhydrostatic pressure; both sides have 0 psi imposed surface pressure, so thesystem is balanced and is in equilibrium. The objective in well control is to balance the pressures on each side of the system so that the BHP is held eqor greater than the formation pressure (Figure 4.3).



Assume the system is closed at the top on both sides; 6,000 psi of pressure is exerted at the bottom. The hydrostatic pressure of the mud is only equal to 5,200 psi. The 6,000 psi being exerted by the formation is enough to light the 10.0 ppg mud and blow it out of the U-tube, if the U-tube is left open. What must be done, then, is to balance the formation pressure by imposing pressures at the surface. Since the U-tube is filled by equal lengths of 10.0 ppg mud on both sides, the imposition of equal surface pressures will be necessary to keep the U-tube itself balanced (Figure 4.4).

Figure 4.4 U-tube with 800 psi Imposed Surface Pressure

Expressed mathematically, we want the bottom hole pressure to equal the formation pressure.

BHP = HP + Surface Pressure

Surface Pressure = BHP - HP

Surface Pressure + (6000 - 5200) psi

Surface Pressure = 800 psi

The necessary surface pressure is 800 psi.



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Figure 4.5 Unbalanced U-tube

Assume that the drill pipe side is filled with 10.0 ppg mud and annulus side is filled with 9.0 ppg mud. We wish to balance the BHP on both sides of the U-tube. Assume the U-tube is again a closed system.

BHP9.0 ppg = .052 × 9.0 ppg × 10,000 feet = 4680 psi

BHP10.0 ppg = .052 × 10.0 ppg × 10,000 feet = 5200 psi

In order to balance the U-tube, we need to impose surface pressure on the swhich has the least amount of hydrostatic mud pressure. In this case, the anside has the lighter mud, so surface pressure must be imposed on that side oU-tube. We need to impose enough surface pressure on the annulus side to the BHP on the annulus side up to the BHP on the drill pipe side.

We want:

HP(10.0 ppg ) = 5,200 psi = 4,680 psi + Surface Imposed Pressure

HP(10.0 ppg)

Drill pipe side =HP(9.0 ppg) + Surface Imposed Pressure

Annulus Side



HP(9.0 ppg)

The surface imposed pressure needs to be 520 psi on the annulus side to make the U-tube balance.

BHP = 5200 psi = 4680 psi + 520 psiHP(10.0 ppg) HP(9.0 ppg) Surface Imposed pressure

Figure 4.6 U-tube with Gas Influx

Assume the following conditions:

1. The U-tube is closed on both sides.

2. The drill pipe is filled with 10.0 ppg mud3. Total length of both the drill pipe side and annulus side = 10,000 ft.4. The formation pressure is 6,000 psi.5. The annulus is filled with 7,000 ft of 10.0 ppg mud and 3000 ft of gas.

(Disregard the gradient of the gas.)

We want to compute the SIDPP and SICP which will be required to balance the U-tube with formation and which will balance both sides of the U-tube itself.

We want to balance the BHP and FP on the drill pipe side,

*BHP = FP = SIDPP + HP10.0 ppg @ 10000’



and also to balance the BHP and FP on the annulus side,

**BHP = FP = SICP + HP10.0 ppg @ 7000’

and to balance the U-tube itself,

SIDPP + HP10.0 ppg @ 10000’ = SICP + HP10.0 ppg @ 7000’

the HP10.0 ppg @ 10000’ = 5,200 psi

and HP10.0 ppg @ 7000’ = 3,640 psi

FP = 6000 psi. We want the BHP = FP,

so from * above,

6000 psi = SIDPP + HP10.0 ppg @ 10,000’

if the SIDPP = 800 psi, the BHP = FP on the drill pipe side and from ** above,

6000 psi = SICP + HP10.0 ppg @ 7000’

6000 psi = SICP + 3,640 psi

The SICP required to balance the FP and BHP on the annulus side is 2,360 psi.

With 800 psi imposed at the surface on the drill pipe side and 2,360 psi imposed at the surface on the annulus side, the U-tube is balanced with respect to the formation and both sides are in balance relative to each other.



Figure 4.7 Balancing a U-tube While Circulating

The circulating pressure was 2,500 psi before the gas influx and with the well open. In this example assume the following conditions are known to exist:

1. The system is being circulated and back pressure is being imposed at the surface by varying the choke opening size.

2. The total system pressure loss at the pump being used is 2,500 psi with well open.

3. The annulus pressure loss at the pump rate in use is 100 psi.4. The drill pipe is filled with 10,000 feet of 10.0 ppg mud, and the annulus is

filled with 3000 ft. of gas and 7,000 feet of 10.0 ppg mud.5. The formation pressure is 5,700 psi.6. Disregard the gradient of the gas.

We want to find out what drill pipe pressure reading is required and what casing pressure reading is required in order to balance both sides of the U-tube relative to each other and to equalize the BHP on both sides of the U-tube with the formation pressure. In other words, we want:

BHPdrill pipe side = BHPannulus side = FP



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The total system pressure loss was measured as being 2500 psi prior to the kick. Of this, 2500 psi, 2400 psi was lost as a result of mud friction in the surface equipment, drill pipe, and the bit jets; 100 psi was lost in the annulus. The annulus pressure loss exerts and additional 100 psi on bottom as a result of circulating friction in the annulus. The pressure losses in the surface equipment, drill pipe, and bit jets do not result in additional pressure being exerted on bottom. The annulus pressure loss plus the choke pressure loss plus the hydrostatic pressure of the mud and gas on the annulus side are equal to the BHP exerted on the annulus side.

BHPannulus side = HPmud + HPgas + Choke Pressure + Annulus Pressure Loss

HPmud = 10.0 ppg × .052 × 7000' = 3460 psi

HPgas = 0 psi

Annulus Pressure Loss (APL) = 100 psi

BHP needs to be equal to FP, so

5700 psi = FP + BHPannulus

5700 psi = 3640 psi + 0 psi + Choke Pressure + 100 psi

5700 psi = 3740 psi + Choke Pressure

A choke pressure of 1,960 psi will balance the annulus side with the formatiopressure.

We now need to compute the drill pipe pressure which satisfies the specifiedbalances.

The system pressure loss was measured as being 2,500 psi with the annulusopen prior to the kick. Under static conditions,

FP = SIDPP + HP10.0ppg @ 10,000’ + BHP

5,700 psi = 5,200 psi + SIDPP

SIDPP = 500 psi

500 psi must be exerted at the surface on the drill pipe side before any mmovement can take place. We already know that an additional 2,500 psi pressure will be required because of friction to pump the mud at our desipump rate. Therefore, a pump pressure reading of 3,000 psi will be indicawhen the pump is brought up to the necessary circulating rate.


Well ControlKill Procedures

In a closed U-tube system, a balance between the two sides of the U is automatically established. The surface indicated pressures will automatically be those necessary to maintain balance in the closed system. The imposition of additional pressure anywhere in a closed, balance U-tube system will result in that additional imposed pressure being felt equally at all points in the U-tube system. Assume for example that we have a closed and balanced U-tube system with 100 psi pressure gauge readings on both sides. If we pressure up the annulus side to make it read 200 psi at the gauge, the drill pipe gauge will also read 200 psi and the BHP will rise by 100 psi. The 100 psi increase will also be felt at all other points in the closed system.

The drill pipe side of the U-tube is normally uncontaminated with formation fluid, so the hydrostatic pressure exerted by the mud in the drill pipe is effective over the total vertical depth and this pressure is known. The system pressure loss is known by prior measurement. The SIDPP is known also. This means that the BHP on the drill pipe side is known. If we pump at a constant rate and restrict the choke openings correctly, we can calculate the BHP on the drill pipe side. Since the system is balanced, we can hold the bottom hole pressure on the drill pipe side equal to the formation pressure. The annulus side will also be balanced relative to the formation pressure since the drill pipe side and annulus side are balanced relative to each other. Thus, we can hold the bottom hole pressure constant by manipulating the drill pipe pressure. Given the system pressure loss, hydrostatic pressure of the mud in the drill pipe, and the SIDPP, we can compute the formation pressure and the necessary drill pipe pressure at all times.

The annulus side of the U is contaminated with an unknown weight and volume of formation influx. Due to this, the casing pressure cannot be used to compute BHP; but any change in casing pressure from a balanced condition will result in a like change in drill pipe pressure. The system is balanced and closed, so any change in the imposed pressure at the choke will be felt equally at all points in the system. Thus, it is possible to hold the bottom hole pressure constant at the desired level. This is the underlying principle of well control.

4.4 Kill Procedures

4.4.1 Slow Pump Rate

As was stated previously that the bottom hole pressure can be controlled at any given time if the system pressure loss is known and the hydrostatic pressure exerted by the mud in the drill pipe is known. The system pressure loss should be recorded on a regular basis and any time the mud weight changes.



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The pumping rates at which system pressure losses are taken are normally from 1 to 3 barrels per minute. The system pressure loss is generally not taken at the normal circulating rate for a variety of reasons. Among these reasons are:

1. The system pressure loss at normal circulating rate plus and shut-in pressures may be excessive for the pump and surface conditions in use.

2. Any change in the choke opening size at normal pump rates may cause drastic pressure loss changes across the choke, which makes choke control difficult.

3. The mud being displaced in the annulus during a kill operation needs to be weighted before it is pumped into the well. It may also be contaminated and need treatment. Most rigs do not have the mud handling facilities to treat and weight the mud rapidly enough to keep up at normal pumping rates.

4. Faster pump rates result in higher annulus pressure losses. High annulus pressure losses increase the possibility of lost circulation.

The pump rate at which the system pressure loss is recorded for purposes of well control is called the slow pump rate, reduced pump rate, slow pump pressure, kill rate, or reduced circulating pressure. All these terms may be used interchangeably.

A slow pump rate of 1 to 2 barrels per minute is considered optimum in many cases because the system pressure losses are relatively low at this rate, the mud can be weighted and treated, and the mechanical stresses on the pumps are not too great. Slower rates are often impractical because the pump motors may not have enough power to drive the pump with low RPMs.

If the rig pump cannot be run at the desired output and pressure, an efficiency reduction can be effected by pulling various discharge and suction valves on the pump. The manufacturer’s recommendations should be followed concerningwhich valves to pull to obtain a desired reduction in pump efficiency. A high pressure - low volume pump (e.g., a cement pump) can also be used if the dpump rate cannot be reached by the rig pumps.

If the kill rate or pressure is not known before the kick, a kill rate pressure caobtained using the following procedure.

1. Shut in the well and record the SIDPP and the SICP.

2. Hold the SICP constant with the choke and bring the pump up to the despumping rate.

3. Note the circulating pressure obtained after the pump has been brought uthe kill rate speed.

4. The kill rate pressure is equal to the observed circulating pressure minusSIDPP.



4.4.2 Shut-In Pressure

After a kick has been detected and the well has been shut-in, it will be necessary to determine the shut-in drill pipe pressure (SIDPP) in order to determine the formation pressure and the necessary mud weight to kill the well. The shut-in drill pipe pressure is the amount by which the formation pressures exceeds the hydrostatic head of the mud in the drill pipe.

The amount of time which is required for the shut-in pressure to stabilize depends on the rock permeability, degree of underbalance, type of influx, and the depth of the well. In areas of low rock permeability, a considerable amount of time may be required for the shut-in pressures to stabilize.

In some situations, gas may tend to migrate up the annulus since it is lighter than the mud in hole. Gas migration will cause the pressures on both the drill pipe and casing to rise. The rise in pressure which occurs because of gas migration is a false indication of the amount of formation pressure present.

Pressure recorded on the casing or drill pipe side which is in excess of the pressure initially required to balance the formation pressure is call trapped pressure. Trapped pressure can result from either closing the well in without completely shutting down the pumps or gas migration. Trapped pressures will cause all kick calculations to be incorrect.

Although the presence of trapped pressure may not be apparent by a cursory examination of shut-in pressure, a procedure can be followed if its presence is suspected.

A recommended procedure for checking trapped pressures is as follows:

1. Bleed small amounts (less than 1 bbl) on the casing side and then shut the well in. If the drill pipe pressure continues to decrease each time mud is bled through the choke, keep repeating the bleeding and shut-in sequence.

2. If the SIDPP remains the same following two successive bleed-offs, use this figure as the true SIDPP. Continued bleeding will only allow more formation influx to occur.

3. Bleed from the casing side only in small amounts (1/4 to 1/2 bbl if possible). Bleeding large amounts of mud may allow additional influx of formation fluids to occur.

There are instances in which a float valve is installed in the drill string. A float valve is a simple one way valve that prevents the movement of fluids and pressures up the drill pipe. When a float valve is present in the string it naturally prevents the kick pressure from being recorded on the drill pipe. In the cases, the equivalent shut-in drill pipe pressure must be found another way.

The SIDPP can be found by either of two methods if a float valve is in use. One of the suggested methods involves the case in which the kill rate is known prior to



p to

ned t the

t

ill

fluid lace e. d

rill

e tion ain er, or

taking the kick. The second suggested method involves a procedure which can be followed if the system pressure loss was not known prior to taking the kick.

Case 1: Obtaining a shut-in drill pipe pressure if the kill rate pressure is known, float valve in use.

1. Shut-in the well, record the shut-in casing pressure and obtain the prerecorded kill rate from the driller’s log.

2. Hold the casing pressure constant with the choke and bring the pumps uthe prerecorded kill speed.

3. Note the circulating pressure obtained with the pump at the kill rate.4. Shut down the pump and close the choke. The circulating pressure obtai

with the pump at the kill rate minus the prerecorded circulating pressure asame pump rate is the shut-in drill pipe pressure.

Case 2: Obtaining a shut-in drill pipe pressure if the kill rate is unknown - floavalve in use.

1. Shut in the well and line up a low volume high pressure pump on the standpipe.

2. Start the pump and fill up all the lines with mud. Any air left in the lines wcause false pressure readings.

3. Increase the pressure on the pump. Note the pressure obtained when thefirst begins to move. Fluid is incompressible, so no movement can take puntil the pressure exerted on the bottom side of the float valve is overcomNote: The fluid has moved when a small volume of mud has been pumpewithout a change in pressure.

4. The pressure obtained when the fluid first begins to move is the shut-in dpipe pressure.

4.4.3 Influx Identification

If a kick occurs, the type of influx which has occurred can be determined. Thinflux may be either gas, oil, water, or a combination of the three. The calculais an approximation at best because the hole may not be gauge and the pit gmay not be accurately noted. If the fluid influx is a mixture of gas, oil and watexact nature of the influx will be impossible to obtain. However, the formula fdetermining the gradient of the wellbore influx fluid is:

INFLUX GRAD. = (mud gradient) - (SICP - SIDPP) (length of influx)

Where the mud gradient = gradient of the mud in the drill pipe and influx gradient = gradient of the wellbore influx.



ated

The influx gradient valve can be divided by.052 to obtain the density of the influx in ppg.

As a general rule, an influx with an equivalent mud weight of 1 to 3 ppg is assumed to be gas, 3 to 5 ppg is assumed to be a mixture of gas and water or gas and oil, and 5 to 7 ppg is assumed to be either oil, water, or an oil-water mixture.

Example: Assume the following wellbore conditions:

TVD = 10,000 feet

Mud weight in drill pipe = 12.0 ppg

Hole ID = 9.875 inches

Drill Pipe OD = 5 inches

SIDPP = 520 psi

SICP = 650 psi

Pit gain = 40 bbl

Determine the nature of the influx.

Solution:

1. Mud gradient = 12.0 ppg × .052 = .624 psi/ft

2. Annular volume (bbl/ft) = (9.8752 - 52) × .0009714 = .0700 bbl/ft3. Length of influx (ft) = bbl gained (bbl)

annular volume (bbl/ft)

= 40 bbl = 571 ft.0700 bbl/ft

4. Gradient of influx (psi/ft) = mud gradient - (SICP - SIDPP)length of influx

= .624 psi/ft - (650 psi - 520 psi) 571 ft

= .624 psi/ft - 130 psi571 ft

= 624 psi/ft -.228 psi/ft

= .396 psi/ft

5. Change the influx gradient to an equivalent mud weight .396 psi/ft ÷ .052 = 7.61 ppg.

6. An flux with a 7.61-ppg mud weight equivalent would probably be oil or water. The comparatively high weight means that not much gas is associwith the influx.


Well ControlKick Killing Procedures

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olved at a ipe be

jor

ed ay

4.4.4 Kill Weight Mud

After a well has been properly shut-in, the SIDPP and SICP recorded and the pit gain noted, the next step is to compute the mud weight necessary to kill the well. The kill weight mud (KWM) is figured as follows:

KWM = SIDPP × 19.12 + OMWTVD

or

KWM = SIDPP + OMW.052 × TVD

Where KWM = Kill weight mud (weight necessary to balance the well

TVD = True Vertical Depth of the well

SIDPP = Shut-in drill pipe pressure

OMW = Original mud weight

4.5 Kick Killing Procedures

There have been a number of well kill procedures devised. Three of the procedures are in common usage today. In all three cases, the principles invare the same. The purpose is to maintain the bottom hole pressure constant level equal to or slightly greater than the formation pressure. Since the drill ppressure is a direct bottom hole pressure indicator, the drill pipe pressure canmanipulated in a systematic manner, and the well can be controlled. The mamethods of performing well-kill operations by manipulation of the drill pipe pressure are:

Wait and Weight Method. After the well is shut-in, the surface mud system is weighted up to the weight required to kill the well. The kill weight mud is pumpinto the well and the well is killed in one complete circulation. This method malso be called the Engineer’s Method or the One Circulation Method.

Driller’s Method. After the well is shut-in and readings are recorded, pumping is begun immediately. The influx is pumped from the wellbore without any prior weighting of the mud. Once the influx has been pumped from the well, the well is shut-in, and the surface mud system is weighted up to the necessary kill weight. The light mud in the well is then displaced with kill weight mud. This method is sometimes called the Two Circulation Method.



Concurrent Method. After the well is shut-in, pumping is begun immediately and the mud weight is raised while the kick is being circulated out. The use of this method may require several circulations before the well is fully killed.

4.5.1 Wait and Weight Method

Before initiating circulation, the bottom hole pressure is equal to the hydrostatic pressure of the mud in the drill pipe plus the shut-in drill pipe pressure. If the initial circulating pressure is held equal to the kill rate pressure plus the shut-in drill pipe pressure, then the bottom hole pressure is still the same as it was prior to starting circulation. In the wait and weight method, kill weight mud is immediately pumped down the drill pipe. This raises the hydrostatic pressure exerted by the mud in the drill pipe, so the drill pipe pressure must be allowed to decrease as the kill mud makes its way to the bit. When the kill weight mud reaches the bit, the hydrostatic pressure exerted by the mud in the drill pipe is equal to or greater than the formation pore pressure. The well is now dead on the drill pipe side, and the SIDPP will be 0 at this point. When the pump is restarted and brought up to the kill rate once again, the drill pipe pressure will now be equal to the circulating pressure required to move the mud at that rate. Since no additional changes will be made to the mud on the drill pipe side, the drill pipe pressure and pump rate should be held constant while the annulus is displaced with kill weight mud. When the kill weight mud reaches the surface, the well should be dead (i.e., no shut-in pressures and no flow with the pumps off).

In order to keep track of the various procedures and pressures which need to be used to kill a well, a worksheet is usually filled out after the well has been shut-in and the various readings have been recorded. The worksheet or kill sheet shows the pressures required versus the amount of mud pumped. The heart of the kill sheet is a schedule of drill pipe pressure versus strokes (amount of mud pumped).

The pressure schedule for the drill pipe is filled out as follows:

1. Calculate the number of strokes required to displace the dill pipe with kill weight mud.

2. Calculate the initial circulating pressure. This is done by adding the SIDPP to the prerecorded kill rate pressure.

3. Calculate the final circulating pressure

Final Circulating Pressure = Kill Rate Pressure × KWMOMW

where: KWM = Kill weight mud

OMW = Original mud weight



The final circulating pressure is higher than the kill rate pressure because the higher mud weight used in the kill operation has a greater system pressure loss than the lower weight mud. The factor KWM/OMW is a way of compensating for this difference in system pressure loss.

4. Plot the amount of mud pumped (either barrels or strokes) along the horizontal axis.

5. Plot the drill pipe pressure along the vertical axis. The drill pipe pressure will fall at a constant rate as the drill pipe is displaced with the kill weight mud, at which point the drill pipe pressure will be held constant at the final circulating pressure. Therefore, the plot can be completed by plotting only two points. Plot initial circulating pressure at 0 strokes. Plot the final circulating pressure at the strokes required to displace the drill pipe with kill weight mud (Figure 4.8).

Connect the two points with a straight line. The straight line indicates the pressure which should be held on the drill pipe at all times while the kill weight mud is being pumped down the drill pipe. The choke opening is varied as required to keep the drill pipe pressure regulated.

Figure 4.8 Drill Pipe Pressure Schedule

Fill in the drill pipe pressure schedule:

Assume SIDPP = 500 psi

Kill rate pressure = 1000 psi

Original mud weight = 10.0 ppg



two

ace

p to e

is

in.

lling drill

the the

Kill weight mud = 11.0 ppg

Strokes to displace drill pipe = 500 strokes

Solution: Initial Circulating Pressure

= Kill rate pressure + SIDPP

= 1,000 psi + 500 psi

= 1,500 psi (at 0 strokes)

Final circulating pressure

= Kill rate pressure × KWMOMW

= 1000 psi × 11.0 ppg10.0 ppg

= 1100 psi (after 500 strokes)

Plot 1,500 psi at 0 strokes and plot 1,100 psi at 500 strokes. Connect thepoints with a straight line.

When the wait and weight method of well control is being used, the followingsteps should be followed:

1. Shut-in the well using the preferred shut-in sequence.

2. Record the SIDPP, SICP, and the amount of pit gain. Check for trapped pressure.

3. Compute the mud weight necessary to kill the well and weigh up the surfmud system to this weight. Fill out the kill sheet while the mud is being weighted up.

4. Hold the casing pressure constant by controlling the choke and bring thepump up to the prerecorded kill rate. Once the pump has been brought uthe kill rate, be certain that the drill pipe pressure is equal to the sum of thSIDPP and the prerecorded circulating pressure at the kill rate.

5. Follow the drill pipe pressure schedule while the light mud in the drill pipebeing displaced with kill weight mud.

6. Once the drill pipe has been filled with heavy mud, the well may be shut-The SIDPP should be 0 at this point. This step is optional and is simply acheck to make certain that the kill weight mud calculation is correct.

7. If Step 6 has been followed, hold the casing pressure constant by controthe choke and bring the pump up to the kill rate once more. Be certain thepipe pressure is equal to the final circulating pressure.

8. Hold the drill pipe pressure constant (while maintaining the pump rate at kill rate) at the final circulating pressure until the kill weight mud reaches surface.



9. When the kill weight mud reaches the surface, shut down the pump and shut-in the well. All shut-in pressures should be zero. Open the choke and check for flow. Then open the preventer stack, close the choke, and re-check to see that the well is dead.

Some people prefer a mathematical method of doing drill pipe pressure schedules. The reason is that a table listing the drill pipe pressure values versus amount of mud pumped is easier for some people to read than the graph.

Consider the data used in the previous drill pipe pressure schedule:

SIDPP = 500 psi

Kill rate pressure = 1000 psi

Original mud weight = 10.0 ppg


Stroke to displace drill pipe = 500 strokes

The initial circulating pressure is 1,500 psi. The final circulating pressure is 1,100 psi. We know that the drill pipe pressure should fall at a constant rate while kill weight mud is being pumped down the drill pipe. In this case it falls from 1,500 psi to 1,100 psi in 500 strokes. Therefore, the drill pipe pressure decrease per stroke is:

DP pressure decrease per stroke

= Initial circulating pressure - Final circulating pressureStrokes required to displace DP with KWM

= 1500 psi - 1100 psi 500 strokes

= .8 psi/stroke

A .8-psi/stroke decrease is impossible to read with present rig instrumentation, but if we construct a table of drill pipe pressure values, we can use the drill pipe pressure decrease per 100 strokes pumped which is:

.8 psi/stroke × 100 strokes = 80 psi per 100 strokes

The table is constructed as follows:

Table 4.1 Drill Pipe Pressure Values

Strokes Pumped Drill Pipe Pressure

0 1500 psi

100 1500 psi - 80 psi = 1420 psi

200 1420 psi - 80 psi = 1340 psi



d. o

ised light d

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ump

PP the

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inal

The table states that the drill pipe pressure should be 1,420 psi after pumping 100 strokes, 1,340 psi after pumping 200 strokes, etc. This method eliminates any errors which may occur as a result of reading the drill pipe pressure graph incorrectly.

4.5.2 Driller’s Method

Another method of well control is the driller’s method or two circulation methoThis method requires fewer calculations than the wait and weight method. Twcirculations of the mud in the wellbore are required to kill the well using this method. During the first circulation, the formation fluid influx is circulated fromthe wellbore. The well is then shut-in, and the mud weight at the surface is rato the density necessary to kill the well. The pump is then restarted, and the mud in the wellbore is displaced with kill weight mud. At the end of the seconcirculation, the well is checked to make sure it is dead.

The driller’s method is implemented by using the following procedure:

1. Shut-in the well using the preferred shut-in procedure.

2. Record the SIDPP, SICP, and the amount of pit gain. Be sure to check fotrapped pressure.

3. Compute the mud weight necessary to kill the well.4. Hole the choke pressure constant by controlling the choke and bring the p

up to the kill rate.5. Hole the drill pipe pressure constant at the initial circulating pressure (SID

+ kill rate pressure) by controlling the choke and pump at the kill rate untilinflux is out of the hole.

6. After the influx is out of the hole, shut-in the well and raise the mud weighthe pits to the kill weight.

7. Hold the casing pressure constant and bring the pump up to the kill rate.8. While pumping at the kill rate, hold the casing pressure constant by

controlling the choke and displace the mud in the drill pipe with kill weighmud.

9. Once the drill pipe has been displaced with kill weight mud, observe the fcirculating pressure on the drill pipe pressure gauge.

300 1340 psi - 80 psi = 1250 psi

400 1250 psi - 80 psi = 1180 psi

500 1180 psi - 80 psi = 1100 psi

Table 4.1 Drill Pipe Pressure Values

Strokes Pumped Drill Pipe Pressure



sed. le,

ure a x has the ant ure ill

n the

drill thod. own

ted

10. Keep pumping at the kill rate and hold the drill pipe pressure constant at the observed final circulating pressure by controlling the choke until the kill weight mud reaches the surface.

11. When the kill weight mud reaches the surface, shut down the pump, close the choke, and verify that the SIDPP and SICP are both zero. If so, then open the choke to be sure the well does not flow. If no flow is observed, open the preventers and check again to be sure the well is completely dead.

The drill pipe pressure graph may be eliminated when the driller’s method is uSince the kill weight mud is not circulated until after the influx is out of the hothe choke can be used to hold the drill pipe pressure constant at the initial circulating pressure (kill rate pressure + SIDPP). This action is enough to ensconstant bottom hole pressure equal to the formation pressure. Once the influbeen removed from the wellbore, the annulus is no longer contaminated, so SICP is now the same as the SIDPP. Holding the casing pressure at a constvalue equal to the original SIDPP now assures a constant bottom hole pressequal to the formation pressure. The casing pressure is held constant until kweight mud reaches the bit. Once kill weight mud reaches the annulus, the hydrostatic forces in the annulus begin to change, but the hydrostatic forces idrill pipe are no longer subject to change.

4.5.3 Concurrent Method

Holding a constant drill pipe pressure now with the Concurrent Method. This pipe pressure schedule is similar to the one used for the Wait and Weight MeThe difference lies in the fact that several different weight muds are pumped dthe drill pipe in succession. The drill pipe pressure is used as the bottom holepressure indicator.

A drill pipe pressure schedule for use with the Concurrent Method is construcas illustrated:

Example:

Assume the following well conditions:

TVD = 10,000 feet

SIDPP = 520 psi

SICP = 650 psi

Pit gain = 25 bbl

Time required to pump from surface to bit = 30 minutes

Mud weight in use = 10.0 ppg

Kill rate = 30 strokes/min



ents as

To :

rate,

ppg

to

es)

It has been decided to kill the well using the Concurrent Method. Since it is necessary to begin killing the well as soon as possible, ad decision has been made to increase the surface mud weights in .2 ppg increments. Fill out a drill pipe pressure schedule to be used during the kill operation.

Solution:

Kill weight mud = 520 psi × 19.23 + 10.0 ppg = 11.0 ppg10,000 feet

Initial circulating pressure = 1,000 psi + 520 psi = 1520 psi

Final circulating pressure = 1,000 psi × 11.0 ppg = 110 psi w/KWM10.0 ppg

The mud density needs to be increased by 1.0 ppg to kill the well. Since the density is going to be increased by .2 ppg at a time, 5 drill pipe mud displacemwill be made. The initial and final circulating pressures are exactly the same those which would be used in the Wait and Weight Method. This method is different only in that it takes 5 times as long to kill the well, but the principles involved are exactly the same as those used in the Wait and Weight Method.fill out a drill pipe pressure schedule the following procedure may be followed

1. Compute the time necessary to pump from the surface to the bit at the kill the kill weight mud, the initial circulating pressure and the final circulatingpressure.

2. Decide the density increments in which the mud weight will be raised (.1 per circulation, .2 ppg per circulation, etc.)

3. Calculate the number of drill pipe displacements which will be necessaryraise the mud weight and calculate the total time or number of strokes involved. In this case, 5 displacements of the mud in the drill pipe are necessary and 30 minutes are required for each displacement at 30 strokes/min.

4. The mud weights being pumped down the drill pipe and the strokes (or timinvolved are plotted along the horizontal axis. The drill pipe pressures areplotted along the vertical axis as follows (Figure 4.9):



Figure 4.9 Drill Pipe Pressure Schedule

A procedure which can be followed when the Concurrent Method is being used is as follows:

1. Shut-in the well using the preferred shut-in procedure.

2. Allow the SIDPP and SICP to stabilize. Check for trapped pressures. Record the SIDPP, SICP, and the amount of pit gain.

3. Fill out the kill sheet. Weight up the pits quickly to the desired weight.4. While holding the choke pressure constant, bring the pump speed up to the

kill rate. The initial circulating pressure should be equal to the sum of the SIDPP and the kill rate circulating pressure.

5. Pump at the kill rate and follow the drill pipe pressure schedule until the kill weight mud reaches the bit.

6. When the kill weight mud reaches the bit, the pump may be shut down, the well shut-in, and the shut-in pressures checked. The SIDPP should be equal to zero.

7. Restart the pump and maintain its speed at the kill rate. Hold the drill pipe pressure constant at the final circulating pressure by partially/gradually opening or closing the choke until the kill weight mud reaches the surface.

8. When the kill weight mud reaches the surface, stop by partially/gradually opening or closing the choke, close the choke, and check to see that the SIDPP and SICP are both equal to zero. If they are, open the choke and check for flow. The preventer stack may be opened and the well again checked for flow.

2000


Well ControlKill Procedures with Subsurface BOP Stacks

4.6 Kill Procedures with Subsurface BOP Stacks

The use of the marine riser on sea floor wellheads in deepwater drilling applications requires several special considerations in kick detection and kick killing.

Most of the additional problems and procedure changes resulting from the use of a marine riser and subsea preventer stack are associated with (1) low formation fracture gradients, (2) kick detection, and (3) pressure losses in the choke line.

The two earliest and most positive signs that a kick condition exists are: (1) an increase in the pit level, and (2) an increase in the mud return flow rate. The roll and heave of a mobile drilling vessel causes the pit level to fluctuate, even though the amount of mud in the pits may be constant. A pit-level float attached to a recorder will often show a 5 to 50 barrel fluctuation in pit level at any given time. A real increase in pit level may manifest itself only after a large gain has occurred. Large gains bring about additional stresses on the wellbore during a well control operation.

The heave of the vessel also results in constant changes in the flowline height relative to the ocean floor. Mud exits the well at varying rates, which makes flowline monitoring devices of limited value. Fortunately, both the pit level and return flow rate can be monitored accurately by additions or changes in the conventional type monitoring systems.

The roll and heave of a floating drilling vessel results in pit level fluctuation similar to those illustrated in Figure 4.10.



Figure 4.10 Pit Level Changes that Result from Heave and Roll of a Floating Drilling Vessel - No Change in the Amount of Mud in the Pits

A single float mounted in the pit is insufficient to monitor the actual pit volume. However, a pit level monitor can be mounted at both ends of the pit. If the two (or more) floats in each pit are tied together in such a way that the total volume is read out on a recorder, the pit volume can be monitored accurately. This principle is illustrated in Figure 4.11.



Figure 4.11 Compensating for Pit Level Changes that Result from Heave and Roll on a Floating Rig - Constant Volume of Mud in the Pits

In the illustration above, a rise in mud level on one side of the pit results in a decrease in mud level on the other side of the pit. Since the mud volume remains constant and both pit level monitors are tied together, the total volume can be read as a constant because the rise in level of one pit level monitor is accompanied by an equal decrease in level by the other pit monitor. The sum of their readings is indicated on the recorder. Pit volume totalizers have been developed which can accommodate eight or more pit floats, sum their individual readings and display the total volume and total change in volume on a recorder.

In order to monitor the return flow rate with any accuracy, a sensor must be placed in a position where level changes do not take place. The vessel motion at the surface does not affect the rate at which mud passes a point on the ocean floor. Electronic sensors have been developed which are able to monitor return mud flow at or near the ocean floor. This approach allows the accurate measurement of flow rate from the well.

Once a kick has been detected on a floating drilling rig, the well needs to be shut-in. The hang-off procedure discussed earlier may be necessary to prevent damage to the drill string or a stationary preventer. If the weather is severe, the motion compensator will not prevent all drill string motion. The weight of the string may be placed on the rams and flexible pump-in lines can be rigged up. Hanging-off will result in the drill string remaining motionless relative to the preventer elements, and the flexible pump-in lines will allow vessel motion without placing tension or compression forces on the drill string, which would



result if a kelly or other fixed-position pump-in line was used. Hanging-off may not be necessary or desirable in every instance, but it should be used if any of the following conditions develop or are anticipated:

1. Bad weather

2. Motion compensation failure3. Moving off location

Two chokes lines and additional preventers are generally included to serve as backups in case of component failure on a subsea stack. Two annular preventers, several sets of rams (pipe rams, blind rams, and shear rams) are included. The bottom set of pipe rams is generally placed below the choke lines. This allows the well to be closed in if repairs need to be made to any BOP components or choke lines. The shear rams are also generally located beneath all the choke lines so that the drill string can be severed and the rig moved off quickly if an impending blowout develops.

Choke lines generally run from the ocean floor to the surface when a subsea preventer stack is in use. These choke lines have relatively small inner diameters, and in deepwater applications where long choke lines are in use, considerable pressure loss resulting from mud flow through the choke line can develop. The pressure loss in a choke line results in additional bottom hole pressure. If the bottom hole pressure is to be held constant at a known value, the amount of pressure loss in the choke line must be known.

The slow pump rate should be taken through both the riser (preventers open, choke closed) and through the choke line with a preventer closed. If both readings are taken at the same pump rate and mud properties, the difference in the two readings will be equal to the pressure loss in the choke line.

Example: After making a connection, the driller obtained a reduced circulating pressure through the riser (normal drilling conditions) of 800 psi at 30 stk/min. He then closed the upper annular preventer, opened the choke and choke lines, and brought the pump up to 30 stk/min. The pressure obtained through the choke line was 1,00 psi at 30 stk/min:

The pressure loss in the choke line was:

The 300 psi pressure loss in the choke line results in an additional 300 psi of bottom hole pressure. In fact, an additional 300 psi is applied to all points in the wellbore that are below the base of the choke line. At shallower depths, the

1,100 psi 800 psi = 300 psi

Circulating pressure obtained through choke line

Circulating pressure obtained through riser

Circulating loss through choke line



300 psi can cause considerable increases in the equivalent mud weights seen by the formation.

The reduced circulating pressure should be obtained at the slowest possible pump rate. If a gas kick occurs, the gas will begin to expand as it is pumped from the wellbore. As the bubble expands, the amount of mud returning from the well will be greater than the amount of mud being pumped into the well. This increased return flow rate results in an increase in choke line pressure. (Pressure loss through a conduit is dependent upon the flow properties and velocity of the fluid traveling through that conduit.) If the choke line pressure loss is of concern prior to the time a kick occurs, the pump rate should be slowed down enough to hold this pressure loss to a minimum. It may be necessary to obtain reduced circulating pressures with a cement pump or other high pressure low volume pump in order to meet this requirement.

The reduced circulating pressure which was obtained through the riser is the pressure which should be used in making the kill sheet calculations. The initial circulating pressure is equal to the sum of the reduced circulating pressure obtained through the riser and the shut-in drill pipe pressure. The final circulating pressure is obtained by multiplying the ratio of the kill weight mud to original mud weight by the reduced circulating pressure obtained through the riser. The other procedures used in killing a well from a floating drilling vessel are very similar to those used in killing a well which employs a surface-mounted preventer stack. The main consideration, therefore, is obtaining a reduced circulating pressure. Failure to obtain the reduced circulating pressure will necessitate calculating the pressure loss through the choke line which, as with most pressure loss calculations, is an approximation. The approximation that results from calculating the pressure loss through a choke line can result in significant errors in kill sheet calculations. Knowledge in advance of the choke line pressure loss is simpler and eliminates errors.

The choke line pressure loss may be approximated by using the following formula:

Pressure loss through choke line =

where: p = mud weight (ppg)

q = pump rate (gpm)

PV = plastic viscosity (centipoise) of the mud

D = inner diameter of the choke line

L = length of the choke line

Example:

0.000077p0.8

Q1.8

PV( )2L×

D4.8( )

------------------------------------------------------------------



We need to determine the choke line pressure loss, give the following conditions:

Choke line length = 2000 feet

Choke line inner diameter = 2.5 inches

Pump rate = 100 gpm

PV = 35 centipoise (cp)

Mud weight = 12.8 ppg

Pressure loss through choke line =

= 118 psi

The calculated pressure loss through the choke line is 118 psi. If a reduced circulating pressure is not known, it may be determined by using the following procedure:

1. Decide what the kill rate is to be (either in barrels/min or strokes/min).

2. Calculate the pressure loss through the choke line at the desired pump rate.3. Subtract the calculated choke line pressure loss from the shut-in casing

pressure.4. As the pump is brought up to speed gradually, reduce the casing pressure until

it is reduced by an amount equal to the answer obtained in Step 3 and hold it at this value until the pump is brought up to speed.

5. Once the pump is at the desired kill speed and the casing pressure is at the desired value, record the standpipe pressure reading. This reading is equal to the initial circulating pressure.

6. The initial circulating pressure minus the shut-in drill pipe pressure corresponds to the reduced circulating pressure, which is used in making the final circulating pressure calculation.

7. Using the answers obtained in steps 5 and 6, the kill sheet can be completed.

Example:

We need to obtain a reduced circulating pressure. The well has been shut-in and following conditions exist:

SIDPP = 500 psi

SICP = 800 psi

Choke line length = 2000 feet

Choke line ID = 21/2 inches

PV = 35 cp

0.000077 12.800.8 100 )( 1.8 35 )( 0.2[ ] 2000×2.5( )4.8

-------------------------------------------------------------------------------------------------------



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Desired pump rate = 100 gal/min

The operator has decided to use 100 gal/min as the kill rate. The choke line pressure loss has been calculated as 118 psi. The operator brings the pump up to 100 gal/min, and he allows the casing pressure to decrease by 118 psi as he brings the pump rate up. The new casing pressure is 800 psi - 188 psi = 682 psi (700 on gauge). He notes the standpipe pressure is 1,000 psi with the pump displacing 100 gal/min, and the casing pressure is 682 psi. The initial circulating pressure (which corresponds to what the system pressure through the riser would have been at 100 gal/min) is equal to the initial circulating pressure minus the shut-in drill pipe pressure. In this case, the reduced circulating pressure is 1,000 psi - 500 psi = 500 psi. As a result we have:

SIDPP = 500 psi

Initial circulating pressure = 1000 psi

Reduced circulating pressure = 500 psi

The pressure loss through the choke line is often called the “hidden choke effIt must be taken into account each time a well using a subsea stack is killed.

A sequence which can be followed during well control operations using subsblowout preventers can now be developed. A recommended sequence of eveas follows:

1. Upon detection of a kick, pick up the kelly, shut down the pumps, and shuthe well.

2. Read and record the SIDPP, SICP, and the amount of pit gain.3. Notify the operator personnel.4. Fill out the kill sheet if the reduced circulating pressure and choke line

pressure drops are known. If a reduced circulating pressure was not previously obtained, calculate the choke line pressure loss by formula or hydraulic slide rule. Bring the pump up to the desired kill rate and allow thcasing pressure to fall below its initial shut-in value by an amount equal tocalculated choke line pressure loss. (Controlling the choke in such a manthat allows the casing pressure to fall at the proper rate as the pump is brup to speed is awkward. It may be more simple to open the choke first, bthe pump up to speed and then gradually close the choke opening until thcasing pressure reads the desired value.) Observe the initial circulating pressure and then shut down the pump and close in the well once again.out the kill sheet and begin weighting up the surface mud system if the Wand weight or concurrent method is to be used. If the driller’s method is toused, the kill operation can begin as soon as the necessary calculations completed.

5. Bring the pump up to speed. Regulate the casing pressure as the pump ibrought up to speed. Once the pump is at the desired kill rate, “fine tune”choke opening until the drill pipe pressure gauge indicates the proper val



6. Kill the well by following the appropriate pressure schedule and kill procedure.

7. Once kill weight mud reaches the surface, shut down the pump, close the choke, and verify that the well is dead. Open the choke and check for flow through the choke line.

8. Since the preventers are located on the ocean floor, the riser is still full of original mud. This light mud must be displaced prior to opening the preventer stack. To do this, close the bottom set of pipe rams and circulate kill weight mud down the choke line. Continue this reverse circulation procedure until the riser has been displaced with kill weight mud. The rams can then be opened without the danger of allowing additional influx to enter the wellbore.

4.6.1 Other Considerations In Deepwater Drilling

The importance of early kick detection cannot be overemphasized, especially in a deepwater drilling environment. The reasons that early kick detection are especially important on a floating vessel are as follows:

1. The fracture gradients in deep water are relatively low.

2. Choke line friction during bubble expansion may cause lost returns. An underground blowout may occur.

3. The collapse resistance of large diameter pipe is lower than the collapse resistance of smaller diameter pipe of the same wall thickness. A gas bubble which is allowed to enter the riser can unload the riser of mud, leaving the riser subject to the full hydrostatic force exerted by the water surrounding it. The riser may collapse as a result.

The fracture gradients are low in deepwater drilling operations, because the fracture gradient of a formation is directly related to the overburden stresses applied to it. A larger overburden generally implies a higher fracture gradient (this is the same as saying that fracture gradients increase with increasing depth, which they generally do). Water exerts less stress on an underlying formation than the same amount of overlying rock would exert on that same formation. For example, a formation at 10,000 feet relative to the kelly bushing in 2,000 feet of water may have only 8,900 psi of overburden earth acting upon it. This formation would have a fracture gradient similar to an 8,900-foot formation on land (remember overburden stress is 1.0 psi/ft).

In 1,000 feet of water, a formation at 4,000 feet (relative to the kelly bushing) will have a .3-to .5-ppg lower fracture gradient than a formation at 4,000 feet on land. This can make a considerable difference in what happens during a well control operation.

Lost returns which occur during a well control operation present severe danger to a floating drilling vessel. The formation may allow the gas to be expelled to the sea directly underneath the drilling vessel. This will result in aerated water.


Well ControlComparison of the Three Methods of Well Control

Aerated water is incapable of sustaining a floating vessel, and the rig may sink if the aeration is severe and uniform at all points directly beneath the hull of the vessel. There has been some discussion that water aeration will only occur beneath certain portions of a drilling vessel at any given time. If this is indeed true, the vessel would probably not sink, but it could dip at a precarious angle in the area where water aeration is taking place due to the decreased buoyancy in that particular area.

4.7 Comparison of the Three Methods of Well Control

4.7.1 Gas Kicks

One of the stated objectives of well control is to minimize the borehole stresses. For our purposes, minimizing borehole stresses of necessity means that the equivalent mud weighs at various depths must be held to minimum values.

If a gas kick occurs, the gas will expand as it approaches the surface because of the decrease in hydrostatic pressure which exerts force on top of the gas bubble. The volume of the gas bubble can be expressed as a function of the pressure exerted upon it. For example, a gas may occupy a certain volume of 100 cubic feet with 500 psi of pressure confining it. The same gas would then occupy a volume of 200 cubic feet if the pressure confining it were reduced to 250 psi. The volume that a gas occupies also depends on temperature and the compressibility properties of that particular gas. The purpose of this section is not to present a discussion of gases and the physical laws they obey, but to compare the borehole stresses which occur through using any one of the three previously mentioned well control procedures.

In order to control a well, the bottom hole pressure needs to be maintained constant at a level equal to the formation pressure. The bottom hole pressure (on the annulus side) is the sum of the hydrostatic pressure exerted by the gas itself, the hydrostatic pressure exerted by the mud below the gas, the annulus pressure loss while circulating and the surface imposed back pressure (choke pressure).

A comparison of the borehole stresses which occur when any of the three methods is used will be presented (Figure 4.12). Gas expands as it rises to the surface and this increase in gas bubble length results in a decrease in the hydrostatic pressure exerted by the fluids in the annulus. An increase in surface imposed pressure (choke pressure) is necessary to maintain the bottom hole pressure constant at the desired level. If an oil or water kick occurs, expansion does not take place, and the



borehole stresses encountered are lower than those which would be expected in a gas kick.

Example: Assume the following wellsite conditions exist:

Hole diameter = 81/2 inches

Drill pipe OD = 41/2 inches

Drill pipe ID = 3.826 inches

Total depth = 15000 feet


Pump output = .15 bbl/stk

Kill rate pressure = 1000 psi at 20 stk/min

Pit gain = 25 bbl

SIDPP = 780 psi

SICP = 1100 psi

Surface stack is in use. For purposes of simplicity, a constant hole and pipe diameter are assumed.

The following calculations have been made:

Drill pipe capacity = 213 bbl

Kelly to bit = 1420 stks

Capacity of annulus = 758 bbl (0.0505 bbl/ft)

Strokes, bit to surface = 5053 stks

Total strokes required to = 6473 stksdisplace mud in the well

Barrels required to displace = 971 bblmud in the well


Initial circulating pressure = 1780 psi

Length of influx = 25 bbl = 495 ft.0505 bbl/ft

Influx gradient = mud gradient - (SICP - SIDPP)Length of Influx

= .78 psi/ft - 320 psi = .13 psi/ft495 ft

A .13-psi/ft gradient for the wellbore fluid influx means that the kick is gas.



re ed for eight hod

s not er of

f the

Hydrostatic pressure exerted by the gas = .13 psi/ft × 495 feet = 64 psi

Formation pressure = 15.0 ppg × .052 × 15,000 feet + 780 psi

= 11,700 psi + 780 psi

= 12,480 psi

Using the data above, the casing pressure expected while killing this kick wecalculated. The casing pressure versus barrels of mud pumped were calculateach of the three previously discussed well control methods. The Wait and WMethod assumes that the kill will be made in one circulation. The driller’s metwould require two circulations to complete the kill. The concurrent method assumes five displacements of the mud in the drill pipe plus two to three displacements in the annulus to complete the kill. The concurrent method doerequire any set number of circulations to complete a kill operation. The numbcirculation required and the rate of mud weight increase depend upon rig capabilities and operator preference. In addition, the table includes a listing ocasing pressures which occur when the well is overkilled with 17.0 ppg mud (Table 4.2).

Table 4.2 Casing Pressures Expected (psi)

Barrels of Mud Pumped

Wait and Weight 16.0 ppg Kill Mud

Driller’s Method 16.0 ppg Kill Mud

Concurrent Method 16.0 ppg Kill Mud


0 1110 1110 1110 1110

100 1128 1131 1131 1130

213 1149 1152 1152 1908

413 1008 1197 1163 1555

513 971 1253 1199 1408

680 1444 1678 1619 1607

758 221 780 660 430

858 109 780 639 224

971 0 780 624 0

1071 0 678 624 0

1184 0 561 624 0

1284 0 458 603 0

1384 0 355 582 0

1584 0 150 562 0

1684 0 46 535 0

1729 0 0 468 0

1942 0 0 312 0



Figure 4.12 Comparison of Kill Methods

2913 0 0 156 0

3884 0 0 0 0

Table 4.2 Casing Pressures Expected (psi)



Driller’s Method 16.0 ppg Kill Mud

Concurrent Method 16.0 ppg Kill Mud




l ulus ert e ed sure

ure aches

lus well

at drill pipe. sides drill asing se a not be

n. l he se of efore, h sides

ance

Of the three methods used, the wait and weight method using the proper kill weight mud results in the least amount of casing pressure and the least borehole stresses. The casing pressures are lower using the wait and weight method with 16.0 ppg kill weight mud than they are if the driller’s method and 16.0 ppg kilweight mud are used. The reason is that the kill weight mud reaches the annwhile the influx is still in the hole, and this heavier kill weight mud helps to exadditional hydrostatic pressure on bottom. The additional hydrostatic pressurexerted by the kill weight mud means that the choke pressure (surface impospressure) can be held at a lower value and still maintain the bottom hole presat the desired value. Using the concurrent method allows lower casing pressvalues than the driller’s method. This is because some of the heavier mud rethe annulus before the gas bubble is out of the hole. Since this heavier mud (15.2 ppg) is less than the kill weight mud (16.0 pg), the casing pressures arehigher than those encountered when using the wait and weight method.

This brings up an additional interesting point. Since heavier mud in the annuseems to allow the use of lower casing pressures, why not kill the well with agreater-than-necessary mud weight? Most engineers agree that overkilling a(using a greater-than-necessary mud weight to kill the well) has no tangible benefit, and may, in fact, be detrimental to the kill operation. The reason is thoverkilling a well causes a higher bottom hole pressure to be exerted on the pipe side due to the extra hydrostatic pressure exerted by the mud in the drill The bottom hole pressure is held constant on both the drill pipe and annulus of the “U”. The two bottom hole pressures are also held equal to one anotherduring the well kill. Since the bottom hole pressure exerted by the mud in the pipe is higher than necessary, higher choke pressures must be held on the cside in order to keep the system in balance. In fact, overkilling a well can cauconsiderable increase in borehole stresses. Excessive safety factors should included in the kill mud. Only enough safety factors should be included to overcome any errors in pressure gauge readings on the rig. If a trip margin isdesired, it can be added while the mud is conditioned following a kill operatioOverkilling a well is the same as having a slug in the drill pipe. When the drillpipe is slugged, mud flows from the drill pipe into the annulus. The mud levefalls in the drill pipe until it is low enough for the bottom hole pressure to be tsame as the annulus side bottom hole pressure. In the case of overkill, the uthe choke precludes any hydrostatic pressure decrease in the drill pipe. Thermore choke pressure must be used to keep the bottom hole pressure on botequal.

The conclusions reached in this section are as follows:

1. The wait and weight method, using only the mud weight necessary to balthe formation pressure, allows lower casing pressures to be imposed.

2. Overkilling a well has no tangible benefit and may be detrimental.3. If a trip margin is to be added, it should be added after the well is dead.



ent to nnel dient be

Using the same well and casing pressure data, a table of equivalent mud weights at various depths was compiled.

It should be evident that the choke pressure imposed at the surface has a pronounced effect on the equivalent mud weights at various depths. The equivalent mud weights at the shallower well depths are particularly affected by the choke pressure. In order to kill any kicks safely, the equivalent mud weights at any depth in an open hole must not be allowed to exceed the fracture gradients at that particular depth. A 5000-foot string of casing with a fracture gradient at the shoe of 17.0 ppg would not have been sufficient to allow the well to be killed, because the equivalent mud weight at 5,000 feet reached 19.4 ppg. The formation would have broken down at initial shut-in producing a “down-hole blowout.”

A casing string must be set at a depth which has a high enough fracture gradiexceed the maximum anticipated mud weight at that depth. Often, field persoassume that the difference between the existing mud weight and fracture grain weakest exposed part of the well is equal to the amount of kick which can tolerated. This is not true, particularly with only surface pipe set in the well.

Example:


Last casing set = 3,500 feet

Fracture gradient at the weakest point (3,500 feet) = 13.0 ppg

Total depth = 10,000 feet

Question:

Table 4.3 Equivalent Mud Weights at Various Depths vs. Barrels of Mud Pumped - Wait and Weight Method - 16.0 ppg Kill Mud - Gas Kick


1000 ft 5000 ft 12,000 ft 15,000ft

0 36.3 19.3 16.8 16.0

100 36.7 19.3 16.8 16.0

213 37.1 19.4 16.2 16.0

413 34.4 18.9 16.0 16.0

513 33.7 16.8 16.0 16.0

680 28.8 16.2 16.0 16.0

758 18.3 16.0 16.0 16.0

858 17.1 16.0 16.0 16.0

971 16.0 16.0 16.0 16.0



, the n

si

r an g ture

to

is s the ud at

feet r

tly rill P can

Can we tolerate a 3.0 ppg kick?

Solution:

A 3.0-ppg increase in pore pressure at 10,000 feet corresponds to a shut-in drill pipe pressure of 1,560 psi. The 1,560 psi is felt equally at all points in the system, because the system is a closed, balanced “U.” Thereforepressure felt by the formation at 3,500 feet is equal to the hydrostaticpressure exerted by the mud at 3,500 feet plus the 1,560 psi of shut-ipressure.

Pressure at 3500 ft = (10.0 ppg × .052 × 3500) ft + 1560 psi = 3380 p

3380 psi at 3500 feet is equivalent to a .966-psi/ft pressure gradient o18.6-ppg equivalent mud weight. Obviously, we cannot stand a 3.0-ppkick even though the present mud weight is 3.0 ppg less than the fracgradient.

Question:

If we are unable to tolerate a 3.0 ppg kick, what size kick are we abletolerate?

Solution:

The fracture gradient at 3,500 feet is 13.0 ppg. The mud weight in use10.0 ppg. Therefore, the increase in pressure which can be tolerated idifference between the hydrostatic pressure exerted by a 10.0 ppg m3,500 feet and the hydrostatic pressure exerted by a 13.0 ppg mud at3,500 feet.

(.052 × 13.0 ppg × 3500 feet) - (.052 × 10.0 ppg × 3500 feet)

= 2366 psi - 1820 psi

= 546 psi

The 546 psi is the maximum casing pressure which can be withstood at 3500with 10.0 ppg mud in the well. An increase in mud density will result in a lowecasing pressure tolerance. If no influx occurs (i.e., if the kick is caught instanand the well is shut-in instantly) the shut-in casing pressure and the shut-in dpipe pressure are numerically equal. A 546-psi SIDPP is the maximum SIDPthat can be tolerated with 10.0 ppg mud in the well. The size of the kick whichbe tolerated prior to circulation is:

546 psi × 19.23TVD



e

that o

oast llbore.

lent

d by

e

e

ppg

where TVD = true vertical depth of the well

546 psi × 19.23 = 1.05 ppg10,000 feet

A 1.05 ppg kick is the maximum kick which can be shut-in safely under thgiven well conditions. Circulation adds limits as described in the followingsection.

4.7.2 Kick Tolerance

Kick tolerance factor is the maximum allowable pressure or its equivalent ppgthe weakest point in a wellbore can withstand, which is based upon having ninflux of formation fluid in the wellbore. If an influx of formation fluid has occurred, then the actual kick tolerance factor will become less. In the Gulf Carea the last casing set is normally assumed to be the weakest point of a we

The kick tolerance factor is computed by the following method:

1. Using the casing seat as the weakest point in the well, convert its equivappg fracture gradient into psi fracture pressure.

2. Using the present mud weight, determine the hydrostatic pressure exertethe mud at the casing shoe.

3. Subtract the hydrostatic pressure exerted by the mud from the psi fracturpressure. The answer obtained is the maximum allowable pressure (kicktolerance factor).

4. To express the kick tolerance factor in ppg, divide the maximum allowablpressure by .052 times the true vertical depth of the well.

Example:

TVD = 12,000 feet

Present mud weight = 13.0 ppg

Weakest point in the well (last casing shoe) has a fracture gradient of 15.0at 7,000 feet.

Question:

What is the kick tolerance factor and its equivalent ppg?

1. Equivalent fracture gradient at 7,000 feet is 15.0 ppg.

Psi required to break the formation down is:

Fracture pressure = 15.0 ppg × .052 × 7,000 feet = 5,460 psi

2. Hydrostatic pressure (HP) exerted by the mud at 7,000 feet is:



ny

nd ve t of gas

e vier ues to

g he the he r may

the

until the t mud

HP = 13.0 ppg × .052 × 7,000 feet = 4,732 psi

3. Subtract the HP from the fracture pressure to obtain the maximum allowable pressure (kick tolerance factor).

Kick tolerance factor = 5460 psi - 4,732 psi = 728 psi

4. Convert 728 psi kick tolerance factor into equivalent ppg.

728 psi = 1.17 ppg.052 × 12,000 feet

A 1.17- ppg kick is the maximum size kick which can be handled. If ainflux has occurred in the annulus, this size kick cannot be handled without breaking the formation down.

4.7.3 Saltwater or Oil Kicks

There is a pronounced difference between what happens during a gas kick awhat happens during an oil or saltwater kick. The oil or saltwater does not hathe expansion properties of a gas, so casing pressures do not rise as a resulexpansion. The casing pressure resulting from an oil or saltwater kick is its maximum value at initial shut-in. The casing pressure remains constant at thinitial shut-in value until either the top of the influx reaches the surface or heamud reaches the annulus. The casing pressure then begins to fall and continfall at a rate depending upon the amount of influx still in the annulus and the hydrostatic pressure exerted by the mud in the annulus.

If the Wait and Weight Method is being used to kill an oil or saltwater kick, thecasing pressure will fall once kill weight mud reaches the annulus. The casinpressure will continue to fall until the kill weight mud reaches the surface. If tConcurrent Method is used, the casing pressure will begin to fall either whenfirst of the heavier mud reaches the annulus or the top of the influx reaches tsurface. Depending upon mud system weight-up, the casing pressure may onot decline continuously when the Concurrent Method is used. If the driller’s method is used, the casing pressure falls when the top of the influx reaches surface and continues to fall steadily until the influx is removed from the wellbore. The casing pressure then remains constant and equal to the SIDPPthe first of the kill weight mud reaches the annulus. Once kill weight mud is inannulus, the casing pressure then declines at a steady rate until the kill weighreaches the surface, at which time the casing pressure falls to zero.

Assume the following wellsite conditions exist:

Hole diameter = 81/2 inches

Drill pipe OD = 41/2 inches



Drill pipe ID = 3.826 inches

Total depth = 15,000 feet


Pump output = .15 bbl/stk

Kill rate pressure = 1,000 psi at 20 stks/min

Pit gain = 25 bbl

SIDPP = 780 psi

SICP = 960 psi

Surface stack in use. For purposes of simplicity, the hole and pipe diameters are assumed to be constant.

The following calculation were made:

Drill pipe capacity = 213 bbl

Capacity of the annulus = 758 bbl

Total mud in well = 971 bbl


Length of influx = 495 feet

Influx gradient = Mud gradient - (SICP - SIDPP)Length of influx

= .78 psi/ft - (960 psi - 780 psi)495 feet

= .78 psi/ft - .36 psi/ft

= .42 psi/ft influx gradient

The influx gradient indicates that the kick is probably a mixture of saltwater and oil. Therefore, no influx fluid expansion should occur.

The following table of expected casing pressures versus amount of kill mud pump was constructed using the data above. The calculations were based on using the Wait and Weight Method.

Table 4.4 16.0 ppg Kill Weight Mud Casing Pressures Expected with Oil/Saltwater Kick

Barrels of Mud Pumped Casing Pressure Expected (psi)

0 960

100 960

213 960

413 752



The well data is exactly the same as that mud in Table 4.2 (Wait and Weight column) with the exception of changing the type of wellbore fluid influx.

Note: No expansion occurs and that the casing pressures are constant at the initial shut-in value until the kill weight mud reaches the annulus.

Once kill weight mud reaches the annulus, the casing pressure begins a continuous decline which lasts until the well is dead (kill weight mud at the surface).

Using the same well data used to compile Table 4.4 and Table 4.5, which gives the equivalent mud weights at various depths in the well versus the amount of mud pumped was compiled.

Note: The equivalent mud weight is constant at the required level at 15,000 feet. A comparison of Table 4.3 with Table 4.5 shows lesser borehole stresses at most points in the well. In almost all cases, an oil or saltwater kick will result in lower stresses on the wellbore than would occur with a gas kick.

513 649

680 477

758 219

858 116

971 0

Table 4.4 16.0 ppg Kill Weight Mud Casing Pressures Expected with Oil/Saltwater Kick

Barrels of Mud Pumped Casing Pressure Expected (psi)

Table 4.5 Equivalent Mud Weights at Various Depths versus Barrels of Mud Pumped - Wait and Weight Method - 16.0 ppg Kill Weight Mud - Combination Oil and Saltwater Kick


1000 ft 5000 ft‘ 12,000 ft 15,000 ft

0 33.5 18.7 16.5 16.0

100 33.5 18.7 16.5 16.0

213 33.5 18.7 16.25 16.0

413 29.5 17.9 16.0 16.0

513 27.5 16.8 16.0 16.0

680 24.2 16.15 16.0 16.0

758 19.2 16.0 16.0 16.0

858 17.2 16.0 16.0 16.0

971 16.0 16.0 16.0 16.0


Well ControlSpecial Problems in Well Control

e ke rns.

lue, und.

evel

m

iven f

4.8 Special Problems in Well Control

This section deals with problems that require special handling during a kill operation. The special problems considered are:

1. Lost returns

2. Plugged drill pipe or plugged bit3. Washed out or plugged choke4. Hole in the drill pipe5. Excessive casing pressure6. Drill pipe off bottom or out of the hole7. Gas bubble migration and expansion

If a problem does arise during the kill operation, knowledge of all the alternative solutions to that problem will help the operation go more smoothly and will help to realize the stated objectives of the well control operation.

4.8.1 Lost Returns

Lost returns is one of the most serious problems encountered in drilling operations. When lost returns occur in conjunction with abnormal pressure or a kick, the problem is serious indeed.

Lost returns may make it possible to maintain sufficient length of the mud column to obtain the required hydrostatic head. The influx fluid may enter the lost returns zone before it can reach the surface, causing “an underground blowout.”

During routine drilling, the condition of lost circulation or lost returns is fairly obvious and easily detected by the loss in volume of drilling fluid in the surfacpits. Under abnormal pressure or kick conditions, (circulating through the cholines to reserve pit, for example), which masks normal indications of lost retuOther indications of lost returns under kick conditions may be:

1. Increasing casing pressure followed by a sudden decrease to a lower vaprobably indicating a formation fracture - relieving the pressure undergro

2. Sudden reduction in drill pipe pressure caused by a sudden drop in fluid lin the annulus with the resulting “U” tube effect on the drill pipe side.

3. General wide fluctuation of drill pipe and casing pressure. Also results frosudden changes in “U” tube effects.

The detection of lost returns may depend upon a combination of the above gfactors. Oftentimes, especially if returns are only partially lost, the detection olost returns may be difficult.



In order to make any decision regarding remedies to a lost returns problem, the location of the zone which is taking mud must be known. Gulf Coast operators generally assume the loss zone is at or near the last casing shoe. However, this may not always be true. A number of methods of loss zone detection exist.

A radioactive tracer may be pumped down the drill pipe, through the bit, and up the annulus. It should enter the loss zone when it reaches that zone in the annulus. The loss zone can then be detected by wireline radioactivity detection devices. The disadvantage to this method is that the wellbore may be contaminated with radioactivity, which makes pinpointing the exact location of the loss zone difficult.

Temperature surveys may also be run on a wireline and used to locate a loss zone. The theory behind a temperature survey is that fluid from deeper, hotter zones is entering a shallower, cooler zone. As the wireline probe is lowered, the temperature increases at a fairly steady rate until the loss zone is encountered. As the loss zone is encountered the temperature increases sharply.

Figure 4.13 Use of Temperature Survey to Detect Loss Zone

If lost returns occur, fluid flow above the loss zone will normally cease. In an underground blowout situation, the fluid flow is taking place between the kicking zone and the loss zone. This fluid flow naturally creates some noise. A noise log which is lowered on a wireline will indicate very little noise above the loss zone. Once the probe is opposite the loss zone, the noise intensity increases. A disadvantage to this type of survey is the sensitivity of the noise probe. Any extraneous surface noise can cause severe distortion in the noise log.

If no pipe is in the wellbore, a loss zone may be detected mechanically by running a spinner survey. The spinner will detect fluid motion mechanically.



Killing a Well with Lost Circulation Problems by Curing the Lost Circulation First

Once a loss zone location has been pinpointed, the operator is faced with a decision of whether to control the well first and worry about the lost returns later, or whether it will be necessary to cure the lost returns problem prior to killing the well.

If an operator elects to cure the lost circulation problem first, he has a number of alternatives available to him. Among the alternatives are: lost circulation material, squeezes, chemical or cement squeezes, and time.

Once the bottom of the influx is above a section of the wellbore, the stresses imposed against that section decrease.

Note: This is true only for the wait and weight method of kick control. If the returns loss is partial, use of a light hand on the choke and continuing ahead as planned with the well control procedure may be sufficient to effect a cure for the problem. This type of cure will only be effective in areas where the rocks exhibit some plasticity. Fractures in many of the types of formation on the Gulf Coast can be healed with the simple application of time and the relief of stress. In hard rock areas the formations are not generally as plastic as Gulf Coast formations. Time and the relief of stress against a loss zone will probably not be sufficient to cure a lost circulation problem in this type of formation.

In hard rock country, lost circulation material may be useful in combatting a lost circulation problem. These types of rocks generally require plugging of the fracture or isolation of the loss zone before returns can be regained. Lost circulation material in sufficient quantities may be effective in plugging the fracture. Pills consisting of lost circulation material can be pumped down the drill string and spotted in the loss zone, or they can simply be bullheaded down the annulus and forced into the lost circulation zone. The amount of lost circulation material used to form a pill varies from about 5 ppb to about 60 ppb, depending upon the characteristics of the loss zone and lost circulation material.

Another method of curing a lost circulation problem prior to killing a well is to spot a high solids squeeze or a gunk squeeze in the loss zone. When a mud which exhibits a high filtration rate characteristics is subjected to pressure, liquid will be squeezed from the drilling fluid providing there is a filter medium of sufficient permeability to allow the passage of the liquid phase of the drilling mud. The loss zone, in this case, provides the permeable medium for liquid to be squeezed out of the mud, a filter cake is deposited on the permeable medium itself. This filter cake deposit consists of the solids which were originally associated with the liquid in the mud. When high filtration rates are in evidence, a great deal of liquid is squeezed out of a mud, and a large amount of solids are deposited in the form of a filter cake (Figure 4.14 and Figure 4.15).



Figure 4.14 Before Filtration

Figure 4.15 After Filtration

In Figure 4.15 (after filtration) the filter cake is deposited on the face of the sand. The sand presents enough of a permeable medium to allow the passage of any liquid squeezed from the mud as a result of differential pressure (Pm - Pf0).

A cure for lost circulation which uses a high filtration rate requires, spotting this pill opposite the loss zone, and applying differential pressure to effect the filtrate loss. The solids which are deposited as a result of filtration plug the fractures in the loss zone and enable normal circulation to be restored. Pressure should be



allowed to build up and should be held on the loss zone for several hours. If squeeze pressure does not build up, this technique will not be successful. The volume of the pill normally varies from 50 to 200 barrels, depending upon the amount of uncased hole in the well and the extent of fracturing in the loss zone.

Killing a Well Prior to Curing Lost Circulation Problems

There are two major approaches that involve killing a well prior to curing a lost circulation problem. One approach involves isolation of the kicking zone by placing a barite or cement plug above the kicking zone. The lost circulation problem is then worked on. Once the problem of lost circulation is solved, the plug can be redrilled with sufficient mud weight to control the formation pressures which initially caused the kick. The second major approach involves placing a slug of heavy mud between the kicking zone and the loss zone. This mud should have high enough density to exert enough hydrostatic pressure to balance the kicking formation. Once the kicking formation is balanced by hydrostatic pressure, the lost circulation problem which exists uphole can be worked on.

Probably the most common and effective technique which can be used in sealing off a kicking zone is the setting of a barite plug. A barite plug consists of water and barite. The barite is designed to settle out once the plug has been spotted in the open hole. The barite which settles forms an impermeable bridge above the kicking zone which isolates the kicking zone from the rest of the wellbore. Sometimes a thinner is also added to the barite plug slurry because mud already present in the wellbore may be thick enough to suspend the barite in the plug when it mixes with the mud. If the barite in the plug is suspended, settling out of the barite will not occur and the bridge cannot form. The barite plug should a density of 18.0-22.0 ppg. If possible, the plug density should be around 18.0 ppg because an 18.0 ppg barite plug has better settling characteristics than a 22.0 ppg barite plug. A detailed procedure which is used to spot the barite plug in the wellbore is given below:

1. Choose the desired slurry weight.

2. Decide on the volume of slurry to be used. 500 barrels is a good guideline to use for a plug length of 150 feet to 200 feet in the hole.

3. Calculate the barrels of slurry required and add 10+ barrels extra to compensate for hole washout.

4. Mix the barite through the cement pump hopper directly into the drill string.5. Pump the barite plug slurry down the drill pipe with the cement pumps at 6 to

12 barrels per minute and bleed and equal volume of mud through the choke on the annulus side. (On technique is simply to hold the casing pressure constant at its value prior to beginning the displacement.)



6. Note the initial drill pipe pressure after the pump has been brought up to the desired displacement rate, keeping the pump rate constant. If a gas bubble reaches the surface prior to completing the placement of the barite plug, the choke can be adjusted to hold the drill pipe pressure constant at whatever value it had when the displacement started.

7. Follow the barite plug slurry with a mud weight of calculated kill weight or higher. This will allow the drill pipe to be kept under control following the spotting of the plug.

8. Underdisplace and leave about 2 barrels of plug slurry in the drill pipe.9. Pull up out of the plug.10. Hold back pressure at the surface and allow about 8 hours for the plug to

bridge and solidify.11. Once a plug is formed, work on the lost circulation problem. An operator

should be prepared to keep accurate volume counts during the displacement operation. Provision should also be made to switch immediately to the rig pumps if the cement pump malfunctions. Any delay in switching pumps may allow the plug to solidify in the drill pipe.

Another possible solution to a lost circulation problem involves the spotting of a heavy slug of mud between the kicking zone and the loss zone. If the distance between the two formations is great enough, the hydrostatic pressure exerted by a shortened column of heavy mud on bottom may be sufficient to balance the formation pressure. Once the kick is controlled, the lost circulation problem can be worked on (Figure 4.16).

Figure 4.16 Spotting Heavy Mud Below Loss Zone



The hydrostatic pressure which must be exerted by the mud in order to control the well is 6,760 psi. The is no mud above the loss zone, which is at 3,500 feet. This leave the bottom 6,500 feet of the well to work with. In this case, 6,500 feet of mud must be spotted below the loss zone, and this mud must exert 6,760 psi of hydrostatic pressure. This corresponds to a 1.04 psi/ft hydrostatic pressure gradient or a 20.0 ppg mud weight. The surface system should be weighted to 20.0 ppg and then pumped down the drill pipe. Continue pumping until the first of the 20.0 ppg mud is calculated to enter the loss zone. When this occurs, the well should be dead. The lost circulation problem can then be attacked without danger of a blowout.

In order for this method to work, there must be enough height difference between the kicking zone and the loss zone for a shortened column of mud to exert enough hydrostatic pressure to balance the formation pressure in the kicking zone. If the distance between the two respective formations is relatively short, unrealistically high mud densities will be required, and this method will not work. The kicking zone will either have to isolated beneath a plug or the lost circulation cured.

Natural Forces Acting to Bridge a Well

One of the functions of a drilling mud is to exert sufficient hydrostatic pressure against exposed formations to hold the hole open. When lost circulation occurs, the hydrostatic pressure exerted against the formations in the well is reduced and the hole may cave and bridge. Such a bridge can effectively separate the upper hole from the pressure zone. In a sense, then, time is an ally because it allows nature to use its own mechanism for effectively isolating the loss zone and the kicking zone. The major drawback to this occurring is stuck pipe and being unable to circulating through the drill string.

4.8.2 Drill Pipe Plugged or Bit Plugged

If a kick is being circulated out and the drill pipe pressure suddenly increases with no appreciable change in casing pressure, the problem is probably a result of a bit jet partial plugging or partially plugged drill pipe. This problem can be recognized by a lack of change in the casing pressure gauge.

There are two different alternative which may be used to combat this problem.

1. A decision can be made to live with the problem until the well is killed.

a The pump can be slowed down while holding the casing pressure at a constant value. Once a new circulating pressure is established at the reduced rate, use the newly obtained drill pipe pressure in subsequent kill sheet calculation and kill operations. This will probably necessitate redoing the drill pipe pressure schedule and new pump rate.



b If the increase in drill pipe pressure which resulted because of the plugging can be tolerated at the old pump rate, note the new value of drill pipe pressure and redo the kill sheet to accommodate the pressure changes.

2. If the plugging is complete or nearly so and the pressures cannot be tolerated, then either the jets must be blown out of the bit (if the jets are what is plugged), the drill pipe backed off above the area that is plugged, or the drill pipe perforated. If perforations or backing-off are anticipated, care must be taken to insure that the perforations or back-off points are deep enough that mud of reasonable density can be used to kill the well. A back-off or perforations that are significantly above the bit will require a higher kill weight mud because of the shortened length of the mud column.

4.8.3 Washed or Plugged Choke

Sand and sloughing shale which entered the wellbore can have adverse effects on choke performance. Sand, especially when it travels through a choke opening at high velocity, is very abrasive and can wash out a choke. Sloughing shale tends to plug the choke and choke manifold.

Recognizing a choke problem is a relatively simple matter because choke problems affect both the drill pipe and casing pressures in the same manner. If the choke becomes washed out, closing the choke will not cause the increase in drill pipe pressure and casing pressure which would normally be expected. A plugged choke will prevent or reduce the decrease in drill pipe and casing pressures which would normally be expected as the choke opening is widened.

If the problem is not too severe and pressures can be kept in the desired ranges, it may be possible to tolerate the choke problem until the well is dead. If the choke is only partially plugged, it may be sufficient to simply lower the pump speed, obtain new circulating pressure figures, and continue the kill. If the choke is partially washed out, it may be possible to restrict the opening slightly and continue as planned.

If the choke obviously requires repair or cleaning out, another choke can be substituted and the kill continued. In instances where only one choke is available, it will be necessary to close the master valve going to the choke manifold until repairs can be made to the choke. After the necessary repairs have been effected, the well kill operation can be continued as planned.

4.8.4 Hole in the Drill Pipe

If a hole develops in the drill pipe during a kill operation, remedial actions must be taken immediately. The main symptom associated with this type of problem is



y

e

d okes hole

bing

an be

ty e is

en e

res

ipe) of the ipe re

e with

d

fill

a sharp reduction in drill pipe pressure with no commensurate reduction in casing pressure. Allowing the problem to go uncorrected will eventually result in a “washout” which will make it impossible to circulate kill mud to the bit and maeven result in parting of the drill string and resultant fish in the hole.

The most conventional technique used to correct this problem is to pump somsoft line down the drill pipe. The soft line follows the fluid flow and will flow intoa hole in the drill pipe. When the soft line reaches the hole in the drill pipe anseals it, the drill pipe pressure should increase immediately. Counting the strit takes to pump the soft line down gives a good indication of the depth of the in drill pipe.

If the use of soft line is not successful, it may be necessary to run a string of tudown into the original drill string. A packer is affixed to the end of the tubing. Once the packer is positioned beneath the hole in the drill pipe, the packer cset and the kill operation can be continued through the tubing.

If absolutely necessary, the drill pipe can be stripped out of the hole, the fauljoint replaced, and the pipe stripped back in the hole. If a back pressure valvnot already in the string, a wireline bridge plug can be run.

4.8.5 Drill Pipe Off Bottom or Out of the Hole

A kick which occurs when the bit is significantly off bottom (during a trip or whout of the hole) is difficult and often impossible to kill. The reason is that mudcannot be circulated below the bit. This results in a shortened column of mudwhich must be of high density if the well is to be controlled. If the bit is a longway from bottom, the mud density required to effect a kill is so great that it isimpossible to formulate. The drill pipe must be worked back to bottom with thpreventers closed.

If the drill pipe in the well has insufficient weight to overcome wellbore pressuand friction against the preventer elements, the pipe has to be forced into thewellbore. This process is called snubbing. Snubbing (forced insertion of drill pis necessary whenever the wellbore pressure times the cross-sectional area pipe in the well exceeds the weight of the pipe in the well, thus pushing the pout of the hole. If the pipe will slack off on its own without forcing, the proceduof running it through the closed preventers into a wellbore under pressure is termed stripping. Stripping and/or snubbing are the procedures which must bused to get the pipe to bottom if it is anticipated that the well cannot be killed a shortened mud column.

It must be remembered that if a kick occurs when the bit is off bottom, the muweight already in the hole is probably high enough to contain the wellbore pressure. After all, the mud weight was high enough to drill that far. Good hole


Well ControlShallow Gas Hazards

procedures and checks to be sure that the hole is not swabbing can eliminate the problem of kicks with the bit off bottom. If a bubble enters the wellbore and is below the bit, the bubble cannot be circulated out until the bit is below the level of the bubble, and it may, in fact, be impossible to kill the well without first working the bit down to a point where mud can be circulated beneath the bubble.

One method of working the pipe to bottom is the volumetric method. As pipe enters the wellbore, it displaces mud which is already present in the wellbore. If the mud which the pipe displaces is not released from the wellbore, higher pressures will develop in the wellbore. The amount of mud released should be equal to the amount displaced by pipe entering the wellbore. The problem with this method is that relatively small volumes are involved, and it is very difficult to bleed the exact amount necessary through the choke. More mud than necessary is generally bled through the choke, which results in additional fluid influx into the wellbore.

The second method of allowing displaced mud to leave the wellbore is called the pressure method. A cementing pump is rigged up to the choke line and pressure is brought up to a level slightly greater than the level which is imposed on the choke by the wellbore. The return line is rigged up to the cement mixing tank. The mast valve to the choke line is then opened. Since the cement pump is holding a slightly higher pressure on the choke than that imposed by the wellbore, no additional influx occurs. As pipe is moved (stripped/snubbed) into the wellbore, the mud that the pipe displaces results in increased wellbore pressure being imposed on the choke. When the wellbore pressures exceed the cement pump pressure, fluid will escape the wellbore and enter the return line running to the cement suction tank. The mud volume in the cement suction tank can be accurately monitored to insure that the correct volume of mud is leaving the wellbore. As the pipe enters the influx bubble, a large volume increase will be noted because of the increase in vertical height of the bubble. Once the pipe is through the bubble, the influx can be circulated from the well using a standard kill procedure.

4.9 Shallow Gas Hazards

Shallow exposed formation often have extremely low fracture gradients. In deep water drilling operations or in cases in which the gap between the flowline and mean sea level is large, these already low fracture gradients are lessened even further due to decreased overburden pressure gradients. This combination of factors often results in formation fracture gradients which are too low to withstand the hole stresses imposed as a result of shutting in a kicking well. If formation fracturing does occur as a result of shut-in, the possibility exists that these fractures may broach to the surface and place the personnel and rig in jeopardy.



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gas hen neath ccur

Shallow gas reservoirs are usually high pressure, low volume accumulations. The combination of low fracture gradients and difficulty in detecting a shallow pressured gas zone further enhances the hazards involved. Seismic data and offset well histories have aided considerably in the detection of those shallow pressure gas zones, but the operator still needs contingency plans in case one of these reservoirs is penetrated without prior warning. Contingency plans for encountering shallow pressured gas zones should include at least the following considerations:

1. Can the well be shut-in or should it be diverted? The fracture gradient must be known or closely estimated in order to make this decision correctly.

2. If the drilling operation is to be carried out from a floating rig, should a marine riser be used in a diverter operation or should diversion be carried out subsea.

4.9.1 Shut-In Versus Diversion

The decision either to divert or to shut-in depends on the fracture gradient in the weakest exposed section of open hole. A known fracture gradient can be translated into a maximum allowable casing pressure figure which should never be exceeded in shallow formations due to the danger of inducing fractures which broach the surface. The maximum allowable casing pressure can be calculated by using the following formula:

Maximum allowable casing pressure = (FG - MW) × .052 × D

where:

FG = fracture gradient in ppg

MW = mud weight in use (ppg)

D = depth of weakest exposed zone in the well (TVD)

In the Gulf Coast and in most other areas, the formation directly beneath thecasing shoe is usually assumed to be the weakest exposed portions in the wellbore. Due to the low fracture gradients which exists in the formations direbeneath drive pipe and conductor pipe seats, chances are good that any shua kick would result in exceeding the maximum allowable casing pressure. Therefore, MMS Order 2 requires that provisions be made to divert mud andsafely downwind in the event of a kick occurs prior to setting surface pipe. Wa fracture induced as a result of a shut-in broaches to the surface, erosion beone or more legs of a platform or jackup may occur. Loss of buoyancy may oif a floating rig is being used. In any event, fire is a possibility. Therefore, diversion, though risky, may be less hazardous than attempting to shut-in a shallow kick.



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In those cases in which a floating rig is being used, and the location can be abandoned quickly, an operator may on occasion attempt to shut-in a kick which occurs when drilling shallow hole. The operator’s reasoning is that diversion risky procedure. If shut-in can be accomplished without fractures broaching tosurface, the chances are good that the well can be killed using conventional techniques, thus minimizing the risk of dealing with a potentially disastrous surface blowout. If broaching does occur, the operator simply moves off locaThe decision to attempt shut-in of a shallow kick from a highly mobile floating is often a value judgement, and all factors affecting this decision need to be considered most carefully. In most cases, the risks involved in diversion are lthan those involved in the attempted shut-in of a shallow well kick.

4.9.2 Use of the Marine Riser

In floating drilling operations, the operator is confronted with several alternatiin dealing with shallow gas hazards. First, the operator must decide whether oto use a marine riser while drilling shallow hole. Secondly, if the operator elecuse a marine riser, he must decide whether to attempt to divert kicks subseadivert kicks at the surface. Each alternative procedure has advantages and disadvantages which must be weighed carefully when decisions are made.

Suppose an operator elects to use a marine riser during his initial drilling operations. There are advantages unrelated to well control which occur with use of a riser. Use of a riser allows treatment of the returning mud stream anconsiderable savings in time and money in those instances in which sea watalone is unsatisfactory as a drilling fluid. In addition, formation samples and gmay be examined and evaluated at the surface as drilling progresses.

Use of a marine riser while drilling shallow holes does pose some disadvantaregarding well control. Gas may cause the mud in the riser to unload. This rein decreased hydrostatic pressure acting against the kick which allows the inrate to increase. Higher pump rates are necessary to outrun kicks having higrates of fluid influx. Unloading the mud in the riser also allows the hydrostaticpressure exerted by the water outside the riser to act against the riser wall, thraising the possibility of riser collapse. If the operator elects to attempt to contshallow kick by spotting a column of heavy mud above the kick zone, the possibility exists that excess heavy mud may accumulate in the riser, resultinlost circulation, an even worse condition.

There are arguments which indicate that dispensing with a marine riser and drilling blind may be the best way to proceed when attempting to drill shallowportions of a wellbore with a floating rig. The presence of the water assures tsome hydrostatic pressure is always available to act against the shallow kickformation. The possibilities of riser collapse and borehole unloading are thuseliminated. This practice allows sufficient time for the well to bridge or deplet



only

The operator also has sufficient time to attempt to control the well by spotting a shortened column of heavy mud beneath the mudline. The primary disadvantage involved with drilling ahead blind in shallow hole without a marine riser is that a gas kick may result in reduced rig buoyancy due to the presence of gas bubbles in the water beneath the rig. Those who advocate dispensing with the riser in shallow portions of the well, however, agree that reduced buoyancy does not present severe danger to a drilling vessel because ocean current is usually sufficiently strong to carry all of the gas cut water safely away.

4.9.3 Diverter Operation

Use of a diverter system presumes that the formation fracture gradients are too low to withstand shut-in pressures resulting from a shallow kick.

Floating rigs requiring diverter systems can be rigged up to divert either at the ocean floor or at the surface. The surface diverter system, which consists of a bag type preventer and vent lines mounted above the riser pipe may be preferable to a subsea diverter system for the following reasons:

1. If diverter vent lines are run from the ocean floor to the surface, pressure losses will develop in the vent lines during diverter operations. This may cause high equivalent mud weights in weak sections of the open hole and result in an underground blowout.

2. If the formation fluids are vented at the ocean floor through shortened vent lines, reduced buoyancy of the drilling vessel may result. Although this solution negates the possibility of riser collapse and high pressure losses, the venting of fluids directly below the drilling vessel may not be an acceptable alternative in some cases. The ocean currents may not be sufficient to carry vented fluids safely away from the rig.

Since a diverter operation does not result in the imposition of surface pressure to counteract formation pressure, the operator has only three (3) chances of successfully controlling the well.

1. He may be able to spot enough mud in the annulus above the kicking zone to balance the formation pressure.

2. The shallow reservoir may deplete itself before too much time has passed.3. The hole may bridge, thus sealing off the kicking zone.

Possibility number one generally involves pumping some heavy mud down the drill pipe and into the annulus in hopes enough of this heavy mud can be spotted to stop the well flow. Some operators have adopted the practice of mixing several hundred barrels of heavy reserve mud prior to spud-in and keep this mud on board for possible use during a diverter operation. Possibilities two and three are natural events over which the operator has little control. If the operator is unable to balance the formation pressure with mud hydrostatic pressure, the operator’s


Well ControlGas Bubble Migration and Expansion

objective is to divert the kick safely downwind until the hole bridges over or the reservoir depletes.

A diverter operation should be carried out in the following manner:

1. If a kick is suspected, pick up the kelly high enough to clear any tool joints which may be opposite the sealing element on the diverter bag type preventer.

2. If the well is flowing, open the downwind diverter vent line.3. Close the bag type preventer. (You must be sure that at least one of the vent

lines is completely open before the bag preventer closes on the drill pipe. Failure to do this may result in an underground blowout.)

4. Pump mud own the drill pipe at an increased pump rate. Many operators keep a pit of heavy reserve kill mud for use in diverter operations. Keep pumping mud down the drill pipe until the well stops flowing. If you pump away the reserve kill mud, and the well continues to flow, switch immediately to the active pit and keep pumping. If the well is still flowing after the entire system has been pumped away, switch to sea water. Pumping should then be continued at an increased rate until the flow stops.

Under no circumstances should both diverter lines be closed on a kicking well. Diverter systems should be designed so that one or both vent lines are completely open prior to the time the bag type preventer closes.

Diverter systems should also be tested at frequent intervals for proper functioning. Since diverters are not designed as high pressure assemblies, no maximum test pressures are specified.

4.10 Gas Bubble Migration and Expansion

At conditions of standard temperature and pressure, the volume occupied by a gas multiplied by the pressure of that gas is equal to a constant value. Symbolically, the relationship is:

where: PV = constant

P = pressure of the gas

V = volume occupied by the gas

Carrying this logic a bit further, we can state that:

PiVi = PfVf

where: Pi = initial pressure of the gas

Vi = initial volume occupied by the gas

Pf = final pressure of the gas



Vf = final volume occupied by the gas

As the pressure confining a certain amount of gas is decreased, its volume increases. For example, consider a one barrel volume of gas which has a pressure of 5,200 psi downhole. According to the formula, this gas would have a volume of 347 barrels when it reaches the surface because the only pressure confining the gas at that point is atmospheric pressure (15 psi).

Under oilfield conditions, the volume occupied by a given gas also depends on the temperature of the gas and the compressibility of the particular gas. The formula used to account for these two additional variables results in modification to the original PV = K gas law formula. The modified formula is then:

where: Pi = initial pressure of gas

Vi = initial volume of gas

Zi = initial compressibility of gas

Ti = initial gas temperature

Pf = final pressure of gas

Vf = final volume of gas

Zf = final gas compressibility

Tf = final temperature of gas

This particular formula is only generally used to predict maximum casing pressures.

Since gas is lighter than mud, gas will tend to rise or percolate up through a column of mud if given sufficient time. The rate at which gas migrates depends heavily on mud properties and composition of the gas itself. The maximum rate at which a gas bubble will normally rise through a column of mud on a shut-in well is generally assumed to be about 1,000 ft/hr. However, this figure may vary greatly under different circumstances.

If a kicking well can be shut-in without lost returns or equipment failure, it is often assumed that all the conditions will remain stable indefinitely and that the well can be killed almost at leisure. Gas migration on a shut-in well can change this assumed stable condition to an unstable and dangerous situation.

In order to understand the effects of gas migration on a shut-in well, consider the following example.

Example: Well depth = 10,000 ft

PiVi

ZiTi

----------PfVf

ZfTf

----------=



r’s thing. ulus

states he is still

Formation pressure = 5,200 psi


At initial shut-in, assume the following conditions:

SIDPP = 520 psi

SICP = 600 psi

Influx is gas

1. The pressure in the gas bubble at initial shut-in is equal to the formation pressure (Figure 4.17).

Figure 4.17 Pressure in the Well with a Gas Bubble at Initial Shut-In Equal to the Formation Pressure

At this time, the formation pressure is balanced by the pressure of the gas which is in the wellbore. The gas itself is confined by the combination of mud hydrostatic pressure and surface imposed pressure.

2. Five hours later, the gas has migrated 5000 feet up the hole. The operatorepresentative has spent all this time waiting on orders, and has done noSince no mud has been pumped or bled off, the volume of mud in the annhas not changed. The volume of gas has not changed either. The gas lawthat PV = constant. Therefore, if the volume of gas is not changed, then tpressure is also unchanged. At this point, the pressure in the gas bubble 5200 psi. The formation sees the following (Figure 4.18).



Figure 4.18 Pressures After the Gas Bubble has Migrated 5000 Feet

The pressure in the gas bubble acts uniformly in all directions. Since the gas pressure is the same as it was initially, the pressure confining the gas must also be the same. The pressure confining the gas results from a combination of surface imposed pressured and hydrostatic pressure exerted by the mud above the bubble. Since the hydrostatic pressure exerted by the mud above the bubble has decreased due to gas migration, the surface imposed pressure must increase to compensate. The formation on bottom now feels the pressure in the gas bubble plus the hydrostatic pressure exerted by the mud below the bubble. Thus, the bottom hole pressure on the annulus side is not equal to 7,540 psi. Since the system is a closed, balanced U-tube, the drill pipe pressure also increases. Note that the shut-in pressures on both sides have increased over initial values by equal amounts. The increased surface imposed pressure results in dramatic increases in the equivalent mud weights at various points in the wellbore.

3. If the bubble is allowed to migrate all the way to the surface without allowing any expansion, the following wellbore conditions will result (Figure 4.19).



Figure 4.19 Pressures After the Gas Bubble has Migrated to the Surface Without any Expansion

At this point, the formation feels the pressure of the gas bubble plus the hydrostatic pressure of the 9,829 feet of mud now beneath the bubble. The drill pipe side of the U-tube also reflects an equal amount of increased surface imposed pressure.

Gas migration is recognized by noting the increase in shut-in pressures on both the drill pipe and casing sides. During gas migration, both pressures will continue to increase equally until the bubble reaches the surface, the formation breaks down, casing burst or equipment failure occurs. In most cases the bubble will not reach the surface before one of the latter possibilities becomes reality.

If the bit is on bottom when a kick occurs, handling gas migration is a relatively simple matter. As the shut-in drill pipe pressure increases to values above that necessary to balance formation pressure, small amounts of mud should be bled from the annulus side to relieve the excess drill pipe pressure. Mud should be bled in amounts of less than one barrel. Bleeding mud through a manual choke and directing this mud into a calibrated tank is one way of accurately gauging the amounts bled off. Mud should be bled whenever the shut-in drill pipe pressure rises significantly above its initial shut-in value. Bleeding small amounts of mud from the annulus each time the well pressure is bled off helps to insure that no additional influx occurs as a result of the bleeding operation.

In those instances in which the drill pipe pressure gauge cannot be used as a direct indicator of bottom hole pressure (i.e., pipe off bottom as out of the hole, drill pipe or bit plugged, float value in use), the procedure for handling gas migration becomes more complicated. Gas migration can be recognized by noting increases



in casing pressures to values higher than those at initial shut-in. The position of the gas bubble in the wellbore must be estimated and the number of barrels of mud required to exert a given hydrostatic pressure must be known before a procedure can be implemented.


Appendix A

Appendix A SPWLAR Recommended Abbreviations for Lithology Descriptions

Word Abbreviation Word Abbreviation

above ab barite(ic) barabsent abs basalt(ic) Bas, basabundant abd basement Bmacicular acic become(ing) bcmafter aft bed(-ed) Bd, bdagglomerate Aglm bedding Bdgaggregate Agg belemnites Belmalgac, algal Alg, alg bentonite(ic) Bent, bentallochem Allo bioclastic bioclaltered alt biothem(-al) Bioh, biohalternating altg biomicrite Biomiamber amb biostrom(-al) Biost, biostammonite Amm biotite Biotamorphus amor bioturbated bioturbamount amt birdseye Bdeyeamphipora Amph bitumen(-inous) Bit, bitand & black(-ish) blk, blkshangular ang blade(-ed) Bld, bldanhedral ahd blocky blkyanhydrite(ic) Anhy, anhy blue(-ish) bl, blshanthracite Anthr bored(-ing) Bor, boraphanitic aph botryoid(-al) Bot, botapparent apr bottom Btmappears ap boudinage boudgapproximate apprx boulder Bldaragonite arg boundstone Bdstarenaceous aren brachiopod Brachargillaceous arg brackish brakargillite argl branching brhgarkose(ic) Ark, ark break Brk, brkas above a.a. breccia(-ted) Brec, brecasphalt(ic) Asph, asph bright brtassemblage Assem brittle britassociated assoc brown brnat @ bryozoa Bruauthigenic authg bubble Bublaverage Av, av buff buband(ed) Bnd, bnd bulbous bulb

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company A-1January 2001

Appendix A

burrow(-ed) Bur, bur color colcalcarentie Clcar common comcalcareous calc compact cpctcalcilutite Clclt compare cpcalcirudite Clcrd concentric cncncalcisilitite Clslt conchoidal conchcalcisphaera Casph concretion(-ary) Conc, conccalcisphere Clcsp conglomerate(-ic) Cgl, cglcalcite(-ic) Calc, calctc conodont Conocaliche cche conquina Coqcarbonaceous carb conquina(-iod) Coqidcarbonate crbnt considerable conscarbonized cb consolidated consolcavem(-ous) Cav, cav conspicuous conspiccaving Cvg contact Ctccement(-ed, -ing) Cmt, cmt contamination(-ed) Contamcenter(-ed) Cntr, cntr content Contcephalopod Ceph contorted cntrtchaetetes Chaet coral, coralline Cor, corinchalcedony(-ic) Chal, chal core cchalk(-y) Chk, chky covered covcharophyte Char cream crmchert(-y) Cht, cht crenulated crenchitin(-ous) Chit, chit crinkled crnlkchitinozoa Chtz crinoid(-al) Crin, crinalchlorite(-ic) Chlor, chlor cross xchocolate choc cross-bedded x-bdcirculate(-ion) Circ, circ cross-laminated x-lamclastic clas cross-stratified x-stratclay(-ey) Cl, cl crumpled crpldclaystone Clst crystal(-line) Xl, xlnclean cln crystocrystalline crpxlnclear clr cube(-ic) Cub, cubcleavage Clvg cuttings ctgscluster Clus cypridopsis Cypcoal C dark dk, drkcoarse crs dead ddcoated(-ing) cotd, cotg debris Debcoated grains cotd gn decrease(-ing) Decr, decrcobble Cbl dendrite(-ic) dendcolonial coin dense dns


A-2 © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Appendix A

depauperate depau feet ftdescription Descr feldspar(-athic) Fspr, fsprdesication dess fenestra(-al) Fen, fendetrital detr ferro-magnesian Fe-magdevitrified devit ferruginous ferrdiabase Db fibrous fibrdiagenesis(-etic) Diagn, diagn fill(-ed) fldiameter Dia fine(-ly) f, fnlydisseminated dissem firm frmdistillate Dist fissile fisditto " or do fleggy flgdolomite(-ic) Dol, dol flake(-ky) Flk, flkdolostone dolst flat fldominant(-ly) dom flesh flsdrill stem test DST floating fltgdrilling drlg flora Flodrusy dru fluorescene(-ent) Fluor, fluorearthy ea foliated folEast E foot Ftechnoid Ech foraminifer Foramelevation Elev foraminiferal foramelongate elong formation Fmembedded embd fossil(-iferous) Foss, fossendothyra Endo fracture(-d) Frac, fracequant eqnt fragment(-al) Frag, fragequivalent Equiv framework frmwkeuhedral euhd frequent freqeuryamphipora Euryamph fresh frsexinic eux friable frievaporite(-itic) Evap, evap fringe(-ing) Frg, frgexcellent ex frosted frosexposed exp frosted quartz F.O.G.extraclast(-ic) Exclas, exclas fucoid(-al) Fuc, fucextremely extr fusulinid Fusextrusive exv gabbro Gabfacet(-ed) Fac, fac galeolaria Galfaint fnt gas Gfair fr impression impfault(-ed) Flt, flt in part I.P.fauna Fau geopetal geptfavosites Fvst gilsonite Gil



Appendix A

girvanella Girv indurated indglass(-y) Glas, glas inoceramus Inocglauconite(-itic) Glauc, glauc insoluble inslglobigerina(-inal) Glob, glob interbedded intbdgloss(-y) Glos, glos intercalated intercalgneiss(-ic) Gns, gns intercrystalline intxingood gd interfragmental intfraggrading grad intergranular intgrangrain(-s, -ed) Gr, gr intergrown intgngrainstone Grst interlaminated intrlamgrainte Grt interparticle intpargrainte wash G.W. interpretation intptgranule(-ar) Gran, gran intersticies inststgrapestone grapst interval Intvlgraptolite Grap intraclast(-ic) Intclas, intclasgravel Grv intraparticle intrapargray, grey(-ish) Gry, grysh intrusive intrgraywacke Gwke invertebrate Invtbgreasy gsy iridescent iridgreen(-ish) gn, gnsh ironstone Fe-stgrit(-ty) Gt, gt irregular(-ly) irrgypsum(-iferous) Gyp, gyp isopachous isohackly hkl ivanovia Ivanhalite(-iferous) Hal, hal jasper Jasphard hd joint(-d, -ing) Jt, jtheavy hvy kaolin(-itic) Kao, kaohematite(-ic) Hem, hem lacustrine lacheterogeneous hetr lamina(-itions, ated) Lam, lamheterosteqina Het large lgehexagonal hex laterite(-itic) Lat, lathigh(-ly) hi lavender lavhomogeneous hom layer Lyrhorizontal hor leached lchdhornblende hornbd lens, lenticular Len, lenthydrocarbon Hydc lentil(-cular) lenigneous rock Ig, ig light ltimbedded imbd lignite(-itic) Lig, liginch in limestone Lsinclusion(-ded) Incl, incl limonite(-itic) Lim, limincreasing incr limy lmyindistinct indst lithic lit



Appendix A

lithographic lithgr milky mkylithology(-ic) Lith, lith mineral(-lized) Min, minlittle Ltl minor mnrlittoral litt minute mnutlocal loc moderate modlong lg mold(-ic) Mol, molloose lse mollusc Molllower l mosaic moslumpy lmpy mottled mottlustre Lstr mud(-dy) md, mdylutite Lut mudstone Mdstmacrofossil Macrofos muscovite Muscmagnetite, magnetic Mag, mag nacreous nacmanganese Mn no sample n.s.marble Mbl no show n/smarine marn no visible porosity n.v.p.marl(-y) Mrl, mrl nodules(-ar) Nod, nodmarlstone Mrlst North Nmaroon mar novaculite Novacmassive mass numerous nummaterial Mat occasional occmatrix Mtrx ochre ochmaximum max odor odmedium m or med oil Omember Mbr oil source rock O.S.R.meniscus men olive olvmetamorphic(-osed) meta, metaph olivine olvnmetamorphic rock Meta oncolite(-oidal) Onc, oncmetasomatic msm ooid(-al) Oo, oomica(-iceous) Mic, mic oolicast(-ic) Ooc, oocmicrite(-ic) Micr, micr oolite(-itic) Ool, oolmicro mic oomold(-ic) Oomol, oomolmicro-oolite Microol opaque opmicrocrystalline microxin orange(-ish) or, orshmicrofossil microfos orbitolina Orbitmicrograined micgr organic orgmicropore(-osity) micropor orthoclase Orthmicrospar Microspr orthouartzite O-Qtzmicrostylolite Microstl ostrcod Ostrmiddle Mid overgrowth ovgthmiliolid Milid oxidized ox



Appendix A

oyster Oyst primary primpackstone Pkst prism(-atic) prispaper(-y) Pap, pap probable(-ly) probparaparchites Para production Prodpart(-ly) Pt, pt prominent promparticle Par pseudo oolite(-ic) Psool, psoolparting Ptg pseudo- psparts per million PPM pumicestone Pstpatch(-y) Pch, pch purple purppearly prly pyrite(-itized, itic) Pyr, pyrpebble Pbl pyrobitumen Pyrbitpelecypod Pelec pyroclastic pyrclpellet(-al) Pel, pel pyroxene pyrxnpelletoid(-al) Peld, peld quartz(-ose) Qtz, qtzpendular(-ous) Pend, pend quartzite(-ic) Qtzt, qtztpentamerus Pent radial(-ating) Rad, radpermeability(-able) Perm, perm radiaxial Radaxpetroleum pet range rngphlogopite Phlog rare rphosphate(-atic) Phos, phos recemented recemphreatic phr recovery(-ered) Rec, recphyllite (-ic) Phyl, phyl recrystallized rexizdpin-point (porosity) p.p. red(-ish) rd, rdshpink(ish) pk, pksh reef(-old) Rf, rfpisoid(-al) Piso, piso remains Rempisolite(-ic) Pisol, pisol renalcis Renpitted pit replaced(-ment) Rep, repplagioclase Plag residue(-ual) Res, resplant Plt resinous rsnsplastic plas rhomb(-ic) Rhb, rhbplaty plty ripple Rplpolish(-ed) Pol, pol rndd,frosted,pitted r.f.p.pollen Poln rock Rkpolygonal poly round(-ed) rnd, rnddpoor(-ly) P rubble(-bly) Rbl, rblporcelaneous porcel rubist Rubporosity (porous) Por, por rugose rugporphyry prphy saccharodial saccpossible(-ly) poss salt(-ly) Sa, sapredominant(-ly) pred salt and pepper s&ppreserved pres salt cast(-ic) sa-c



Appendix A

salt water S.W. sphaerocodium Sphaersame as above a.a. sphalerite Sphalsand(-y) Sd, sdy shperule(-itic) Spher, sphersandstone Sst spiclue Spicsaturation(-ated) Sat, sat splintery Splinscales sc sponge Spgsacphopod Scaph spore Sposcarce scs spotted(-y) sptd, sptyscattered scat stachyode Stachschist(-ose) Sch, sch stain(-ed, -ing) Stn, stnscolecodont Scol stalactitic stalsecondary sec strata(-ified) Strat, stratsediment(-ary) Sed, sed streaming stmgselenite Sel striae(-ted) Stri, striseptate sept stringer strgrshadow shad stromatolite Stromiltshale(-ly) Sh, sh stromatoporoid Stromshell Shl structure Strshelter porosity Shlt por styliolina Stylioshow shw stylolite(-itic) Styl, stylsiderite(-itic) Sid, sid sub sbsidewall core S.W.C. subangular sbangsilica(-iceous) Sil, sil sublithic sblitsize sz subrounded sbrnddsheletal skel sucrosic sucslabby slb sugary sugslate(-y) Sl, sl sulphur(-ous) Su, suslickenside(-d) Slick, slick superficial oolite Spfoolslight(-ly) sli, slily surface Surfsmall sml syntaxial synsmooth sm syringopora syringsoft sft vermillon vermsolenopora Solen tabular(-ate) tabsolitary sol tan tnsolution, soluble Sol, sol tasmanites Tassomewhat smwt tension tnssorted(-ing) srt, srtg tentaculties TentSouth S ternginous terspar(-ly) Spr, spr texture(-d) Tex, texspare(-ly) sps, spsly thamnopora Thamspeck(-ed) Spk, spkld thick thk



Appendix A

thin thn vertebrate vrtbthin section T.S. vertical vertthin-bedded t.b. very vthroughout thru very poor sample V.P.S.tight ti vesicular vestop Tp violet vitough tgh visible vistrace Tr vitreous(-ified) vittranslucent trnsl volatile volattransparent trnsp volcanic rock Volctrilobite Tril vug(-gy) Vug, vugtripoli(-itic) Trip, trip wackestone Wksttube(-ular) Tub, tub washed residue W.R.tuff(-aceous) Tf, tf water Wtrtype(-ical) Typ, typ wavy wvyunconformity Unconf waxy wxyunconsolidated uncons weak wkunderclay Uc weathered wthdunderlying undly well Wlunidentifiable unident West Wuniform uni white whupper u with w/vadose Vad without w/ovariation(-able) Var, var wood Wdvaricolored varic yellow(-ish) yel, yelshvariegated vgt zeolite zeovared vrvd zircon Zrvein(-ing, -ed) Vn, vn zone Znveinlet Vnlet



Appendix B

SD B-1Ja

ATa

rdness Porosity Oil Show

S ntation or ation

Intergranular Possible

S nsolidated Intergranular Possible

S ntation Intergranular Possible

C - 7 on ’s scale

none none

L Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Companynuary 2001

ppendix B Classification Tablesble B.1 Classification of Arenaceous Deposit and Chert

Rock Type ColorCrystal or Grain Size

Major and MinorCharacteristics Ha

iltstone WhiteGrayGreenBrownGray greenGray brown

Silt size by definition

Quartz VarietyPyriticGlauconiticCoal InclusionsCarbonaceousArgillaceous

Common VarietyPyriticGlauconiticCoal InclusionsCalcareousDolomitic

CemeIndur

and ClearYellowPink

Grain size Angularity Sorting

MineralsClay Matrix

Unco

andstone ClearWhiteGrayGreenBrownGray greenGray brown

Grain size AngularitySorting

MineralsClay Matrix

Ceme

hert WhiteGrayAmberBrownSpotted

Microcrystalline by definition

TransparencyPyrite inclusions

AngularitySplintery

Conchoidal Fracture

HardMOH

Appendix B

SDL Applied FundamentalsJanuary 2001


ee of action

stict

mrd

Not applicable Oil shale in only a few known areas

ic Not applicable None

ic Not applicable None

B-2 © 2001 Sperry-Sun, a Halliburton Company

Table B.2 Classification of Argillaceous Sediments



Shale GreenGrayBrownGray greenGray brownRedYellowBlackBlue

See Definition CalcareousPyriticGlauconiticSiltySandyCarbonaceousMicaceousFossiliferousCoal Inclusions

WaxeyEarthyLaminatedBandedRoughGrittySmoothBrittle

Degrcomp

1. pla2. sof3. fir4. ha

Clay GreenGrayBrownGray greenGray brown

See Definition CalcareousCarbonaceous

SiltySandy

Glauconitic

PlastSoftFirm

Marl GreenGrayBrownGray greenGray brownYellowBlueBlack

See Definition SiltySandy

CarbonaceousGlauconitic

PlastSoftFirm

Appendix B

SD B-3Ja

Ta


C ated or ionally

nsolidated

Intergranular and Moldic porosity

Possible

C ated or ionally

nsolidated

Intergranular and Moldic

Possible

C plastic ated

Chalky and pin-point porosity

Possible


ble B.3 Classification of Limestone



alcirudte WhiteGrayBuffTanBrownGray brown

Larger than 2 mm in diameter

ArgillaceousCarbonaceous

PyriticGlauconitic

Silty or sandyFossil Fragments

DolomiticMicriteSparite

Induroccasunco

alcarenite WhiteGrayBuffBrownGray brownTan

Sand size 1/16 to 2 mm


PyriticGlauconitic

Silty or sandyFossil fragments

DolomiticMicriteSparite

Induroccasunco

alcilutite BrownBuffTanWhiteGray

Silt and/or clay size 1/10000 to 1/16 mm


PyriticGlauconitic

Silty or sandyDolomitic

MicriteSparite

Soft,indur

Appendix B



ated times osic and e

Intercrystalline vuggy, fracture, etc.

Possible


’s scale 3

CaCO3 ary with acteristics

Intercrystalline and other possibilities

Possible

’s scale 3

CaCO3 ary with acteristics

Intercrystalline and other possibilities

Possible


Table B.4 Classification of Dolomite



Dolomite WhiteBuffTanGrayBrown

Crystalline Micro-XLN to VC-XLN

MineralsPyriteAnhydriteGypsumSaltGlauconiteCalcareousCarbonaceousArgillaceous

TexturesRelic fossilsSuccrosicVuggyStyoliticChalkyVeinletsVeins

Indursomesuccrfriabl

Table B.5 Classification of Limestone and Limestone Matrices



Micrite ClearWhiteBuffGrayTanBrown

Smaller than 0.01 mm


PyriticGlauconitic


Dolomitic

MOH

Purewill vchar

Sparite ClearWhiteBuffGrayTanBrown

Larger than 0.01 mm


PyriticGlauconitic


Dolomitic

MOH

Purewill vchar

Appendix B

SD B-5Ja

Ta


GC2

MOH’s Not applicable Probably

none

AC

rated Secondary fracture porosity

Possible if fractured


ble B.6 Classification of Sulfates



ypsum aSO4 - H2O

WhiteClearGray

Crystalline Amorphous

TransparencySalt inclusions

PlateyAnhydritic

Clay

(not found below approx. 3,000 ft.)

Soft2 onscale

nhydriteaSO4

WhiteBuffTanGray

Crystalline Amorphous

Pearly lusterDolomite inclusionsGypsum inclusions

Limestone inclusionsSalt inclusions

PyriticGlauconiticArgillaceous

Carbonaceous

Indu

Appendix B



Appendix C

Appendix C Buoyancy Factors

lb/galBuoyancy

Factorlb/gal

Buoyancy Factor

lb/galBuoyancy

Factorlb/gal

Buoyancy Factor

6.0 .9083 9.8 .8502 13.6 .7922 17.4 .73416.1 .9068 9.9 .8487 13.7 .7906 17.5 .73266.2 .9053 10.0 .8472 13.8 .7891 17.6 .73116.3 .9037 10.1 .8457 13.9 .7876 17.7 .72956.4 .9022 10.2 .8441 14.0 .7861 17.8 .72806.5 .9007 10.3 .8426 14.1 .7845 17.9 .72656.6 .8991 10.4 .8411 14.2 .7830 18.0 .72496.7 .8976 10.5 .8395 14.3 .7815 18.1 .72346.8 .8961 10.6 .8380 14.4 .7800 18.2 .72196.9 .8946 10.7 .8365 14.5 .7784 18.3 .72047.0 .8930 10.8 .8350 14.6 .7769 18.4 .71887.1 .8915 10.9 .8334 14.7 .7754 18.5 .71737.2 .8900 11.0 .8319 14.8 .7738 18.6 .71587.3 .8884 11.1 .8304 14.9 .7723 18.7 .71427.4 .8869 11.2 .8289 15.0 .7708 18.8 .71277.5 .8854 11.3 .8273 15.1 .7693 18.9 .71127.6 .8839 11.4 .8258 15.2 .7677 19.0 .70977.7 .8823 11.5 .8243 15.3 .7662 19.1 .70817.8 .8808 11.6 .8227 15.4 .7647 19.2 .70667.9 .8793 11.7 .8212 15.5 .7631 19.3 .70518.0 .8778 11.8 .8197 15.6 .7616 19.4 .70358.1 .8762 11.9 .8182 15.7 .7601 19.5 .70208.2 .8747 12.0 .8166 15.8 .7586 19.6 .70058.3 .8732 12.1 .8151 15.9 .7570 19.7 .69908.4 .8716 12.2 .8136 16.0 .7555 19.8 .69748.5 .8701 12.3 .8120 16.1 .7540 19.9 .69608.6 .8686 12.4 .8105 16.2 .7524 20.0 .69448.7 .8671 12.5 .8090 16.3 .75098.8 .8655 12.6 .8075 16.4 .74948.9 .8640 12.7 .8059 16.5 .74799.0 .8625 12.8 .8044 16.6 .74639.1 .8609 12.9 .8029 16.7 .74489.2 .8594 13.0 .8013 16.8 .74339.3 .8579 13.1 .7998 16.9 .74179.4 .8564 13.2 .7983 17.0 .74029.5 .8548 13.3 .7968 17.1 .73879.6 .8533 13.4 .7952 17.2 .73729.7 .8518 13.5 .7937 17.3 .7356

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company C-1January 2001

Appendix C

C-2 © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Appendix D

ire” h the rvoir the

ud he this mits

ate that to

shing

Appendix D “Formation Evaluation by Analysis of Hydrocarbon Ratios” (Pixler Paper)

Introduction

Surface data logging was first offered commercially in August 1939. This logging method quickly gained favor among many operators because the type of fluid in the formation could be determined within minutes after the formation was drilled. The presence and magnitude of the methane show was and is the most important factor in mud log interpretation. However, this magnitude in some instances was improperly understood, and as a consequence some operators still do not use surface data logging, even though the early technique frequently made the difference between a successful well and an abandoned hole. Both the “hot wlog of gas combustibles in the sample and the percent-of-gas log obtained witconventional gas trap and the gas chromatograph indicate only that the resein question contains hydrocarbons. The methods do not necessarily indicatequantitative amounts of the various hydrocarbons in the mud.

The addition of a new Steam Still Reflux gas sampling system to gas chromatography enables accurate determination of the composition of the mgas sample. A knowledge of gas composition makes it possible to establish trelationship of methane to the heavier hydrocarbon shows. An awareness ofrelationship led to a new, additional mud log interpretative technique that perrelating the quantitative amounts of methane (C1), ethane (C2), propane (C3), butane (C4), and pentane (C5) to in-place reservoir fluid content.

A long-accepted premise is that as formations are drilled, the drilling mud filtrpartially flushes the formation fluid ahead of the bit. It was generally thought the formations were flushed to an irreducible minimum - generally consideredbe about 30 percent of in-place fluids. Experience in surface data logging, however, has shown that this rarely happens. This partial flushing does not prevent surface data logging from successfully determining productive or non-productive formations. Experienced logging engineers, in possession of quantitative gas analyses, make interpretations that take into account the fluthat results in rocks of various permeabilities, the effect of overbalanced mudweight and the effect of initial filtrate loss.

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company D-1January 2001

Appendix D

ple in the

of f the

e , and

esults

mple

ted of

ain f to a ing

ts to

rt, ort.

. The s more

Method

Ordinarily, when formation cuttings are drilled they retain much of the formation pore fluid. This fluid is released to the mud column as the cuttings travel up the annulus. Most of the formation fluid in the cuttings will be “produced” into thedrilling mud during the top 500 feet of hole travel. Conventionally, a mud samis diverted to a mechanically operated gas trap to obtain a sample of the gas mud.

The efficiency of this trap is from 15 to 70%, depending upon the gel strengththe mud, the amount of mud flowing through the trap and the rotation speed otrap impeller. The magnitude of the conventional gas show is, therefore, quantitative only to the air-gas sample obtained. The sample is accurately analyzed by the gas chromatograph; but, because the sample furnished by thconventional gas trap represents only a fraction of the gas present in the mudbecause that fraction is not representative of the total gases in the mud, the rare still only qualitative.

When the Steam Still Reflux Unit is used to obtain the gas sample, the gas sawill represent almost 100 percent of the hydrocarbon fractions C1 through C5 that were in the mud sample. This enables the chromatograph analysis to be relaquantitatively to the mud, and the readings to be reported as parts per millioneach hydrocarbon vapor (C1 through C5) to mud volume.

Because the cuttings from a particular formation “produce” the gas they continto the drilling mud, it was reasonable to assume that this same formation, icompleted, would produce gases of similar composition. This assumption ledcomparison of PPM logs of hydrocarbon vapors with similar data from producwells. Plots were made of the ratio of methane to each of the heavier hydrocarbons from many analyses of wellhead samples. These plots were compared with plots, made from PPM logs, of gas in mud. Both groups of ploshowed definite patterns between (1) the magnitude of the ratios of methaneeach of the heavier hydrocarbons, and (2) the slope of the lines of the plottedratios. These in turn, indicate productive potential and reservoir permeability.

The Steam Still Reflux Unit consists of a small steam boiler, mud-injection pomud-steam mixing chamber, Reflux-Condensing Unit and a gas-extraction pFive (5) milliliters (ml) of mud are injected into the purged mud-steam mixingchamber. The mud is rolled with 2,000 to 4,000 volumes of steam. The hydrocarbons (C1 through C5) extracted from the mud are collected at the Reflux-Condensing Unit, withdrawn with a syringe, diluted to the standard chromatograph sample size and injected into the chromatograph for analysisReflux-Condensing Unit removes only the lighter paraffin series hydrocarbonfrom the mud sample tested. For example, if the mud contains diesel oil, the complex hydrocarbons - C6 and above - condense and drop back into the

D-2 © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Appendix D

mud-steam mixing chamber. Therefore, regardless of whether the fluid phase of the mud is oil or water, the gas sample analyzed contains only the light fractions through C5, and the analysis is representative of the formation gas.

The full importance of determining formation gas composition has not always been apparent. At first it was observed that if the magnitude of butane in the mud was greater than the magnitude of either propane or ethane, the zone in question would produce water and hydrocarbons. Later, the ratios of methane to each of the heavier hydrocarbons components were plotted on semilog paper. Hydrocarbon ratio plots obtained from PPM logs and available data from wellhead gas sample analyses were compared. The comparison of the plots from PPM logs and wellhead gas analysis showed a striking correlation. The correlation demonstrated that PPM logs made with Steam Still-Reflux samples could be interpreted

The magnitude of the methane-to-ethane ratio determines if the reservoir contains gas or oil or if it is nonproductive. The slope of the line of the ratio plot of C1/C2, C1/C3, C1/C4 and C1/C5 indicates whether the reservoir will produce hydrocarbons or hydrocarbons and water. Positive line slopes indicate production; negative slope lines indicate water-gearing formations. An undersaturated reservoir may show a negative slope, but such occurrences are rare. The ratio plots may not be definitive for low permeability zones, but unusually steep plots indicate tight zones. A ratio of C1/C2 between 2 and 15 indicates oil. A ratio of C1/C2 between 15 and 65 indicates gas. The lower the C1/C2 ratio, the richer the gas or the lower the oil gravity. If the ratio of C1/C2 is below about 2 or above about 65 the zone is nonproductive.

Figure 1 Hydrocarbon ratio plots obtained from wellhead sample analyses, limestone


Appendix D

Figure 2 Hydrocarbon ratio plots, productive reservoirs, South Texas reservoirs, Rocky Mountain area

Field Examples

Figure 1 shows average hydrocarbon ratio plots from limestone reservoirs in the Rocky Mountain area. Plot 1 is derived from analyses of gases from Mississippian oil-producing reservoirs. The C1/C2 ratio is 3.5. The slope of the line is again positive and not steep. Plot 2 was obtained from analyses of gases from wells producing gas-condensate from the Silurian. The C1/C2 ratio is 12; the line slope is again positive and not steep. Plot 3 is from gas-condensate wells producing from the Ordovician. The C1/C2 is 15 and, again, the slope of the line is not steep; all three plots show slopes favorable to production. Plot 4 shows ratios obtained from an analysis of gas from the Lower Ordovician, which produced gas and water. The plot shows a negative slope of the section from the C1/C4 ratio to the C1/C5 ratio. Many tests have verified the fact that if a ratio plot shows a negative slope, the zone in question is water-bearing.

Figure 2 shows plotted hydrocarbon ratios for productive reservoirs in South Texas. Plot 1 was made from an analysis of a wellhead sample of gas-condensate produced from a Frio sand, Hidalgo County. The production is rich in liquid hydrocarbons as indicated by the low C1/C2 ratio. Plot 2 is from an analysis of a wellhead gas sample from a 11,000 ft oil reservoir, North Lindsey field. The pentane was not reported, but the low C1/C2 ratio indicates oil production. Plot 3 was obtained from a gas show at 12,690 ft on the PPM log of the State Tract 49 No.1 Well, Nueces County, Texas. Formation tests resulted in gas production.


Appendix D

Experience shows that if the C1/C2 ratio is above 65 the zone is too tight for commercial production. Figure 3 shows the ratio plots obtained from PPM logs on the Texas Gulf Coast wells that were nonproductive in the zones of interest. Plot 1 is from the PPM log of the R.A. Tally No.1 well, Victoria County, Texas. The C1/C2 ratio was 470. The zone was tested extensively but it was a low permeability reservoir that could not be commercially completed. Plots 2 and 3 are from the State Tract 49 No.1 well, Nueces County, Texas. Plot 2 was from a sand encountered at about 8,060 ft. The relatively high ratios of C1/C2, C1/C3, C1/C4, and C1/C5 indicated that the zone was nonproductive because of the low permeability. This was subsequently verified by testing. Plot 3 was obtained from a sand at 9,130 ft. The negative slope of the ratio plot, C1/C2 to C1/C3, indicated that the zone was water-bearing. Subsequent formation tests showed water and non-commercial amounts of gas.


Appendix D

Figure 3 Hydrocarbon ratio plots, non-productive reservoirs, South Texas - Evaluation of show

Plot 4 was obtained from the PPM log of the Kovar No.1 well, Victoria County, Texas. The sand encountered from which the plot was made is at 10,120 ft. The gas show appeared to be good, but a negative slope of the C1/C3 ratio to the C1/C4 ratio was positive identification of a water-bearing formation.

Evaluation Technique

It is apparent that with this evaluation system, potential production can be accurately predicted. The only significant time lapse between penetration of the formation and evaluation of its productive possibilities is the time required to pump the mud from the bottom of the hole to the surface and analyze it by the Steam Still-Reflux and chromatograph method. Figure 4 shows the evaluation technique, which may be described as follows.

First, record the net increase of each gas component over the background gas; next, plot the ratios C1/C2, C1/C3, C1/C4, C1/C5 on the ratio lines as indicated. Then evaluate, within the following limits, the section in question for probable production as indicated by the plotted curve:

1. Productive dry gas zones may show only C1, but abnormally high shows of C1 only are usually indicative of salt water.

2. If the C1/C2 ratio is low in the oil section and the C1/C4 ratio is high in the gas section the zone is probably nonproductive.

3. If any ratio (C1/C5 excepted if oil is used in the mud) is lower than a receding ration, the zone is probably nonproductive. For example, if C1/C4 is less than C1/C3, the zone is probably water-bearing.

4. The ratios may not be definitive for low permeability zones; however, steep ratio plots may indicate tight zones.


Appendix D

at l.

Figure 4 PPM log and report form for analyses from gas shows on PPM logs

Application

The PPM log is only one of many tools that are ordinarily used for formation evaluation. But in many instances, the PPM log has furnished the vital information necessary to make the final decision on a well. One well drilled in inland waters of Louisiana had what appeared on the PPM log to be a good sand body, but the PPM log showed only a nominal increase in gas. After the sand was penetrated and the well deepened, hole trouble was encountered. No other information of interest was available on the sand. The cost of the sidetracking to investigate the sand was sizable. Tight hole conditions and the low magnitude of the gas show indicated that the sand had good permeability and that possibly formation hydrocarbons had been flushed ahead of the bit. A plot of hydrocarbon ratios indicated oil production. Therefore, at considerable expense, the sand was investigated and a new oil field was found.

An interesting well drilled in St. Martin Parish, LA, was the No.1 St. Martin Bank and Trust located on the southeast flank of the Anse La Butte Dome. A good sand was encountered at about 8,000 ft showed oil, but the negative slope of the ratio plot indicated that the sand was water-bearing. The well was deepened to approximately 9,600 ft. One of the partners, a successful independent with a talent for finding oil by “feel” and by prudent use of the latest technology, decided ththe formations in which the well was being drilled were tilted to almost vertica


Appendix D

On his recommendation, the well was plugged back to about 7,000 ft and sidetracked. The sand that was drilled at 8,000 ft in the first hole was encountered in the directional hole at approximately 7,000 ft and the entire sand was hydrocarbon saturated.

The PPM log and the ratio plots from the sand in the sidetrack hole are shown in Figure 5. Table 1 shows the mud gas components related to percent of total gas. In actual practice, the ppm gas shows obtained from the PPM log are not converted to percent of total gas; but note the general decrease in percent methane in the lower section of the sand compared with that in the upper section. The magnitude of the gas show in the straight hole and in the sidetrack hole was significant. An accurate determination, however, of the composition of the gas in both cases led to correct conclusions on the potential productivity of the sand at the different depths in each hole. Note that the ratio Plot 1 at the top of the sand indicates a gas cap. As shown in Table 1, the gas was 93.1 percent methane. Subsequent plots indicated that production would be oil. In each of these cases the C1/C2 ratio was less than 9. The lowest ratio, 4.5, is shown in Plot 6, which was made from the show at the bottom of the sand.

Figure 5 PPM log and hydrocarbon ratio plots, No.1 St. Martin Bank and Trust Well, St. Martin Parish, LA.


Appendix D

y lots t to the cially t. The

lopes.

in the

Another example of the application of the PPM log is No.1 State Tract 198 well, Aransas County, Texas. Many sands were encountered showing the present of hydrocarbons. The logging crew submitted more than 60 ratio plots to the operator during the drilling of the well. In almost all instances subsequent information verified the logging engineers’ predictions of probable productivitbased on the ratio plots. Figure 6 shows a section of the PPM log and ratio pfor this well. The gas composition relating the percent of each gas componenthe total gas is shown in Table 2. Gas condensate production is indicated by PPM log and ratio plots as shown. The zones are tight marine deposits - espethe 10,520 ft zone. Plot 4 has the steepest line slope; pentane was not presenslope of Plot 3 is steep. Plots 2 and 5 show more favorable (less steep) line sThe electric log and subsequent formation tests made of each zone indicatedprobable production. The well was completed as a gas condensate producer11,300 ft section, which is the section plotted as No.5.

Table 1 Mud Gas Components, Percent of Total Gas

Depth (ft) C1 C2 C3 C4 C5

7,460 93.1 3.6 1.5 1.2 0.6

7,475 82.4 9.6 5.9 1.4 0.7

7,485 74.4 13.3 10.0 1.6 0.7

7,490 78.0 11.4 8.6 1.4 0.6

7,500 77.0 14.3 7.2 1.1 0.4

7,515 76.1 17.1 5.1 1.4 0.3


Appendix D

Figure 6 PPM log and hydrocarbon ratio plots, No.1 State Tract 198 well, Aransas County, Texas

Table 2 Mud Gas Composition, Percent of Total Gas

Depth (ft) C1 C2 C3 C4 C5

10,110 92.0 5.2 1.3 1.1 0.4

10,115 92.0 4.6 1.5 1.0 0.9

10,450 93.3 4.8 1.2 0.4 0.3

10,520 92.8 5.8 1.0 0.4 0.0

11,305 92.3 4.8 1.6 0.8 0.5


Appendix D

Conclusions

Only qualitative shows of hydrocarbons in the mud can be derived from conventual mud logs. If chromatography is used, only a general indication of in-place gas composition is obtainable. Such hydrocarbon shows may be reported as units of gas or percent hydrocarbons or parts per million (PPM) as in the air-gas mixture tested. Only the presence in relative amounts, not the actual quantity, of hydrocarbons in mud is indicated, and other supplemental information may be necessary to evaluate the formation in terms of potential productivity. However, if the composition of the gas sample obtained from the mud is representative of the in-place formation gas, then the gas analysis is accurate. The use of the Steam Still-Reflux Unit makes possible a report of formation gas composition on the PPM log. Meaningful ratio plots of gas composition can then be made. Even though many factors affect the amount of reservoir fluid released to the drilling mud, reservoir potential productive capabilities can be determined by a study of the ratio of methane to each of the heavier hydrocarbon components. The hydrocarbon ratio plot is a unique technique and provides the operator with new information for evaluating productive possibilities of exploratory wells.

Computer programs involving percent gas in mud (PPM log) and gas composition are being used in special cases to determine reservoir potential production. The use of computers in mud log interpretation, although new, will contribute significantly towards a better application of the data shown on the PPM log.


Appendix D


Appendix E

Appendix E “Wellsite Formation Evaluation by Analysis of Hydrocarbon Ratios”(Ferrie Paper)

Abstract

To be able to evaluate formation potentials and possible productivity, using the hydrocarbon ratios minutes after the drilling fluid attains the surface. Thereby decreasing the need for running expensive drilling operations (Drill Stem Test, cores, log runs) when formation potential is questionable. That is to say, the use of Drill Stem Tests, cores and log analysis can be minimized through this method.

Theory

That a knowledge of hydrocarbon ratios as they relate to formation fluids, enables a logging technician, on wellsite, to determine possible hydrocarbon shows: and that the relationship between quantitative amounts of methane (C1), ethane (C2), propane (C3), butane (C4) and pentane (C5) to in-place reservoir production and potential. Therefore, it is the presence in relative amounts, not the actual quantity of hydrocarbons in drilling fluids, that determine reservoir potential.

Introduction

In any discussion of the validity of different methods of hydrocarbon detection and evaluation, it is perhaps a good idea to try and envisage exactly what is taking place in the process of drilling a hole in the ground.

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company E-1January 2001

Appendix E

f the ount P,

n he re,

t of

d as of the

e of

e that e e past. ed

tion.

than

The original rock strata-reservoir or not - lies undisturbed before the advent of the bit, and our objective is to attempt to reconstruct the exact physical properties of this strata without interrupting the drilling operation to run a DST, core, etc.

As the bit approaches the strata that we are interested in, a phenomenon known as “flushing” occurs. This, in short, is simply a replacement of some of the pore fluids of the rock by some of the mud, and is caused by hydrostatic pressure omud column usually being in excess of that exerted by the formation. The amof flushing that takes place, depends on a number of factors, e.g., (depth, ROhole size, volume of mud being circulated, physical properties of the formatioand the mud, etc.) and in fact, is very difficult to estimate. However, despite tfact that some portion of the interstitial fluids are flushed away from the wellbothe formation will still contain some of these fluids when the bit finally does arrive.

At this point, the bit will mechanically break up the solid formation into small “cuttings” and, depending mainly on the porosity of the formation (but also onother factors) some oil and gas, if present, will be released into the mud. Mosthe interstitial fluids remain contained in the cuttings, however, being releasethe cuttings travel up the hole; the pressure on them being reduced from that hydrostatic head of the mud to atmospheric. Most of these fluids will be “produced” into the mud stream in the final 200 meters of travel, especially ifeffective permeability is present.

Some of the interstitial fluids, however, will remain in the cuttings, although greater importance is usually placed on the returning mud stream as a sourchydrocarbon information. We have, anyway, two places in which to look for evidence of hydrocarbons in economic quantities - the mud and the cuttings.

Discussion

It has been noted that it is the presence and magnitude of the show of methanis the most crucial factor in surface data logging interpretations. However, thmagnitude of this show has been the cause of some misunderstandings in thBoth the “hot wire” log of gas hydrocarbons and the percent-of-gas log obtainwith the conventional gas trap and the gas chromatograph indicate only that the reservoir in question contains hydrocarbons. There is no accurate method todetermine the quantitative amounts of the various hydrocarbons in the forma

We are of the opinion that, using a Steam Still, chromatograph, and Show Evaluation Report, a more complete and valid picture of the commercial possibilities of any formation can be gleaned from the gas in the mud, ratherany residual fluid in the cuttings. The method, briefly, is as follows:

E-2 © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Appendix E

er, h

for

mes. of

, Steam d

ses tion,

de of

rity e

e for

. ole nd

A 5-ml sample of mud is taken from as deep in the possum belly as possible - close to the flow line - and injected into the mixing chamber of the Steam Still, where it is swept by steam vapor about 2000 times its own volume. The mud is completely stripped of it’s hydrocarbon content, which collects in the condenswhence it is extracted by another syringe and injected into the chromatograpwhere the various components are accurately measured.

The aeration gas trap used in most logging operations is an efficient machineremoving most of the methane from the drilling fluid.

However, the heavier the hydrocarbon, the more inefficient the gas trap becoVariables such as, type of drilling mud, viscosity and density of mud, unstablepower supplies, drop-out and absorption in the trap sampling line, and effectstemperature, humidity, etc., all have an adverse affect upon the gas trap. Theefficiency of this system, under these conditions is anywhere from 15 to 70%Therefore, the aeration trap method is useful for establishing trends but not evaluating shows effectively.

The Steam Still and chromatograph will give a very accurate qualitative and quantitative reading of the volatile hydrocarbons in the drilling mud - methaneethane, propane, iso - and normal butane, and iso- and normal pentane. The Still is a very efficient method of doing this, is easy and simple to operate, anrequires only basic maintenance.

Because the cuttings of the formation “produce” virtually all the producible gathey contain into the mud, it is a reasonable assumption that this same formaif completed, would produce gases of similar composition.

Now, it has been observed that it is the composition, rather than the magnituthe gases in a “show” that is the important factor in terms of formation productivity. The relationship of methane to the heavier hydrocarbon gases isindicative of gas, oil or water productive potential, and in some cases, the reservoir permeability.

A comparison of the ratios of methane to the heavier hydrocarbons from producing wellheads and PPM logs produce a striking similarity. In this similalies the evidence that the hydrocarbon ratio pattern can be used to predict thproductive potential of a reservoir. The Show Evaluation Report is a simple, easy-to-interpret graphical method of outlining these ratios and is usually donevery significant gas show.

So far as the cuttings gas goes, however, the situation is somewhat differentAlthough they undergo a normal production cycle during their travel up the hin the drilling mud, the cuttings, on arrival at the surface, still contain a certainamount of the original oil and/or gas. These interstitial fluids will be containedwithin the pore-spaces of the cuttings, and will be released by the chopping abeating action of the blender.


Appendix E

, etc., the

ive ial,

hen ases ght

nd n of ning

ntial only

e 3

an

It is obvious that most of the volatile hydrocarbons will already have been produced from the cuttings by the time they reach the logging unit, unless the rock has very low permeability. However, much of the heavier liquid hydrocarbons will remain and, in fact, most Cuttings Gas Detectors can detect up to about C18. It is thus primarily an oil detector, and its readings are representations of the oil content of the cuttings obtained instrumentally - independent, that is, of human judgement.

We believe, however, that this is not that important - that a visual estimation by a qualified technician of any oil show in the cuttings can be done more easily, and to sufficient accuracy. Fluorescence under ultra-violet light with or without the aid of a leaching agent, the colour, nature and speed of the “cut,” leaching, stainingare all properties that can be easily investigated, and, put together, plotted onlog as a qualitative estimation of the amount of oil in the cuttings. A quantitatestimation has little value in that it is difficult to relate to any production potentand it’s accuracy, in any case, is doubtful.

Cuttings gas estimation, on the other hand, is useful to a certain extent, but tonly as a negative consideration. If you have negligible amounts of volatile gin the mud, but considerably more in the cuttings, you are looking at a very tiimpermeable formation - not exactly a potential reservoir.

To sum up then, the oil in the mud is given a qualitative examination by the logger, as is the oil in the cuttings. The gas in the mud is given a qualitative aquantitative examination, resulting in the case of a gas show, in an estimatiosome of the economic and productive capabilities of the formation. The remaigas in the cuttings is, for the above reasons, ignored.

Evaluation Method

We find then that we have available to us a viable method of determining poteproduction almost immediately upon penetration of the zone of interest. The significant time lapse is that interval taken for the drilling mud to travel to the surface, in order to be analyzed by the Steam Still and chromatograph. Figurshows the evaluation technique which can be described as follows:

To being with, record only the net increase of each gas over background gas; then calculate and plot the ratios on the ratio lines as indicated. Finally, the show c

C1 C1 C1 C1

C2 C3 C4 C5


Appendix E

then be evaluated, within bounds for probable production and potential, as indicated by the plot.

1. Productive dry gas zones may show only C1 but abnormally high C1 only shows are usually indicative of salt water.

2. If the C1/C2 ratio is low in the oil section and the C1/C4 ratio is high in the gas section, the zone is probably non-productive.

3. If any ratio (C1/C5 excepted, when oil is used in the mud) is lower than a preceding ratio, the zone is probably non-productive. For example, if C1/C4 is less than C1/C3, the zone is probably water bearing.

4. The ratios may not be definitive for low permeability zones; however, steep ratio plots may indicate tight zones.

Field Examples

Figure 4 shows the hydrocarbon ratio plots from a proven reservoir in the Fox Creek area from a well producing gas from the Lower Cretaceous. The C1/C2 ratio is over 15; the slope of the line is positive and moderately steep, but not overly. This sample of gas was taken from the flareline during a DST. The well tested at 202 mcf/d with gas to surface in 7 minutes. Plot #1 was obtained from analysis of fluid from the Upper Devonian. This well had produced through perforations in the production casing. The C1/C2, for Plot #2a, is slightly under 6. This is the ratio plot of fluid recovered from 3285m - 3304m and is indicative of gas condensate; the slope being moderately steep. The C1/C2, for Plot 2b, is slightly under 5; this is the ratio plot of fluid recovered from 3304m - 3311m and is indicative of light crude. The slight decrease in the latter portion of Plot 2b indicates the zone is possibly wet and may be down-dip.

Figure 5 shows plotted hydrocarbon ratios from a well drilled in the Karr Lake area. Plot #1 was made from an analysis of gases from the Lower Cretaceous. The C1/C2 ratio is slightly under 15; the line slope is even, positive and fairly steep. This may indicate poor permeability in this particular formation. Plot #2 was made from analysis of fluid from the Jurassic. The C1/C2 ratio is slightly under 3; the line is fairly flat and low in the oil section and indicates a more viscous crude, which may be water bearing. Both zones, however, appear to be producible with the Lower Cretaceous producing gas-condensate while the Jurassic produces oil and water.

Practical experience shows that if the C1/C2 ratio is above 65, the zone is too tight for commercial production or may only indicate very dry gas (mostly methane).

Figure 6 shows the ratio plots obtained from Alberta and B.C. wells that were non-productive in the zones of interest. The C1/C2 ratio for Plot 1 is slightly under


Appendix E

7; this is the ratio plot taken from the PPM log, of a well in B.C. The slope is obviously negative from C1/C3 ratio to C1/C4 ratio and is indicative of a water bearing formation and this turned out to be the case upon logging and testing. The C1/C2 ratio for Plot 2 is slightly over 70; this ratio plot was taken from the PPM log, of a well in B.C. The slope is again negative from C1/C3 to C1/C4 and did, in fact, indicate a water bearing formation. In both of these cases, however, the hot wire gas detector did show a substantial increase over background gas, and the formation would probably have been tested, had not the recommendation from the logging technician, been heeded. At first glance they appear to be reasonable shows, because of the magnitude of the hydrocarbons present, and the relatively good porosity of the sandstone indicated by the wellsite geologist. However, after show reports were accomplished, it is quite evident that if tested, the results would have indicated water bearing formations.

Applications

The PPM log is only one of several tools that can be used for formation evaluation. However, often times it can furnish the vital information necessary to make the final decision on a well. The author was on the wells indicated by Figure 1 and Figure 2 when totally unexpected shows of gas were encountered in the Lower Cretaceous. The total gas readings showed no great change in the amount of gas present, and the drill rate was not affected except for an anomaly at the top of the formation. When the Steam Still analysis was performed, the amount of heavy hydrocarbons increased greatly while the methane content decreased. Drilling continued until the total gas readings returned to normal, (as shown in Figure 2). Ratio plots were made as drilling progressed through the section noted and the results were relayed to the wellsite geologist. A Drill Stem Test was deemed necessary and one was performed with the results shown on the PPM log in Figure 2. A ratio plot was made later of the fluid recovered from the DST and confirmed the ratio plot made slightly after penetration of the formation. The result is noted by Figure 1. Plot 1 shows the ppm ratio performed by the logger minutes after the formation was penetrated, while Plot 2 shows the percentage of gases, realized by analysis from the DST. The interesting thing to note here is that without the PPM log this formation could have been passed by until the electric log analysis were available, increasing the chances of damaging the formation, etc.

Another example of the PPM log and ratio plot is taken from a well drilled in Western Canada. Many sands and carbonates were noted showing the presence of hydrocarbons. The logging crew submitted over several ratio plots to the operator during the drilling of the well. In most instances it turned out that DST and electric log analysis substantiated their findings. Figure 7 shows a plot of the PPM log and subsequent ratio plots with a corresponding table.


Appendix E

per tive , it is

e an be ctive each

ith

hen p and ing atio

t this ell.

Conclusions

As we have observed by the preceding examples, only qualitative trends can be established by using the conventional aeration gas trap and hot wire or hydrogen flame gas detector. If chromatography is used, we are then able to get an idea of the rough composition, in a gas to air ratio, and this is unsatisfactory for formation evaluation. Such hydrocarbons are usually reported as “units” of gas or partsmillion of gas in the gas-air mixture. We are only seeing the presence, in relaamounts, not the actual quantity of the hydrocarbons in the mud. In this casenecessary to have other forms of formation evaluation in order to deal with productive formation potential. However, if an accurate account of the in-plachydrocarbons is made available, then more meaningful ratio plots of gases cmade. Even though several factors affect the reservoir potential and its producapabilities; these factors can be lessened by studying the ratio of methane toof the heavier hydrocarbons. This plot is unique and provides the operator wnew and relevant information for evaluating productive possibilities of exploratory and frontier wells.

The ratio plot can also be used to aide the operator in his pre-well planning. Wa play is to be drilled, information can be gained from the study of wells in thearea to be looked at. Ratio plots from the gas analysis records can be drawn uevaluated beforehand enabling the operator to see what they should be runninto before the formation has been drilled. When the formation is drilled, the rplots made by the logger can be compared to those made previously, and evaluation conclusions can be drawn from this.

Advances are being made daily in the exploration industry and it is hoped thamethod, though not new, will aide the operator in effectively completing his w


Appendix E

Figure 1 Example Mud Gas Log Show Evaluation Report

Example 1 illustrates the relationship between a chromatographic analysis taken from two different sources. Plot 1 is the ratio taken from the mud stream on wellsite, while drilling is in operation. Plot 2 is the ratio, taken from the formation, of the gas sampled from the DST. The two plots are taken from the lower section of the Basa-Gething. The interesting point to note is that Plot 1 was obtained while drilling was in operation. Within reason, the quality of gas, oil, salt water, etc., can be determined before an expensive testing operation is run. Lithological data is determined, at the same time, by the wellsite geologist; therefore, if money or time is a factor, in well completion, this method can be a viable alternative to expensive testing or logging runs, while drilling.


Appendix E

Figure 2 Section of PPM log used in conjunction with Figure 1

The PPM log is obtained through a quantitative analysis of the hydrocarbons in the drilling fluids, specifically parts per million of the lighter hydrocarbons in the fluid. The total PPM log is the summation of the following factors: a drilling rate column which plots penetration rate inversely to the gas, on a linear scale, a visual porosity column, a lithology column which shows either an interpretive or percentage lithology; five


Appendix E

columns showing C1 through C5 in ppm; a remarks column; and finally a column detailing lithological descriptions.

Figure 3 Standard Show Evaluation Report Form”


Appendix E

Figure 4 Hydrocarbon ratio plots obtained from wellhead sample analysis data


Appendix E

Figure 5 Hydrocarbon ratio plots, productive reservoirs, obtained from wellhead analysis data, Karr Lake area.


Appendix E

Figure 6 Hydrocarbon ratio plots, non-productive reservoirs, Alberta, B.C. - analysis from gas shows on PPM logs.


Appendix E

Figure 7 PPM log and hydrocarbon ratio plots, Western Canada well.


Appendix F

ation

Appendix F “Factors Affecting the Surface Expression of Hydrocarbon Shows”(T. George Paper)

Introduction

The surface expression of hydrocarbon shows as detected by surface data logging techniques is greatly influenced by both surface and downhole factors. These factors are readily understandable on their own, but are rarely applied to surface data logging shows. This lack of application of common occurrences often leads to a misinterpretation of surface data logging show evaluation at best, and at worst to a total disregard for valid show evaluation data. This paper explains how these common surface and subsurface factors influence surface data logging shows and why there are often discrepancies in show evaluation data collected by other means, wireline, cores, sidewall cores, drill stem test, and retrievable formation test devices. Topics include:

1. How hydrocarbons enter the wellbore

2. Formation flushing3. The source of detectable hydrocarbons4. Factors affecting hydrocarbon measurements5. Background gas

In the petroleum industry there seems to exist wide differences of opinion and varying degrees of understanding about how to interpret surface data logging hydrocarbon shows. This conclusion has been reached after conducting numerous employee surface data logging programs and customer seminars on the subject during the past six years. This paper deals with the surface expression of hydrocarbon shows as detected by surface data logging equipment. It contains some explanation as to the reasons for some of the “mud log show” interpretproblems encountered by geologists and mud loggers.

Basic Definitions

equivalent circulating density (ECD) - the density (ppg) equivalent of pressureexerted by a column of fluid in motion.

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company F-1January 2001

Appendix F

filter cake - the discontinuous solids phase of a drilling mud that is deposited on the wall of a wellbore as a result of filtrate entering permeable formations. The cake consists of primarily of gel, barite, and fine drill solids; also called wall cake.

filtrate - the continuous, liquid phase of a drilling mud; can be oil (diesel, crude, mineral, etc.) or water (salt or fresh).

flushing - the process where the filtrate or liquid phase of the drilling mud enters permeable formations and displaces formation pore fluids back into the formation.

gas unit - an arbitrary ratio of gaseous hydrocarbons to air as measured by a hot-wire or other style surface gas detector.

hydrostatic head - the pressure exerted by a column of fluid at rest.

overbalanced - when the effective pressure of the drilling mud column exceeds the pore pressure of the formation.

permeability - the ability of a porous medium to allow fluids to pass through it.

pore - the void space in a rock, filled with either gas, oil or water (salt or fresh).

pore pressure - pressure of the fluid (gas, oil, or water) in a pore.

show - with regard to surface data logging, an exhibition of either gaseous or liquid hydrocarbons at the surface in either the cuttings or drilling mud.

underbalanced - when the effective pressure of the drilling mud column is less than the pore pressure of the formation.

How Hydrocarbons Enter the Wellbore

To begin an understanding of surface hydrocarbon expressions, one first needs to understand the downhole circumstances under which hydrocarbons enter the drilling mud. There are two (2) primary and secondary method by which this occurs.

Primary

Generally, a well is drilled in an overbalanced condition, usually in the range of .3 to .5 ppg. This is done primarily to prevent the uncontrolled influx of formation pore fluids into the mud column and secondarily to prevent the walls of the wellbore from caving in. As the drill bit penetrates the formation, rock chips or

F-2 © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Appendix F

cuttings are dislodged from the bottom of the hole. As cuttings are generated by the bit, some formation pore fluids enter the drilling mud from exposed pores.

While in this overbalanced condition, the only other method by which pore fluids can enter the mud column is when the cuttings reach a point in their travel up the annulus where the hydrostatic pressure exerted on them by the mud column is less than the pore pressure of the fluid inside them. When the cuttings reach this point, any gaseous fluids still inside them will begin to expand and enter the surrounding drilling mud. Liquids in the form of oil or water have a very low coefficient of expansion and essentially remain inside the cuttings unless they are pushed out by expanding gas. (Gas readings may also be generated from formation fragments that slough off the wall of the hole, but they are discounted in this discussion.)

Secondary

Oftentimes, small amounts of hydrocarbons or formation water may enter the well directly from the formation during a connection or a trip. This only occurs, however, when the effective hydrostatic pressure of the mud is temporarily reduced (swab pressure is created and ECD is removed) such that a momentary underbalanced condition is artificially created.

Formation Flushing

Also of importance in understanding surface data logging shows is the process of flushing or filtration. This process is controlled by a number of parameters.

1. The amount of pressure overbalance

2. The type of mud filtrate (oil or water).3. Whether the mud has been chemically treated to control the water loss.4. The wall cake building capabilities of the mud (polymer or gel).5. The type of pore fluids (gas, oil, or water).

Formation Permeability

Of primary consideration with regard to flushing is the formation permeability.


Appendix F

mud

Impermeable Formations

An impermeable formation will not allow filtrate to penetrate and thereby displace formation pore fluids. When this occurs, generally there is no filter cake on the wall of the hole or only a very thin one. This results from the fact that no filtrate moved into the rock to leave the solids behind as filter cake.

Permeable Formations

If the formation is permeable, mud filtrate will enter it and displace pore fluids away from the wellbore and further back into the formation. This process continues until an impermeable filter cake is deposited. (It is significant to note the wall cake can be 10,000 to 50,000 times as impermeable as the formation on which it is deposited.) This may take only a few minutes or a few hours, or the flushing process may remain essentially dynamic since the wall cake may never become completely impermeable.

In brief, when drilling an impermeable formation, the rock itself controls flushing, and when drilling a permeable formation the filter cake becomes the controlling factor. Therefore, when penetrating a permeable formation, wall cake is deposited on the side and bottom of the hole. However, because the drill bit is continually rotating and cutting on the bottom of the hole, the filter cake there is constantly being removed. This causes the rate of filtration and flushing action directly below the bit to remain at an elevated level. (See Figure 1.) On the side of the hole, where the wall cake is relatively free from erosion, the flushing action is controlled by the wall cake itself.

The area directly below the bit is where the greatest amount of flushing occurs. This is significant in that it also happens to be the area from which most of the hydrocarbon readings associated with surface data logging come. This is in contrast to the fact that all of the hydrocarbon information from wireline logs, formation tests, sidewall cores or drill stem test, is derived from the area of formation to the side of the hole behind the “protective” layer of filter cake. Hence, it is one of the reasons there is not always good correlation between log shows and non-mud log type shows.


Appendix F

ved

Figure 1 Elevated Levels of Filtration and Flushing Below the Bit

The Source of Detectable Hydrocarbons

At this point it would be helpful to recall where the hydrocarbons come from that are detected on the surface, namely pores that are opened in the process of drilling and from inside cuttings as they travel up the annulus. With all this in mind, it is obvious that the only hydrocarbons generally ever measured or noted by surface data logging techniques must have come from rock pores that were not flushed while drilling was proceeding. Again, this is taking for granted the fact that the well is being drilled in an overbalanced condition. To carry this thought to its logical conclusion, while drilling a zone supposedly containing hydrocarbons in the normally overbalanced condition, as permeability increases the likelihood of a surface manifestation of those hydrocarbons as detected by surface data logging equipment proportionately decreases. This would explain why known hydrocarbon bearing zones or zones of extremely good quality based on wireline information are sometimes “missed” or at least barely significant when obserfrom a mud logger’s perspective.


Appendix F

gas

y low

s,

d do

lly

ill it in

since to ity of slow e to

kness st a

Conversely, if a formation does contain hydrocarbons and is characterized by reduced permeability, the likelihood of a surface expression of hydrocarbons is increased since flushing was kept to a minimum. Consequently, a very poor wireline hydrocarbon show, as categorized by a tight section, may exhibit excellent oil and gas show characteristics as detected by the mud logger on the surface.

Additionally, the technique of cuttings gas analysis, where a measured quantity of cuttings and water is placed in a blender, agitated and the released hydrocarbons measured by means of a hot wire or equivalent, could also lead one into the trap of thinking that “high means good and low means bad.” In reality, a high cuttingsreading could indicate the existence of a very tight hydrocarbon-bearing formation. On the other hand, a low reading could imply that an extremely permeable, hydrocarbon-rich zone had been flushed or that the zone was trulin hydrocarbon content.

Factor Affecting Hydrocarbon Measurement

With reference to the mud loggers standard hydrocarbon detection techniquenamely the U.V. (Ultra-violet) light box, gas detector and chromatograph, it should also be noted that there are several mechanical factors which can andrastically influence hydrocarbon shows.

When Using the U.V. Box

When using the U.V. box to detect the presence of liquid hydrocarbons, usuathe amount of oil floating on the surface of a water-covered mud or cuttings sample is regarded as being indicative of the formation. (Remember that oil wbe present in the mud, just as gas is, especially if it had gas associated with the formation. Consequently, the mud should also be studied under U.V. to complete a thorough hydrocarbon search.) This may indeed be the fact, but the ratio of the volume of cuttings to the volume of mud they were circulated the surface in determines the concentration of oil and consequently the quantoil observed in a single sample, an already flushed zone drilled at a relatively or purposefully controlled rate of penetration could easily go by undetected du“dilution” of the show. This is especially true if the rate of mud circulation wasrelatively high during the time the zone was being drilled.

Therefore, care should be taken to adequately let your eyes adjust to the darof the U.V. box (30 to 60 seconds) be agitating any water-covered sample. Ju


Appendix F

by a

ing, lar

sed ing e.

nd ver,

s is he

g

few parts per million of oil can be detected using U.V. but not if the sun is bright, your eyes are not adequately adjusted to the darkness of the box, the oil is low gravity (minimal U.V. reflectance) and you’re in a hurry.

When Using the Gas Detector and Chromatograph

Similarly, gas detector and chromatograph readings are expectedly reduced low cuttings-to-mud ratio. Also of note is the fact that, based on the cuttings-to-mud ratio being the factor controlling the magnitude of a gas reada 2 or 3 fold increase in the rate-of-penetration could logically result in a simi2 or 3 fold increase in the surface gas readings. In the field, this situation commonly occurs in the form of a drilling break. A similar gas versus ROP increase would occur merely if the driller applied more weight-on-bit or increathe rotary RPM. Also, if the formation pore pressure increased while maintaina constant mud weight this would produce a drilling situation closer to balancAs a result, the ROP would again increase, which would also produce a correspondingly higher gas reading. Obviously, these situations require that formation variables such as the ratio of hydrocarbon volume to rock volume aformation permeability, remain constant, which is usually not the case. Howethis relationship should be recognized.

Background Gas

A final area of importance is that of background gas. Usually, background gadefined as the normal flowline gas reading under average ROP conditions. Tproblem is how the background gas is used in regards to describing a show. Oftentimes, the logger is directed to subtract the average background gas readinfrom the gas reading measured during a show. Once again recalling the circumstances under which hydrocarbons enter the drilling mud, it is quickly recognizable why this is a faulty practice. To further the point, consider the following example.


Appendix F

ro e

s was on.

ons

begin

0

one mean he

dition

Example

Assume the bit is penetrating a shale section and the surface background gas reading is 30 gas units. Drilling proceeds until the bit is just at the boundary of a show zone; the driller picks the bit up off bottom but continues to circulate the shale cuttings to the surface. Upon “bottoms-up,” the gas reading goes to zesince no more pores are being opened on the bottom of the hole and no morcuttings are releasing their pore fluids to the drilling mud. Usually, the only circumstances where the gas reading would not go to zero would be if the gabeing recirculated or if the well was being drilled in an underbalanced conditiObviously, drilling a permeable hydrocarbon-bearing formation in an underbalanced condition would allow the formation in situ to bleed hydrocarbinto the well regardless of the lack of drilling and cuttings. (This in fact is an excellent method to determine the balance condition.)

Once the surface gas reading has dropped to zero, the driller is instructed to making hole again and the bit immediately penetrates the show zone. Upon “bottoms-up” this time the gas reading shows 200 units. In no way does the 3units of background gas from the shale have anything to do with the 200 unitreading in the show zone and should therefore not be subtracted.

Gas in the Suction Pit

If any gas reading is to be subtracted from any other gas reading it would betaken from a gas trap located in the suction pit. Any gas detected here would there is gas being pumped back down the wellbore where it would mix with tdrilled cuttings gas reading and it should indeed be subtracted from any consequent flowline readings. Most often, the suction pit gas reading is insignificant but should be monitored under at least the following conditions:

1. Degassing equipment is absent or inadequate.

2. If an oil-base (crude or diesel) mud is being used.3. If a hydrocarbon bearing zone has recently been penetrated.

Gas in the suction pit could also cause a misinterpretation of the balance conif it were determined using the gas versus cuttings method described above.


Appendix F

Conclusion

In conclusion, there are many factors to consider when interpreting shows, many of which have not been discussed in this article. However, experience shows the following factors to be of paramount importance:

1. How hydrocarbons enter the wellbore.

2. Formation flushing.3. The source of detectable hydrocarbons.4. Factors affecting hydrocarbon measurement.5. Background gas.

Hopefully, this information will provide answers to some of the questions and bothersome problems encountered when reading and interpreting mud log shows.


Appendix F


Appendix G

ed

in the

Appendix G Glossary

A

abandon v: to cease producing oil and gas from a well when it becomes unprofitable. A wildcat well may be abandoned after it has proven nonproductive. Several steps are involved in abandoning a well: part of the casing is removed and salvaged; one or more cement plugs are placed in the borehole to prevent migration of fluids between the different formations penetrated by the borehole; and the well is abandoned. In many states, it is necessary to secure permission from official agencies before a well may be abandoned.

absolute permeability n: a measure of the ability of a single fluid (as water, gas, or oil) to flow through a rock formation when the formation is totally filled (saturated) with the single fluid. The permeability measure of a rock filled with a single fluid is different from the permeability measure of the same rock filled with two or more fluids. Compare effective permeability.

acid fracture v: to part or open fractures in productive, hard-limestone formations by using a combination of oil and acid or water and acid under high pressure. See formation fracturing.

acidize v: to treat oil-bearing limestone or other formations, using a chemical reaction with acid, to increase production. Hydrochloric or other acid is injected into the formation under pressure. The acid etches the rock, enlarging the pore spaces and passages through which the reservoir fluids flow. The acid is held under pressure for a period of time and then pumped out, and the well is swabbed and put back into production. Chemical inhibitors combined with the acid prevent corrosion of the pipe.

adjustable choke n: a choke in which a conical needle and seat vary the rate of flow. See choke.

air-actuated adj: powered by compressed air, as the clutch and brake system in drilling equipment.

air drilling n: a method of rotary drilling that uses compressed air as the circulation medium. The conventional method of removing cuttings from the wellbore is to use a flow of water or drilling mud. Compressed air removes the cuttings with equal or greater efficiency. The rate of penetration is usually increased considerably when air drilling is used. However, a principal problem in air drilling is the penetration of formations containing water, since the entry of water into the system reduces the ability of the air to remove the cuttings.

American Petroleum n: 1. founded in 1920, this national oil trade organization is the leadingInstitute standardizing organization on oil field drilling and producing equipment. It

maintains departments of transportation, refining, and marketing in Washington, D.C., and a department of production in Dallas. 2. (slang) indicative of a job being properly or thoroughly done (as, “His work is strictly API”). 3. degrees API, usto designate API gravity. See API gravity.

angle of deflection n: in directional drilling, the angle, expressed in degrees, at which a well is deflected from the vertical by a whipstock or other deflecting tool. See whipstock.

annular blowout n: a large valve, usually installed above the ram preventers, that forms a seal preventer annular space between the pipe and wellbore or, if no pipe is present, on the

wellbore itself. Compare ram blowout preventer.

SDL Applied Fundamentals © 2001 Sperry-Sun, a Halliburton Company G-1January 2001

Appendix G

annular space n: 1. the space surrounding a cylindrical object within a cylinder. 2. the space around a pipe in a wellbore, the outer wall of which may be the wall of either the borehole or the casing; sometimes termed the annulus.

anticline n: an arched, inverted-trough configuration of folded and stratified rock layers. Compare syncline.

API abbr: American Petroleum Institute.

API gravity n: the measure of the density or gravity of liquid petroleum products in the United States, derived from specific gravity in accordance with the following equation:

API gravity = 141.5 - 131.5specific gravity

API gravity is expressed in degrees, a specific gravity of 1.0 being equivalent to 10o API.

B

back off v: to unscrew one threaded piece (as a section of pipe) from another.

back up v: to hold one section of an object (as pipe) while another is being screwed into or out of it.

bail n: a cylindrical steel bar (similar to the handle or bail of a bucket, only much larger) that supports the swivel and connects it to the hook. Sometimes, the two cylindrical bars that support the elevators and attach them to the hook are called bails. v: to recover bottomhole fluids, samples, or drill cuttings by lowering a cylindrical vessel called a bailer to the bottom of a well, filling it and retrieving it. See bailer.

bailer n: a long cylindrical container, fitted with a valve at its lower end, used to remove water, sand, mud or oil from a well.

bailing line n: cable attached to the bailer, passed over a sheave at the top of the derrick, and spooled on a reel. See sheave.

barge n: any one of many types of flat-decked, shallow draft vessels, usually towed by a boat. A complete drilling rig may be assembled on a drilling barge, which usually is submersible; that is, it has a submersible hull or base that is flooded with water at the drilling site. Drilling equipment, crew quarters, and so forth are mounted on a superstructure above the water level.

barite or baryte n: barium sulfate BaSO4; a mineral used to increase the weight of drilling mud. Its specific gravity is 4.2 (i.e., it is 4.2 times heavier than water). See barium sulfate and mud.

barium sulfate n: 1. a chemical combination of barium, sulfur, and oxygen. Also called barite. See barite. 2. a tenacious scale that is very difficult to remove.

barrel n: a measure of volume for petroleum products. One barrel is the equivalent of 42 U.S. gallons or 0.15899 cubic meters. One cubic meter equals 6.2897 barrels.

basket sub n: a fishing accessory run above a bit or mill to recover small pieces of metal or junk in a well.

bed n: a specific layer of earth or rock in contrast to other layers of different material lying above, below, or adjacent to it.

G-2 © 2001 Sperry-Sun, a Halliburton Company SDL Applied FundamentalsJanuary 2001

Appendix G

ackup ore

der

ment

belt n: a flexible band or cord connecting and passing about each of two or more pulleys to transmit power or impart motion.

bit n: the cutting or boring element used in drilling oil and gas wells. The bit consists of the cutting element and the circulating element. The circulating element permits the passage of drilling fluid and utilizes the hydraulic force of the fluid stream to improve drilling rates. In rotary drilling, several drill collars are joined at the bottom end of the drill string. The bit is attached to the end of the drill collar. Most bits used in rotary drilling are roller cone bits.

bit breaker n: a heavy plate that fits in the rotary table and hold the drill bit while it is being made up in or broken out of the drill string. See bit.

bit record n: a report on each bit used in a drilling operation that lists the bit type, the amount of footage the bit has drilled, and the nature of the formation penetrated.

blind ram n: an integral part of a blowout preventer that serves as the closing element. Its ends do not fit around the drill pipe but seal against each other and shut off the space below completely.

block n: any assembly of pulleys on a common framework; in mechanics one or more pulleys, or sheaves, mounted to rotate on a common axis. The crown block is an assembly of sheaves mounted on beams at the top of the derrick. The drill line is reeved over the sheaves of the crown block alternately with the sheaves of the traveling block, which is hoisted and lowered in the derrick by the drill line. When the elevators are attached to a hook on the traveling block, and when drill pipe is latched in the elevators, the pipe can be raised or lowered in the derrick. See crown block, elevator, hook, reeve, sheave, and traveling block; also see drilling block.

blooey line n: the discharge pipe from a well being drilled by air drilling. The blooey line is used to conduct the air or gas used for circulation away from the rig to reduce the fire hazard as well as to transport the cuttings a suitable distance from the well. See air drilling.

blowout n: an uncontrolled flow of gas, oil, or other well fluids into the atmosphere. A blowout, or gusher, occurs when formation pressure exceeds the pressure applied to it by the column of drilling fluid. A kick warns of an impending blowout. See formation pressure, gusher, and kick.

blowout preventer n: one of several valves installed at the wellhead to prevent the escape of pressure either in the annular space between the casing and drill pipe or in open hole (i.e., hole with no drill pipe) during drilling or completion operations. Blowout preventers on land rigs are located beneath the rig at the land’s surface; on jor platform rigs, they are located at the water’s surface; and on floating offshrig, on the seafloor. See annular blowout preventer, inside blowout preventer, and ram blowout preventer.

boll-weevil n: (slang) an inexperienced rig or oil-field worker, sometimes shortened to “weevil.”

bomb n: a thick-walled container, usually steel, used to hold sample of oil or gas unpressure. See bottom-hole pressure.

bond n: the state of one material adhering or being joined to another material (as ceto formation). v: to adhere or be joined to another material.

BOP abbr: blowout preventer.


Appendix G

ction,

nter.

bit ed up

a

wall

borehole n: the wellbore; the hole made by drilling or boring. See wellbore.

bottomhole n: the lowest or deepest part of a well. adj: pertaining to the bottom of the wellbore.

bottomhole choke n: a device with a restricted opening placed in the lower end of the tubing to control the rate of flow. See choke.

bottomhole pressure n: 1. the pressure at the bottom of a borehole. It is caused by the hydrostatic pressure of the drilling fluid in the hole and, sometimes, any back-pressure held at the surface as when the well is shut in with blowout preventers. When mud is being circulated, bottomhole pressure is the hydrostatic pressure plus the remaining circulating pressure required to move the mud up the annulus. 2. the pressure in a well at a point opposite the producing formation, as recorded by a bottomhole pressure bomb.

box n: the female section of a tool joint. See tool joint.

brake n: a device for arresting the motion of a mechanism, usually by means of friction, as in the draw works brake. Compare electrodynamic brake and hydromatic brake.

break out v: 1. to unscrew one section of pipe from another section, especially drill pipe while it is being withdrawn from the wellbore. During this operation, the tongs are used to start the unscrewing operation. See tongs. 2. to separate, as gas from liquid.

breakout cat-head n: a device attached to the shaft of the draw works that is used as a power source for unscrewing drill pipe; usually located opposite the driller’s side of the drawworks. See cat-head.

breakout tongs n: tongs that are used to start unscrewing one section of pipe from another seespecially drill pipe coming out of the hole. Also called lead tongs. See tongs.

bring in a well v: to complete a well and put it in producing status.

buck up v: to tighten up a threaded connection (as two joints of drill pipe).

bullet perforator n: a tubular device that, when lowered to a selected depth within a well, firesbullets through the casing to provide hole through which the well fluids may e

C

cable n: a rope of wire, hemp, or other strong fibers. See wire-rope.

cable-tool drilling n: a drilling method in which the hole is drilled by dropping a sharply pointed on the bottom of the hole. The bit is attached to a cable, and the cable is pickand dropped, picked up and dropped, over and over, as the hole is drilled.

cap rock n: 1. impermeable rock overlying an oil or gas reservoir that tends to preventmigration of oil or gas out of the reservoir. 2. the porous and permeable stratoverlying salt domes that may serve as the reservoir rock.

cased adj: pertaining to a wellbore in which casing is run and cemented. See casing.

cased hole n: a wellbore in which casing has been run.

casing n: steel pipe placed in an oil or gas well as drilling progresses to prevent the of the hole from caving in during drilling and to provide means of extracting petroleum if the well is productive.


Appendix G

casing centralizer n: a device secured around the casing at regular intervals to center it in the hole. Casing that is centralized allows a more uniform cement sheath to form around the pipe.

casing coupling n: a tubular section of pipe that is threaded inside and used to connect two joints of casing.

casing elevator n: See elevator.

casing head n: a heavy steel, flanged fitting that connects to the first string of casing and provides a housing for the slips and packing assemblies by which intermediate strings of casing are suspended and the annulus sealed off. Also called a spool. See annular space.

casing shoe n: also called a guide shoe. See guide shoe.

casing string n: the entire length of all the joints of casing run in a well. Casing is manufactured in lengths of about 30 feet, each length or joint being joined to another as casing is run in a well. See combination string.

catch samples v: to obtain cuttings for geological information as formation are penetrated by the bit. The samples are obtained from drilling fluid as it emerges from the wellbore or, in cable-tool drilling, from the bailer. Cuttings are carefully washed until they are free of foreign matter, dried, and labeled to indicate the depth at which they were obtained. See bailer, cable-tool drilling, and cuttings.

cat-head n: a spool-shaped attachment on a winch around which rope for hoisting and pulling is wound. See breakout cat-head and makeup cat-head.

cat-line n: a hoisting or pulling line powered by the cat-head and used to lift heavy equipment on the rig. See cat-head.

caving n: collapse of the walls of the wellbore, also called sloughing.

cellar n: a pit in the ground to provide additional height between the rig floor and the wellhead to accommodate the installation of blowout preventers, rat hole, mouse hole, and so forth. It also collects drainage water and other fluids for subsequent disposal.

cement casing v: to fill the annulus between the casing and hole with cement to support the casing and prevent fluid migration between permeable zones.

cement channeling n: an undesirable phenomenon that can occur when casing is being cemented in a borehole. The cement slurry fails to rise uniformly between the casing and borehole wall, leaving spaces void of cement. Ideally, the cement should completely and uniformly surround the casing and form a strong bond to the borehole wall.

cementing n: the application of a liquid slurry of cement and water to various points inside and outside the casing. See primary cementing, secondary cementing, and squeeze cementing.

chain drive n: a drive system using a chain and chain gears to transmit power. Power transmissions use a roller chain, in which each link is made of side bars, transverse pins, and rollers on the pins. A double roller chain is made of two connected rows of links, a triple roller chain of three, and so forth.

chain tongs n: a tool consisting of a handle and releasable chain used for turning pipe or fittings of a diameter larger than that which a pipe wrench would fit. The chain is looped and tightened around the pipe or fitting, and the handle is used to turn the


Appendix G

any’s

orks,

of

open

tool so that the pipe of fitting can be tightened or loosened.

check valve n: a valve that permits flow in one direction only.

choke n: an orifice installed in a line to restrict the flow and control the rate of production. Surface chokes are part of the Christmas tree and contain a choke nipple, or bean, with a small-diameter bore that serves to restrict the flow. Chokes are also used to control the rate of flow of the drilling mud out of the hole when the well is closed in with the blowout preventer and a kick is being circulated out of the hole See adjustable choke, blowout preventer, bottomhole choke, Christmas tree, kick, nipple, and positive choke.

choke line n: an extension of pipe from the blowout preventer assembly used to direct well fluids from the annulus to the choke manifold.

choke manifold n: the arrangement of piping and special valves, called chokes, through which drilling mud is circulated when the blowout preventers are closed to control the pressures encountered during a kick. See choke and blowout preventer.

Christmas tree n: the control valves, pressure gauges, and chokes assembled at the top of a well to control the flow of oil and gas after the well has been drilled and completed.

circulate v: to pass from one point throughout a system and back to the starting point. For example, drilling fluid is circulated out of the suction pit, down the drill pipe and drill collars, out the bit, up the annulus, and back to the pits.

circulation n: the movement of drilling fluid out of the mud pits, down the drill string, up the annulus, and back to the mud pits.

combination string n: a casing string that has joints of various collapse resistance, internal yield strength, and tensile strength designed for various depths in a specific well to best withstand the conditions of that well. In deep wells, high tensile strength is required in the top casing joints to carry the load, whereas high collapse resistance and internal yield strength are needed for the bottom joints. In the middle of the casing, average qualities are usually sufficient. The most suitable combination of types and weights of pipe helps to ensure efficient production at a minimum cost.

come out of the hole v: to pull the drill string out of the wellbore. This withdrawal is necessary to change the bit, change from a core barrel to the bit, run electric logs, prepare for a drill stem test, run casing, and so on.

company man n: also called company representative, See company representative.

company representative n: an employee of an operating company whose job is to represent the compinterest at the drilling location.

complete a well v: to finish work on a well and bring it to productive status. See well completion.

compound n: a mechanism used to transmit power from the engines to the pump, draw wand other machinery on a drilling rig. It is composed of clutches, chains and sprockets, belts and pulleys, and a number of shafts, both driven and driving.v: to connect two or more power-producing devices (as engines) to run one piecedriven equipment (as the draw works).

conductor pipe n: a short string of large-diameter casing used to keep the top of the wellbore and to provide a means of conveying the up-flowing drilling fluid from the wellbore to the mud pit.

contract depth n: the depth of the wellbore at which the drilling contract is fulfilled.


Appendix G

t

it

r

a

me. ),

used

core n: a cylindrical sample taken from a formation for geological analysis. Usually a conventional core barrel is substituted for the bit and procures a sample as it penetrates the formation. See also sidewall coring. v: to obtain a formation sample for analysis.

core analysis n: laboratory analysis of a core sample to determine porosity, permeability, lithology, fluid content, angle of dip, geological age, and probable productivity of the formation.

core barrel n: a tubular device from 25 to 60 feet long run at the bottom of the drill pipe in place of a bit to cut a core sample.

core catcher n: the part of the core barrel that holds the formation sample.

core cutterhead n: the cutting element of the core barrel assembly. In design it corresponds to one of the three main types of bits: drag bits with blades for cutting soft formations; roller bits with rotating cutting for cutting medium formations; and diamond bits for cutting very hard formations.

coupling n: 1. in piping, a metal collar with internal threads used to join two sections of thread pipe. 2. in power transmission, a connection extending longitudinally between a driving shaft and a driven shaft. Most such couplings are flexible and compensate for minor misalignment of the two shafts.

crooked hole n: a wellbore that has deviated from the vertical. It usually occurs in areas where the subsurface formations are difficult to drill, such as a section of alternating hard and soft strata steeply inclined from the horizontal.

crown block n: an assembly of sheaves or pulleys mounted on beams at the top of the derrick over which the drill line is reeved. See block, reeve, and sheave.

cuttings n pl: the fragments of rock dislodged by the bit and brought to the surface in the drilling mud. Washed and dried samples of the cuttings are analyzed by geologists to obtain information about the formations drilled.

D

daylight tour n: (pronounced “tower”) the shift of duty on a drilling rig that starts at or aboudaylight; also called morning tour. Compare evening tour and graveyard tour.

deadline n: the drill line from the crown block sheave to the anchor, so called becausedoes not move. Compare fastline.

deadline tie-down n: a device to which the deadline is attached, securely fastened to the mast oanchor derrick substructure. Also called a deadline anchor.

degasser n: the equipment used to remove unwanted gas from a liquid, especially fromdrilling fluid.

density n: the mass or weight of a substance; often expressed in weight per unit voluFor instance, the density of a drilling mud may be 10 pounds per gallon (ppg74.8 pounds per cubic foot (lb/ft3), or 1,198.2 kilograms per cubic meter (kg/m3). Specific gravity and API gravity are other units of density. See API gravity and specific gravity.

derrick n: a large load-bearing structure, usually of bolted construction. In drilling, thestandard derrick has four legs standing at the corners of the substructure andreaching to the crown block. The substructure is an assembly of heavy beamsto elevate the derrick and provide space to install blowout preventers, casing


Appendix G

heads, and so forth. Because the standard derrick must be assembled piece by piece, it has largely been replaced by the mast, which can be lowered and raised without disassembly. See crown block, mast, and substructure.

derrickman n: the crew member who handles the upper end of the drill string as it is being hoisted out of or lowered into the hole. He is also responsible for the conditioning of the drilling fluid and circulating machinery.

de-sander n: a centrifugal device for removing sand from drilling fluid to prevent abrasion of the pumps. It may be operated mechanically or by a fast-moving stream of fluid inside a special cone-shaped vessel, in which case it is sometimes called a hydrocyclone. See de-silter.

de-silter n: a centrifugal device for removing very fine particles, or silt, from drilling fluid to keep the amount of solids in the fluid to the lowest possible point. Usually, the lower the solids content of mud, the faster the rate of penetration. It works on the same principle as a de-sander. Compare de-sander.

development well n: 1. a well drilled in proven territory in a field to complete a pattern of production. 2. an exploitation well. See exploitation well.

deviation n: the inclination of the wellbore from the vertical. The angle of deviation, angle of drift, or drift angle is the angle in degrees that shows the variation from the vertical as revealed by a deviation survey. See deviation survey.

deviation survey n: an operation made to determine the angle from which a bit has deviated from the vertical during drilling. There are two basic deviation survey, or drift survey, instruments: one reveals the angle of deviation only; the other indicates both the angle and direction of deviation.

diamond bit n: a drilling bit that has a steel body surfaced with industrial diamonds. Cutting is performed by the rotation of the very hard diamonds over the rock surface.

diesel-electric power n: the power supplied to a drilling rig by diesel engines driving electric generators, used widely offshore and gaining popularity onshore.

diesel engine n: a high-compression, internal-combustion engine used extensively for powering drilling rigs. In a diesel engine, air is drawn into the cylinders and compressed to very high pressures; ignition occurs as fuel is injected into the compressed and heated air. Combustion takes place within the cylinder above the piston, and expansion of the combustion products imparts power to the piston.

directional drilling n: intentional deviation of a wellbore from the vertical. Although wellbores are normally drilled vertically, it is sometimes necessary or advantageous to drill at an angle from the vertical. Controlled directional drilling makes it possible to reach subsurface areas laterally remote from the point where the bit enters the earth. It involves the use of turbo-drills, Dyna-Drills, whipstocks, or other deflecting tools.See Dyna-Drill, turbo-drill, and whipstock.

discovery well n: the first oil or gas well drilled in a new field; the well that reveals the presence of a petroleum-bearing reservoir. Subsequent wells are development wells. Compare development well.

displacement fluid n: in oil well cementing, the fluid, usually drilling mud or salt water, that is pumped into the well after the cement to force the cement out of the casing and into the annulus.

doghouse n: 1. a small enclosure on the rig floor used as an office for the driller or as a storehouse for small objects. 2. any small building used as an office or for storage.


Appendix G

double n: a length of drill pipe, casing, or tubing consisting of two joints screwed together. Compare thribble and fourble. See joint.

double-board n: the name used for the working platform of the derrickman, or monkey board, when it is located at a height in the derrick or mast equal to two lengths of pipe joined together. Compare fourble board and thribble board. See monkey board.

draw works n: the hoisting mechanism on a drilling rig. It is essentially a large winch that spools off or takes in the drill line and thus raises or lowers the drill string and bit.

drill bit n: the cutting or boring element used for drilling. See bit.

drill collar n: a heavy, thick-walled tube, usually steel, used between the drill pipe and the bit in the drill string. Drill collars are used to put weight on the bit so that the bit can drill.

driller n: the employee directly in charge of a drilling rig and crew. His main duty is operation of the drilling and hoisting equipment, but he is also responsible for the operation of downhole tools, and pipe measurement.

drilling block n: a lease or a number of leases of adjoining tracts of land that constitute a unit of acreage sufficient to justify the expense of drilling a wildcat.

drilling contractor n: an individual or group of individuals that own a drilling rig or rigs and contract their services for drilling wells to a certain depth.

drilling crew n: a driller, derrickman, and two or more helpers who operate a drilling rig for one tour each day. See derrickman, driller, and tour.

drilling fluid n: circulating fluid, one function of which is to force cuttings out of the wellbore and to the surface. While a mixture of clay, water, and other chemical additives is the most common drilling fluid, wells can also be drilled using air, gas, or water as the drilling fluid. Also called circulating fluid. See mud.

drilling foreman n: the supervisor of drilling operations on a rig; also the tool pusher or superintendent.

drill line n: a wire rope used to support the drilling tools.

drilling rate n: the speed with which the bit drills the formation; usually called the rate of penetration.

drilling rig n: See rig.

drill pipe n: the heavy seamless tubing used to rotate the bit and circulate the drilling fluid. Joints of pipe 30 feet long are coupled together by means of tool joints.

drill ship n: a ship constructed to permit a well to be drilled from it at an offshore location. While not as stable as other floating structures (as a semisubmersible), drill ships, or ship shapes, are capable of drilling exploratory wells in relatively deep waters. They may have a ship hull, a catamaran hull, or a trimaran hull. See semisubmersible drilling rig.

drill stem n: all members in the assembly used for drilling by the rotary method from the swivel to the bit, including the kelly, drill pipe and tools joints, drill collars, stabilizers, and various subsequent items. Compare drill string.

drill-stem test n: a method of gathering data on the potential productivity of a formation before installing casing in a well. See formation testing.


Appendix G

so e.

drill string n: the column, or string, of drill pipe with attached tool joints that transmits fluid and rotation power from the kelly to the drill collars and bit. Often, especially in the oil field, term is loosely applied to include both drill pipe and drill collars. Compare drill stem.

drum n: 1. a cylinder around which wire rope is wound in the draw works. The draw works drum is that part of the hoist upon which the drill line is wound. 2. a steel container of general cylindrical form. Refined products are shipped in steel drums with capacities of about 50 to 55 U.S. gallons (about 200 liters).

DST abbr: drill-stem test

Dyna-Drill n: a downhole motor driven by drilling fluid that imparts rotary motion to a drilling bit connected to the tool, thus eliminating the need to turn the entire drill string to make hole. The Dyna-Drill, a trade name, is used in straight and directional drilling.

dynamic positioning n: a method by which a floating offshore drilling rig is maintained in position over an offshore well location. Generally, several motors called thrusters are located on the hull(s) of the structure and are actuated by a sensing system. A computer to which the system feeds signals then directs the thrusters to maintain the rig on location.

E

effective permeability n: a measure of the ability of a single fluid to flow through a rock when the pore spaces of the rock are not completely filled or saturated with the fluid. Compare absolute permeability and relative permeability.

electric well log n: a record of certain electrical characteristics of formation traversed by the borehole, made to identify the formation, determine the nature and amount of fluids they contain, and estimate their depth. Also called an electric log or electric survey.

electrodynamic brake n: a device mounted on the end of the draw works shaft of a drilling rig. The electrodynamic brake (sometimes called a magnetic brake) serves as an auxiliary to the mechanical brake when pipe is lowered into a well. The braking effect in an electrodynamic brake is achieved by means of the interaction of electric currents with magnets, with other currents, or with themselves.

elevator n: a set of clamps that grips a stand, or column of casing, tubing, or drill pipe so that the stand can be raised or lowered into the hole.

evening tour n: (pronounced “tower”) the shift of duty on a drilling rig that starts in the afternoon and runs through the evening. Compare daylight tour and graveyard tour.

exploitation well n: a well drilled to permit more effective extraction of oil from a reservoir. It issometimes called a development well. See development well.

exploration well n: a wildcat. See wildcat.

F

fastline n: the end of the drill line that is affixed to the drum or reel of the draw works,called because it travels with greater velocity than any other portion of the linCompare deadline.


Appendix G

fault n: a break in subsurface strata. Often strata on one side of the fault line has been displaced (upward, downward, or laterally) relative to its original positions.

field n: a geographical area in which a number of oil and gas wells produce from a continuous reservoir. A field may refer to surface area only or to underground productive formations as well. In a single field, there may be several separate reservoirs at varying depths.

fill the hole v: to pump drilling fluid into the wellbore while the pipe is being withdrawn in order to ensure that the wellbore remains full of fluid even though the pipe is withdrawn. Filling the hole lessens the danger of blowout or of caving of the wall of the wellbore.

filter cake n: 1. compacted solid or semisolid material remaining on a filter after pressure filtration of mud with the standard filter press. Thickness of the cake is reported in thirty-seconds of an inch or in millimeters. 2. the layer of concentrated solids from the drilling mud that forms on the walls of the borehole opposite permeable formations; also called wall cake or mud cake.

fingerboard n: a rack that supports the tops of the stands of pipe being stacked in the derrick or mast. It has several steel finger-like projections that form a series of slots into which the derrickman can set a stand of drill pipe as it is pulled out of the hole.

fish n: an object left in the wellbore during drilling operations that must be recovered or drilled around before work can proceed. It can be anything from a piece of scrap metal to a part of the drill string. v: 1. to recover from a well any equipment left there during drilling operations, such as a lost bit or drill collar or part of the drill string. 2. to remove from an older well certain pieces of equipment, such as packers, liners, or screen pipe, to allow reconditioning of the well.

fishing tool n: a tool designed to recover equipment lost in the well.

float collar n: a special coupling device, inserted one or two joints above the bottom of the casing string, that contains a check valve to permit fluid to pass downward but not upward through the casing. The float collar prevents drilling mud from entering the casing while it is being lowered, allowing the casing to float during its descent, which decreases the load on the derrick. The float collar also prevents a back flow of cement during the cementing operation.

floorman n: a drilling crew member whose work station is on the derrick floor. On rotary drilling rigs, there are at least two and usually three or more floormen on each crew. Also called rotary helper and roughneck.

fluid n: a substance that flows and yields to any force tending to change it shape. Liquids and gases are fluids.

formation n: a bed or deposit composed throughout of substantially the same kinds of rock; a lithologic unit. Each different formation is given a name, frequently as a result of the study of the formation outcrop at the surface and sometimes based on fossils found in the formation.

formation fracturing n: a method of stimulating production by increasing the permeability of the producing formation. Under extremely high hydraulic pressure, a fluid (as water, oil, alcohol, dilute hydrochloric acid, liquefied petroleum gas, or foam) is pumped downward through tubing or drill pipe and forced into the perforations in the casing. The fluid enters the formation and parts or fractures it. Sand grains, aluminum pellets, glass beads, or similar materials are carried in suspension by the fluid into the fractures. These are called propping agents or proppants. When


Appendix G

arth’s

,

t

ght of

at sing

the pressure is released at the surface, the fracturing fluid returns to the well, and the fractures partially close on the proppants, leaving channels for oil to flow through them to the well. This process is often called a frac job. See propping agent.

formation pressure n: the force exerted by fluids in a formation, recorded in the hole at the level of the formation with the well shut in. It is also called reservoir pressure or shut-in bottom-hole pressure. See reservoir pressure and shut-in bottom-hole pressure.

formation testing n: the gathering of data on a formation to determine its potential productivity before installing casing in a well. The conventional method is the drill stem test. Incorporated in the drill stem testing tool are a packer, valves or ports that may be opened and closed from the surface, and a pressure-recording device. The tool is lowered to bottom on a string of drill pipe and the packer set, isolating the formation to be tested from the formations above and supporting the fluid column above the packer. A port on the tool is opened to allow the trapped pressure below the packer to bleed off into the drill pipe, gradually exposing the formation to atmospheric pressure and allowing the well to produce to the surface, where the well fluids may be sampled and inspected. From a record of the pressure readings, a number of facts about the formation may be inferred.

fourable n: a section of drill pipe, casing or tubing consisting of four joints screwed together. Compare double and thribble. See joint.

fourable board n: the name used for the working platform of the derrickman, or monkey board, when it is located at a height in the derrick equal to approximately four lengths of pipe joined together. Compare double board and thribble board. See monkey board.

fracturing n: shortened form of formation fracturing. See formation fracturing.

G

gas-cut mud n: a drilling mud that has entrained formation gas giving the mud a characteristically fluffy texture. When entrained gas is not released before the fluid returns to the well, the weight or density of the fluid column is reduced. Because a large amount of gas in mud lowers its density, gas-cut mud must be treated to lessen the chance of a blowout.

gas sand n: a stratum of sand or porous sandstone from which natural gas is obtained.

gas show n: the gas that appears in drilling fluid returns, indicating the presence of a gas zone.

geologist n: a scientist who gathers and interprets data pertaining to the strata of the ecrust.

geology n: the science that relates to the study of the structure, origin, history, and development of the earth and its inhabitants as revealed in the study of rocksformations, and fossils.

graveyard tour n: (pronounced “tower”) the shift of duty on a drilling rig that starts at or aboumidnight. Compare daylight tour and evening tour.

gravity n: the attraction exerted by the earth’s mass on objects at its surface; the weia body. See API gravity and specific gravity.

guide shoe n: a short, heavy, cylindrical section of steel filled with concrete and rounded the bottom, which is placed at the end of the casing string. It prevents the ca


Appendix G

from snagging on irregularities in the borehole as it is lowered. A passage through the center of the shoe allows drilling fluid to pass up into the casing while it is being lowered and cement to pass out during cementing operations. Also called casing shoe.

gun-perforate v: to create holes in casing and cement set through a productive formation. A common method of completing a well is to set casing through the oil-bearing formation and cement it. A perforating gun is then lowered into the hole and fired to detonate high-powered jets or shoot steel projectiles (bullets) through the casing and cement and into the pay zone. The formation fluids flow out of the reservoir through the perforations and into the wellbore. See jet-perforate and perforating gun.

gusher n: an oil well that has come in with such great pressure that the oil jets out of the well like a geyser. In reality, a gusher is a blowout and is extremely wasteful of reservoir fluids and drive energy. In the early days of the oil industry, gushers were common and many times were the only indication that a large reservoir of oil and gas had been struck. See blowout.

H

hoist n: an arrangement of pulleys and wire rope or chain used for lifting heavy objects; a winch or similar device; the draw works. See draw works.

hoisting drum n: the large, flanged spooled in the draw works on which the hoisting cable is wound. See draw works.

hook n: a large hook-shaped device from which the swivel is suspended. It is designed to carry maximum loads ranging from 100 to 650 tons and turns on bearings in its supporting housing. A strong spring within the assembly cushions the weight of a stand (90 feet) of drill pipe, thus permitting the pipe to be made up and broken out with less damage to the tool joint threads. Smaller hooks without the spring are used for handling tubing and sucker rods. See stand and swivel.

hopper n: a large funnel- or cone-shaped device into which dry components (as powdered clay or cement) can be poured in order to uniformly mix the components with water (or other liquids). The liquid is injected through a nozzle at the bottom of the hopper. The resulting mixture of dry material and liquid may be drilling mud to be used as the circulating fluid in a rotary drilling operation or may be cement slurry used to bond casing to the borehole.

hydraulic fracturing n: an operation in which a specially blended liquid is pumped down a well and into a formation under pressure high enough to cause the formation to crack open. The resulting cracks or fractures serve as passages through which oil can flow into the wellbore. See formation fracturing.

hydrocarbons n: organic compounds of hydrogen and carbon, whose densities, boiling points, and freezing points increase as their molecular weights increase. Although composed only of two elements, hydrocarbons exist in a variety of compounds, because of the strong affinity of the carbon atom for other atoms and for itself. The smallest molecules of hydrocarbons are gaseous; the largest are solids. Petroleum is a mixture of many different hydrocarbons.

hydromatic brake n: a device mounted on the end of the draw works shaft of a drilling rig. The hydromatic brake (often simply called the hydromatic) serves as an auxiliary to the mechanical brake when pipe is lowered into the well. The braking effect in a


Appendix G

hydromatic brake is achieved by means of a runner or impeller turning in a housing filled with water.

I

impermeable adj: preventing the passage of fluid. A formation may be porous yet impermeable if there is an absence of connecting passages between the voids within it. See permeability.

inland barge rig n: a drilling structure consisting of a barge upon which the drilling equipment is constructed. When moved from one location to another, the barge floats, but when stationed on the drill site, the barge is submerged to rest on the bottom. Typically, inland barge rigs are used to drill wells in marshes, shallow inland bays, and in areas where the water covering the drill site is not too deep.

instrumentation n: a device or assembly of devices designed for one or more of the following functions: to measure operating variables (as pressure, temperature, rate of flow, speed of rotation, etc.); to indicate these phenomena with visible or audible signals; to record them, to control them within a predetermined range; and to stop operations if the control fails. Simple instrumentation might consist of an indicating pressure gauge only. In a completely automatic system, the desired range of pressure, temperature, and so on is predetermined and preset.

intermediate casing string n: the string of casing set in a well after the surface casing, but before the production casing, to keep the hole from caving and to seal off troublesome formations. The string is sometimes called protection casing.

J

jackup drilling rig n: an offshore drilling structure with tubular or derrick legs that support the deck and hull. When positioned over the drilling site, the bottoms of the legs rest on the seafloor. A jackup rig is towed or propelled to a location with its legs up. Once the legs are firmly positioned on the bottom, the deck and hull height are adjusted and leveled.

jet bit n: a drilling bit having replaceable nozzles though which the drilling fluid is directed in a high-velocity stream to the bottom of the hole to improve efficiency of the bit. See bit.

jet gun n: an assembly, including a carrier and shaped charges, that is used in jet perforating.

jet-perforate v: to create a hole through the casing with a shaped charge of high explosives instead of a gun that fires projectiles. The loaded charge is lowered into the hole to the desired depth. Once detonated, the charges emit short, penetrating jets of high-velocity gases that cut holes in the casing and cement and some distance into the formation. Formation fluids then flow into the wellbore through these perforations. See bullet perforator and gun-perforate.

joint n: a single length (about 30 feet) of drill pipe or of drill collar, casing, or tubing, that has threaded connections at both ends. Several joints screwed together constitute a stand of pipe. See stand, single, double, thribble, and fourble.

junk n: metal debris lost in a hole. Junk may be a lost bit, pieces of a bit, milled pieces of pipe, wrenches, or any relatively small object that impedes drilling and must be fished out of the hole. v: to abandon (as a nonproductive well).


Appendix G

out

pany ls or ACT

aving

ell r

o

K

kelly n: the heavy steel member, four- or six-sided, suspended from the swivel through the rotary table and connected to the topmost joint of drill pipe to turn the drill string as the rotary table turns. It has a bored passageway that permits fluid to be circulated into the drill string and up the annulus, or vice versa. See drill stem, rotary table, and swivel.

kelly bushing n: a special device that, when fitted into the master bushing, transmits torque to the kelly and simultaneously permits vertical movement of the kelly to make hole. It may be shaped to fit the rotary opening or have pins for transmitting torque. Also called the drive bushing. See kelly and master bushing.

kelly spinner n: a pneumatically operated device mounted on top of the kelly that, when actuated, causes the kelly to turn or spin. it is useful when the kelly or a joint of pipe attached to it must be spun up; that is, rotated rapidly in order to make it up.

kick n: an entry of water, gas, oil, or other formation fluid into the wellbore. It occurs because the pressure exerted by the column of drilling fluid is not great enough to overcome the pressure exerted by the fluids in the formation drilled. If prompt action is not taken to control the kick or kill the well, a blowout will occur. See blowout.

L

LACT unit n: an automated system for measuring and transferring oil from a lease gathering system into a pipeline. See lease automatic custody transfer.

latch on v: to attach elevators to a section of pipe to pull it out of or run it into the hole.

lead tongs n: (pronounced “leed”) the pipe tongs suspended in the derrick or mast and operated by a wireline connected to the breakout cat-head. Also called breaktongs.

lease n: 1. a legal document executed between a land-owner, as lessor, and a comor individual, as lessee, that grants the right to exploit the premises for mineraother products. 2. the area where production wells, stock tanks, separators, Lunits, and other production equipment are located. See LACT unit and lease automatic custody transfer.

lease automatic custody n: the measurement and transfer of oil from the producer’s tanks to thetransfer connected pipeline on an automatic basis without a representative of either h

to be present. See LACT unit.

location n: the place where a well is drilled.

log n: a systematic recording of data, as from the driller’s log, mud log, electrical wlog, or radioactivity log. Many different logs are run in wells being produced odrilled to obtain various characteristics of downhole formations.

M

magnetic brake n: also called an electrodynamic brake. See electrodynamic brake.

make a connection v: to attach a joint of drill pipe onto the drill string suspended in the wellbore tpermit deepening of the wellbore.


Appendix G

a

oid

s the d to

on

lled a

alled

e igh as

tion

of

lly,

make a trip v: to hoist the drill string out of the wellbore to perform one of a number of operations such as changing bits, taking a core, and so forth, and then to return the drill string to the wellbore.

make hole v: to deepen the hole made by the bit; to drill ahead.

make up v: 1. to assemble and join parts to form a complete unit (as to make up a string of casing). 2. to screw together two threaded pieces. 3. to mix or prepare (as to make up a tank of mud). 4. to compensate for (as to make up for lost time).

make up a joint v: to screw a length of pipe into another length of pipe.

makeup cat-head n: a device attached to the shaft of the draw works that is used as a power source for screwing together joints of pipe; usually located on the driller’s side of thedraw works. See cat-head.

mast n: a portable derrick capable of being erected as a unit, as distinguished fromstandard derrick that cannot be raised to a working position as a unit. For transporting by land, the mast can be divided into two or more sections to avexcessive length extending from truck beds on the highway. Compare derrick.

master bushing n: a device that fits into the rotary table. It accommodates the slips and drivekelly bushing so that the rotating motion of the rotary table can be transmittethe kelly. Also called rotary bushing. See slips and kelly bushing.

mechanical rig n: a drilling rig in which the source of power is one or more internal-combustiengines and in which the power is distributed to rig components through mechanical devices (as chains, sprockets, clutches, and shafts). It is also capower rig.

mill n: a downhole tool with rough, sharp, extremely hard cutting surfaces for removing metal by grinding or cutting. Mills are run on drill pipe or tubing to grind up debris in the hole, remove stuck portions of drill stem or sections of casing for sidetracking, and ream out tight spots in the casing. They are also cjunk mills, reaming mills, and so forth, depending on what use they have. v: to use a mill to cut or grind metal objects that must be removed from a well.

mix mud v: to prepare drilling fluids from a mixture of water or other fluids and one or more of the various dry mud-making materials (as clay, weighting materials, chemicals, etc.).

monkey board n: the derrickman’s working platform. As pipe or tubing is run into or out of thhole, the derrickman must handle the top end of the pipe, which may be as h90 feet in the derrick or mast. The monkey board provides a small platform toraise him to the proper height to be able to handle the top of the pipe. See double board, fourable board, and thribble board.

morning tour n: (pronounced “tower”) also called daylight tour. See daylight tour.

motorman n: the crew member on a rotary drilling rig responsible for the care and operaof drilling engines.

mouse hole n: an opening through the rig floor, usually lined with pipe, into which a lengthdrill pipe is placed temporarily for later connection to the drill string.

mouse hole connection n: the procedure of adding a length of drill pipe or tubing to the active string inwhich the length to be added is placed in the mouse hole, made up to the kethen pulled out of the mouse hole, and subsequently made up into the string.


Appendix G

mud n: the liquid circulated through the wellbore during rotary drilling operations. In addition to its function of bringing up cuttings to the surface, drilling mud cools and lubricates the bit and drill stem, protects against blowouts by holding back subsurface pressures, and deposits a mud cake on the wall of the borehole to prevent loss of fluids to the formation. Although it originally was a suspension of earth solids (especially clays) in water, the mud used in modern drilling operations is a more complex, three-phase mixture of liquids, reactive solids, and inert solids. The liquid phase may be fresh water, seawater, and may contain one or more conditioners. See drilling fluid.

mud analysis n: examination and testing of the drilling mud to determine its physical and chemical properties.

mud cake n: the sheath of mud solids that forms on the wall of the hole when the liquid from the mud filters into the formation; also called wall cake or filter cake.

mud circulation n: the act of pumping mud downward to the bit and back up to the surface by normal circulation or reverse circulation. See normal circulation and reverse circulation.

mud conditioning n: the treatment and control of drilling mud to ensure that it has the correct properties. Conditioning may include the use of additives, the removal of sand or other solids, the removal of gas, the addition of water, and other measures to prepare the mud for conditions encountered in a specific well.

mud engineer n: a person whose duty is to test and maintain the properties of the drilling mud that are specified by the operator.

mud gun n: a pipe that shoots a jet of drilling mud under high pressure into the mud pit to mix additives with the mud.

mud man n: also called a mud engineer. See mud engineer.

mud pit n: a series of open tanks, usually made of steel plates, through which the drilling mud is cycled to allow sand and sediments to settle out. Additives are mixed with the mud in the pit, and the fluid is temporarily stored there before being pumped back into the well. Modern rotary drilling rigs are generally provided with three or more pits, usually fabricated steel tanks fitted with built-in piping, valves and mud agitators. Mud pits are also called shaker pits, settling pits, and suction pits, depending of their main purpose. See shaker pit, settling pit and suction pit.

mud pump n: a large, reciprocating pump used to circulate the mud on a drilling rig. A typical mud pump is a single- or double-acting, two- or three-cylinder piston pump whose pistons travel in replaceable liners and are driven by a crankshaft actuated by an engine or motor. Also called a slush pump.

mud-return line n: a trough or pipe placed between the surface connections at the wellbore and the shale shaker, through which drilling mud flows upon its return to the surface from the hole.

mud screen n: also called a shale shaker. See shale shaker.

N

natural gas n: a highly compressible, highly expandable mixture of hydrocarbons having a low specific gravity and occurring naturally in a gaseous form. Besides hydrocarbon gases, natural gas may contain appreciable quantities of nitrogen, helium, carbon dioxide, and contaminants (as hydrogen sulfide and water vapor).


Appendix G

Although gaseous at normal temperatures and pressures, certain of the gases comprising the mixture that is natural gas are variable in form and may be found either as gases or as liquids under suitable conditions of temperature and pressure.

needle valve n: a globe valve that incorporates a needle-point disk to produce extremely fine regulation of flow.

nipple n: a tubular pipe fitting threaded on both ends and less than 12 inches long.

nipple up v: in drilling, to assemble the blowout-preventer stack on the wellhead at the surface.

normal circulation n: the smooth, uninterrupted circulation of drilling fluid down the drill stem, out the bit, up the annular space between the pipe and the hole, and back to the surface. See mud circulation and reverse circulation.

O

offshore drilling n: drilling for oil in an ocean, gulf, or sea, usually on the continental shelf. A drilling unit for offshore operations may be a mobile floating vessel with a ship or barge hull, a semisubmersible or submersible base, a self-propelled or towed structure with jacking legs (jackup drilling rig), or a permanent structure used as a production platform when drilling is completed. In general, wildcat wells are drilled from mobile floating vessels (as semisubmersible rigs and drill ships) or from jack-ups, while development wells are drilled from platforms. See drill ship, jackup drilling rig, platform, semisubmersible drilling rig and wildcat.

oil field n: the surface area overlying an oil reservoir or reservoirs. Commonly, the term includes not only the surface area, but may include the reservoir, the wells, and production equipment as well.

oil sand n: 1. a sandstone that yields oil. 2. (by extension) any reservoir that yields oil, whether or not it is sandstone.

oil zone n: a formation or horizon of a well from which oil may be produced. The oil zone is usually immediately under the gas zone and on top of the water zone if all three fluids are present and segregated.

open adj: 1. of a wellbore, having no casing. 2. of a hole, having no drill pipe or tubing suspended in it.

open hole n: 1. any wellbore in which casing has not been set. 2. open or cased hole in which no drill pipe or tubing is suspended.

operator n: the person or company, either proprietor or lessee, actually operating an oilwell or lease. Compare unit operator.

overshot n: a fishing tool that is attached to tubing or drill pipe and lowered over the outside wall of pipe lost or stuck in the wellbore. A friction device in the overshot, usually either a basket or a spiral grapple, firmly grips the pipe, allowing the lost fish to be pulled from the hole.

P

P&A abbr: plug and abandon.

pay sand n: the producing formation, often one that is not even sandstone. It is also called pay, pay zone, and producing zone.


Appendix G

perforate v: to pierce the casing wall and cement to provide holes through which formation fluids may enter or to provide holes in the casing so that materials may be introduced into the annulus between the casing and the wall of the borehole. Perforating is accomplished by lowering into the well a perforating gun, or perforator, that fires electrically detonated bullets or shaped charges from the surface. See perforating gun.

perforating gun n: a device fitted with shaped charges or bullets that is lowered to the desired depth in a well and fired to create penetrating holes in casing, cement and formation. See gun-perforate.

permeability n: 1. a measure of the ability of fluids to flow through a porous rock. 2. fluid conductivity of a porous medium. 3. the ability of a fluid to flow within the interconnected pore network of a porous medium. See absolute permeability, effective permeability, and relative permeability.

petroleum n: oil or gas obtained from the rocks of the earth. See hydrocarbons.

pin n: the male section of the tool joint. See tool joint.

pipe ram n: a sealing component for a blowout preventer that closes the annular space between the pipe and the blowout preventer or wellhead. See annular space and blowout preventer.

platform n: an immobile, offshore structure constructed on pilings from which wells are drilled, produced, or both.

plug and abandon v: to place a cement plug into a dry hole and abandon it.

pore n: an opening or space within a rock or mass of rocks, usually small and often filled with some fluid (as water, oil, gas, or all three). Compare vug.

porosity n: the condition of something that contains pores (as a rock formation). See pore.

positive choke n: a choke in which the orifice size must be changed to change the rate of flow through the choke. See choke and orifice.

pressure n: the force that a fluid (liquid or gas) exerts when it is in some way confined within a vessel, pipe, hole in the ground, and so forth, such as that exerted against the inner wall of a tank or that exerted on the bottom of the wellbore by drilling mud. Pressure is often expressed in terms of force per unit of area, as pounds per square inch (psi).

pressure gauge n: an instrument for measuring fluid pressure that usually registers the difference between atmospheric pressure and the pressure of the fluid by indicating the effect of such pressures on a measuring element (as a column of liquid, a weighted piston, a diaphragm, or other pressure-sensitive device).

pressure gradient n: a scale of pressure differences in which there is a uniform variation of pressure from point to point. For example, the pressure gradient of a column of water is about 0.433 psi/ft of vertical elevation (9.794 kPa/m). The normal pressure gradient in a well is equivalent to the pressure exerted at any given depth by a column of 10 percent salt water extending from that depth to the surface (i.e., 0.465 psi/ft or 10.518 kPa/m).

pressure relief valve n: a valve that opens at a preset pressure to relieve excessive pressures within a vessel or line; also called a relief valve, safety valve, or pop valve.

preventer n: shortened form of blowout preventer. See blowout preventer.


Appendix G

primary cementing n: the cementing operation that takes place immediately after the casing has been run into the hole; used to provide a protective sheath around the casing, to segregate the producing formation, and to prevent the migration of undesirable fluids. See secondary cementing and squeeze cementing.

prime mover n: an internal-combustion engine that is the source of power for a drilling rig in oilwell drilling.

production n: 1. the phase of the petroleum industry that deals with bringing the well fluids to the surface and separating them and with storing, gauging, and otherwise preparing the product for the pipeline. 2. the amount of oil or gas produced in a given period.

proppant n: also called propping agent. See propping agent.

propping agent n: a granular substance (as sand grains, aluminum pellets, or other material) carried in suspension by the fracturing fluid that serves to keep the cracks open when the fracturing fluid is withdrawn after a fracture treatment.

psi abbr: pounds per square inch. See pressure.

pump n: a device that increases the pressure on a fluid or raises it to a higher level. Various types of pumps include the reciprocating pump, centrifugal pump, rotary pump, jet pump, sucker rod pump, hydraulic pump, mud pump, submersible pump, and bottomhole pump.

pump pressure n: fluid pressure from the action of the pump.

R

radioactivity well n: the recording of the natural or induced radioactive characteristics of subsurfacelogging formations. A radioactivity log, also known as a radiation log, normally consists

of two recorded curves: a gamma ray curve and a neutron curve. Both indicate the types of rock in the formation and the types of fluids contained in the rocks. The two logs may be run simultaneously in conjunction with a collar locator in a cased or uncased hole.

ram n: the closing and sealing component on a blowout preventer. One of three types - blind, pipe, or shear - may be installed in several preventers mounted in a stack on top of the wellbore. Blind rams, when closed, form a seal on a hole that has no drill pipe in it; pipe rams, when closed, seal around the pipe; shear rams cut through drill pipe and then form a seal. See blind ram, pipe ram, and shear ram.

ram blowout preventer n: a blowout preventer that uses rams to seal off pressure on a hole that is with or without pipe. It is also called a ram preventer. See blowout preventer and ram.

rat hole n: 1. a hole in the rig floor 30 to 35 feet deep, lined with casing that projects above the floor, into which the kelly and swivel are placed when hoisting operations are in progress. 2. a hole of a diameter smaller than the main hole that is drilled in the bottom of the main hole. v: to reduce the size of the wellbore and drill ahead.

reeve v: to pass (as the end of a rope) through a hole or opening in a block or similar device.

reeve the line v: to string wire-rope drill line through the sheaves of the traveling and crown blocks to the hoisting drum.

relative permeability n: a measure of the ability of two or more fluids (as water, gas, and oil) to flow through a rock formation when the formation is totally filled with several fluids.


Appendix G

The permeability measure of a rock filled with two or more fluids is different from the permeability measure of the same rock filled with only one fluid. Compare absolute permeability.

reserve pit n: 1. (obsolete) a mud pit in which a supply of drilling fluid was stored. 2. a waste pit, usually excavated, earthen-walled pit. It may be lined with plastic to prevent contamination of the soil.

reservoir n: a subsurface, porous, permeable rock body in which oil and/or gas is stored. Most reservoir rocks are limestones, dolomites, sandstones, or a combination of these. The three basic types of hydrocarbon reservoirs are oil, gas, and condensate. An oil reservoir generally contains three fluids - gas, oil, and water - with oil the dominant product. In the typical reservoir, these fluids occur in different phases because of the variance in their gravities. Gas, the lightest, occupies the upper part of the reservoir rocks; water, the lower part; and oil, the intermediate section. In addition to occurring as a cap or in solution, gas may accumulate independently of the oil; if so, the reservoir is called a gas reservoir. Associated with the gas, in most instances, are salt water and some oil. In a condensate reservoir, the hydrocarbons may exist as a gas, but when brought to the surface, some of the heavier ones condense to a liquid or condensate.

reservoir pressure n: the pressure in a reservoir under normal conditions.

reverse circulation n: the return of drilling fluid through the drill stem. The normal course of drilling fluid circulation is downward through the drill stem and upward through the annular space surrounding the drill stem. For special problems, normal circulation is sometimes reversed, and the fluid returns to the surface through the drill stem, or tubing, after being pumped down the annulus.

rig n: the derrick or mast, draw works, and attendant surface equipment of a drilling unit.

rig down v: to dismantle the drilling rig and auxiliary equipment following the completion of drilling operations; also called tear down.

rig up v: to prepare the drilling rig for making hole; to install tools and machinery before drilling is started.

roller cone bit n: a drilling bit made of two, three, or four cones, or cutters, that are mounted on extremely rugged bearings. Also called rock bits. The surface of each cone is made up of rows of steel teeth or rows of tungsten carbide inserts. See bit.

rotary bushing n: also called master bushing. See master bushing.

rotary drilling n: a drilling method in which a hole is drilled by a rotating bit to which downward force is applied. The bit is fastened to and rotated by the drill stem, which also provides a passageway through which the drilling fluid is circulated. Additional joints of drill pipe are added as drilling progresses.

rotary helper n: a worker on a drilling rig, subordinate to the driller, sometimes called a roughneck, floorman, or rig crewman.

rotary hose n: a reinforced, flexible tube on a rotary drilling rig that conducts the drilling fluid from the mud pump and standpipe to the swivel and kelly; also called the mud hose or kelly hose. See kelly, mud pump, standpipe, and swivel.

rotary table n: the principal component of a rotary or rotary machine, used to turn the drill stem and support the drilling assembly. It has a beveled gear arrangement to create


Appendix G

ed up

the rotational motion and an opening into which bushings are fitted to drive and support the drilling assembly.

roughneck n: also called a rotary helper. See rotary helper.

round trip n: the action of pulling out and subsequently running back into the hole a string of drill pipe or tubing. It is also called tripping.

roustabout n: 1. a worker on an offshore rig who handles the equipment and supplies that are sent to the rig from the shore base. The head roustabout is very often the crane operator. 2. a worker who assists the foreman in the general work around a producing oil well, usually on the property of the oil company. 3. a helper on a well-servicing unit.

run in v: to go into the hole with tubing, drill pipe, and so forth.

S

samples n pl: 1. the well cuttings obtained at designated footage intervals during drilling. From an examination of these cuttings, the geologist determines the type of rock and formation being drilled and estimates oil and gas content. 2. small quantities of well fluids obtained for analysis.

sand n: 1. an abrasive material composed of small quartz grains formed from the disintegration of preexisting rocks. Sand consists of particles less than 2 millimeters and greater than 1/16 of a millimeter in diameter. 2. sandstone.

scratcher n: a device fastened to the outside of casing that removes the mud cake from the wall of the hole to condition the hole for cementing. By rotating or moving the casing string up and down as it is being run into the hole, the scratcher, formed of stiff wire, removes the cake so that the cement can bond solidly to the formation.

secondary cementing n: any cementing operation after the primary cementing operation. Secondary cementing includes a plug-back job, in which a plug of cement is positioned at a specific point in the well and allowed to set. Wells are plugged to shut off bottom water or to reduce the depth of the well for other reasons. See primary cementing and squeeze cementing.

seismograph n: a device that detects reflections of vibrations in the earth, used in prospecting for probable oil-bearing structures. Vibrations are created by discharging explosives in shallow boreholes, by striking the surface with a heavy blow, or by generating low-frequency sound waves. The type and velocity of the vibrations as recorded by the seismograph indicate the general characteristics of the section of earth through which the vibration pass.

semi-submersible n: a floating, offshore drilling structure that has hulls submerged in the waterdrilling rig but not resting on the seafloor. Living quarters, storage space, and so forth are

assembled on the deck. Semisubmersible rigs are either self-propelled or towed to a drilling site and either anchored or dynamically positioned over the site or both. Semi-submersibles are more stable than drill ships and are used extensively to drill wildcat wells in rough water such as the North Sea. See dynamic positioning.

set casing v: to run and cement casing at a certain depth in the wellbore. Sometimes, the term “set pipe” is used when referring to setting casing.

settling pit n: the mud pit into which mud flows and in which heavy solids are allowed tosettle out. Often auxiliary equipment (as de-sanders) must be installed to spethis process.


Appendix G

illing

et the

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s he ually

t are . ices g a y

;

nce

shaker n: shortened form of shale shaker. See shale shaker.

shaker pit n: the mud pit adjacent to the shale shaker, usually the first pit into which the mud flows after returning from the hole.

shale n: a fine-grained sedimentary rock composed of consolidated silt and clay or mud. Shale is the most frequently occurring sedimentary rock.

shale shaker n: a series of trays with sieves that vibrate to remove cuttings from the circulating fluid in rotary drilling operations. The size of the openings in the sieve is carefully selected to match the size of the solids in the drilling fluid and the anticipated size of the cuttings. Also called a shaker.

shaped charge n: a relatively small container of high explosive that is loaded into a perforating gun. Upon detonation, the charge releases a small, high-velocity stream of particles (a jet) that penetrates the casing, cement, and formation. See gun-perforate.

shear ram n: the components in a blowout preventer that cut, or shear, through drill pipe and form a seal against well pressure. Shear rams are used in mobile offshore drilling operations to provide a quick method of moving the rig away from the hole when there is no time to trip the drill stem of the hole.

sheave n: (pronounced “shiv”) a grooved pulley.

show n: the appearance of oil or gas in cuttings, samples, cores, and so forth of drmud.

shut down v: to stop work temporarily or to stop a machine or operation.

shut-in bottomhole n: the pressure at the bottom of a well when the surface valves on the well arpressure completely closed. The pressure caused by fluids that exist in the formation a

bottom of the well.

sidetrack v: to drill around broken drill pipe or casing that has become lodged permanein the hole, using a whipstock, turbo-drill, or other mud motor. See directional drilling, turbo-drill, and whipstock.

sidewall coring n: a coring technique in which core samples are obtained from a zone that haalready been drilled. A hollow bullet is fired into the formation wall to capture tcore and then retrieved on a flexible steel cable. Core samples of this type usrange from 3/4 to 13/16 inches in diameter and from 3/4 to 1 inch in length. This method is especially useful in soft rock areas.

single n: a joint of drill pipe. Compare double, thribble, and fourable.

slips n pl: wedge-shaped pieces of metal with teeth or other gripping elements thaused to prevent pipe from slipping down into the hole or to hold pipe in placeRotary slips fit around the drill pipe and wedge against the master bushing tosupport the pipe. Power slips are pneumatically or hydraulically actuated devthat allow the crew to dispense with the manual handling of slips when makinconnection. Packers and other downhole equipment are secured in position bslips that engage the pipe by action directed at the surface.

slurry n: a plastic mixture of cement and water that is pumped into a well to hardenthere it supports the casing and provides a seal in the wellbore to prevent migration of underground fluids.

sonic logging n: the recording of the time required for a sound wave to travel a specific distathrough a formation. Difference in observed travel times is largely caused by


Appendix G

variations in porosities of the medium, an important determination. The sonic log, which may be run simultaneously with a spontaneous potential log or a gamma ray log, is useful for correlation and often is used in conjunction with other logging services for substantiation of porosities. It is run in an uncased hole.

spear n: a fishing tool used to retrieve pipe lost in a well. The spear is lowered down the hole and into the lost pipe, and when weight, torque, or both are applied to the string to which the spear is attached, the slips in the spear expand and tightly grip the inside of the wall of the lost pipe. Then the string, spear, and lost pipe are pulled to the surface.

specific gravity n: the ratio of the weight of a given volume of a substance at a given temperature to the weight of an equal volume of a standard substance at the same temperature. For example, if 1 cubic inch of water at 39oF weighs 1 unit and 1 cubic inch of another solid or liquid at 39oF weighs 0.95 unit, then the specific gravity of the substance is 0.95. In determining the specific gravity of gases, the comparison is made with the standard of air or hydrogen. See gravity.

spinning cat-head n: a spooling attachment on the makeup cat-head to permit use of a spinning chain to spin up or make up drill pipe. See spinning chain.

spinning chain n: a Y-shaped chain used to spin up (tighten) one joint of drill pipe to another. In use, one end of the chain is attached to the tongs, another end to the spinning cat-head, and the third end is free. The free end is wrapped around the tool joint, and the cat-head pulls the chain off the joint, causing the to spin (turn) rapidly and tighten up. After the chain is pulled off the joint, the tongs are secured in the same spot, and continued pull on the chain (and thus on the tongs) by the cat-head makes up the joint to final tightness.

spud v: to move the drill stem up and down in the hole over a short distance without rotation. Careless execution of this operation creates pressure surges that can cause a formation to break down, which results in lost circulation. See spud in.

spud in v: to being drilling, to start the hole.

squeeze cementing n: the forcing of cement slurry by pressure to specified points in a well to cause seals at the points of squeeze. It is a secondary cementing method that is used to isolate a producing formation, seal off water, repair casing leaks, and so forth. See cementing.

stab v: to guide the end of a pipe into a coupling or tool joint when making a connection. See coupling and tool joint.

stabbing board n: a temporary platform erected in the derrick or mast some 20 to 40 feet above the derrick floor. The derrickman or another crew member works on the board while casing is being run in a well. The board may be wooden or fabricated of steel girders floored with anti-skid material and powered electrically to raise or lower it to the desired level. A stabbing board serves the same purpose as a monkey board but is temporary instead of permanent.

stake a well v: to locate precisely on the surface of the ground the point at which a well is to be drilled. After exploration techniques have revealed the possibility of the existence of a subsurface hydrocarbon-bearing formation, a certified and registered land surveyor drives a stake into the ground to mark the spot where the well is to be drilled.


Appendix G

stand n: the connected joints of pipe racked in the derrick or mast when making a trip. On a rig, the usual stand is 90 feet long (three lengths of pipe screwed together) or a thribble. Compare double and fourble.

standpipe n: a vertical pipe rising along the side of the derrick or mast, which joins the discharge line leading from the mud pump to the rotary hose and through which mud is pumped going into the hole. See mud pump and rotary hose.

stimulation n: any process undertaken to enlarge old channels or create new ones in the producing formation of a well (e.g., acidizing or formation fracturing) See acidize.

stratification n: the natural layering or lamination characteristic of sediments and sedimentary rocks.

stratigraphic trap n: a petroleum trap that occurs when the top of the reservoir bed is terminated by other beds or by a change of porosity or permeability within the reservoir itself. Compare structural trap. See trap.

string n: the entire length of casing, tubing, or drill pipe run into a hole; the casing string. Compare drill string and drill stem.

string up v: to thread the drill line through the sheaves of the crown block and traveling block. One end of the line is secured to the hoisting drum and the other to the derrick substructure. See sheave.

structural trap n: a petroleum trap that is formed because of deformation (as folding or faulting) of the rock layer that contains petroleum. Compare stratigraphic trap. See trap.

stuck pipe n: drill pipe, drill collars, casing, or tubing that has inadvertently become immobile in the hole. It may occur when drilling is in progress, when casing is being run in the hole, or when the drill pipe is being hoisted.

sub n: a short, threaded piece of pipe used to adapt parts of drill string that cannot otherwise be screwed together because of differences in thread size or design. A sub may also perform a special function. Lifting subs are used with drill collars to provide a shoulder to fit the drill pipe elevators. A kelly saver sub is placed between the drill pipe and kelly to prevent excessive thread wear of the kelly and drill pipe threads. A bent sub is used when drilling a directional hole. Sub is a sort expression for substitute.

submersible drilling rig n: an offshore drilling structure with several compartments that are flooded to cause the structure to submerge and rest on the seafloor. Most submersible rigs are used only in shallow water.

substructure n: the foundation on which the derrick or mast and usually the draw works sit; contains space for storage and well control equipment.

suction pit n: the mud pit from which mud is picked up by the suction of the mud pumps; also called a sump pit and mud suction pit.

surface casing n: also called surface pipe. See surface pipe.

surface data logging n: the recording of information derived from examination and analysis of formation cuttings made by the bit and mud circulated out of the hole. A portion of the mud is diverted through a gas-detecting device. Cuttings brought up by the mud are examined under ultraviolet light to detect the presence of oil and gas. Surface data logging is often carried out in a portable laboratory set up at the well.

surface pipe n: the first string of casing (after the conductor pipe) that is set in a well, varying in length from a few hundred to several thousand feet. Some states require a


Appendix G

minimum length to protect freshwater sands. Compare conductor pipe.

swivel n: a rotary tool that is hung from the rotary hook and traveling block to suspend and permit free rotation of the drill stem. It also provides a connections for the rotary hose and passageway for the flow of drilling fluid into the drill stem.

syncline n: a down-warped, trough-shaped configuration of folded, stratified rocks. Compare anticline.

T

TD abbr: total depth.

thread protector n: a device that is screwed onto or into pipe threads to protect the threads from damage when the pipe is not in use. Protectors may be metal or plastic.

thribble n: a stand of pipe made up of three joints and handled as a unit. See stand. Compare single, double, and fourble.

thribble board n: the name used for the working platform of the derrickman, or monkey board, when it is located at a height in the derrick equal to three lengths of pipe joined together. Compare double board and fourble board. See monkey board.

throw the chain n: to flip the spinning chain up from a tool joint box so that the chain wraps around the tool joint pin after it is stabbed into the box. The stand or joint of drill pipe is turned or spun by a pull on the spinning chain from the cat-head or draw works.

tight formation n: a petroleum- or water-bearing formation of relatively low porosity and permeability. See porosity and permeability.

tight hole n: a well about which information is restricted and passed only to those authorized for security or competitive reasons.

tongs n pl: the large wrenches used for turning when making up or breaking out drill pipe, casing, tubing, or other pipe; variously called casing tongs, rotary tongs, and so forth according to the specific use. Power tongs are pneumatically or hydraulically operated tools that serve to spin the pipe up tight and, in some instances, to apply the final makeup torque. See also chain tongs.

tool joint n: a heavy coupling element for drill pipe made of special alloy steel. Tool joints have coarse, tapered threads and seating shoulders designed to sustain the weight of the drill stem, withstand the strain of frequent coupling and uncoupling, and provide a leakproof seal. The male section of the joint, or the pin, is attached to one end of a length of drill pipe, and the female section, or box, is attached to the other end. The tool joint may be welded to the end of the pipe or screwed on or both. A hard metal facing is often applied in a band around the outside of the tool joint to enable it to resist abrasion from the walls of the borehole.

tool pusher n: an employee of a drilling contractor who is in charge of the entire drilling crew and the drilling rig. Also called a drilling rig foreman, manager, supervisor, or rig superintendent. See drilling foreman.

torque n: the turning force that is applied to a shaft or other rotary mechanism to cause it to rotate or tend to do so. Torque is measured in foot-pounds, joules, meter-kilograms, and so forth.

torque converter n: a connecting device between a prime mover and the machine actuated by it. The elements that pump the fluid in the torque converter automatically increase


Appendix G

er nd

e

es in

ed

ch a y be

.

on is

e alve,

lleys,

the output torque of the engine to which the torque is applied, with an increase of load on the output shaft. Torque converters are used extensively on mechanical rigs that have a compound. See mechanical rig.

total depth n: the maximum depth reached in a well.

tour n: (pronounced “tower”) an 8- or 12-hour shift worked by a drilling crew or othoil field workers. The most common divisions of tours are daylight, evening, agraveyard, if 8-hour tours are employed.

transmission n: the gear or chain arrangement by which power is transmitted from the primmover to the draw works, mud pump, or rotary table of a drilling rig. See prime mover.

trap n: layers of buried rock strata that are arranged so that petroleum accumulatthem.

traveling block n: an arrangement of pulleys, or sheaves, through which drilling cable is reevand that moves up and down in the derrick or mast. See block, crown block, and sheave.

tricone bit n: a type of bit in which three cone-shaped cutting devices are mounted in suway that they inter-mesh and rotate together as the bit drills. The bit body mafitted with nozzles, or jets, through which the drilling fluid is discharged. A one-eyed bit is used in soft formations to drill a deviated hole. See directional drilling and bit.

trip n: the operation of hoisting the drill stem from and returning it to the wellboreSee make a trip.

turbo-drill n: a drilling tool that rotates a bit attached to it by the action of the drilling mudthe turbine blades built into the tool. When a turbo-drill is used, rotary motionimparted only at the bit; therefore, it is unnecessary to rotate the drill stem. Although straight holes can be drilled with the tool, it is used most often in directional drilling.

U

unit operator n: the oil company in charge of development and producing in an oil field in which several companies have joined together to produce the field.

V

valve n: a device used to control the rate of flow in a line, to open or shut off a line completely, or to serve as an automatic or semiautomatic safety device. Thoswith extensive usage include the gate valve, plug valve, globe valve, needle vcheck valve, and pressure relief valve. See check valve, needle valve and pressure relief valve.

V-belt n: a belt with a trapezoidal cross-section that is made to run in sheaves or puwith grooves of corresponding shape. See belt.

vug n: a cavity in a rock.


Appendix G

ght

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ay y be

f oil een

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rom

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other used e, nder

W

waiting on cement adj: pertaining to or during the time when drilling or completion operations are suspended so the cement in a well can harden sufficiently.

wall cake n: also called filter cake and mud cake. See filter cake and mud cake.

weevil n: shortened form of boll weevil. See boll weevil.

weight indicator n: an instrument near the driller’s position on a drilling rig. It shows both the weight of the drill stem that is hanging from the hook (hook load) and the weithat is placed on the bit by the drill collars (weight on bit).

weighting material n: a material that has high specific gravity and is used to increase the densitydrilling fluids or cement slurries.

wellbore n: a borehole; the hole drilled by the bit. A wellbore may have casing in it or mbe open (i.e., uncased), or a portion of it may be cased and a portion of it maopen. Also called borehole or hole. See cased and open.

well completion n: the activities and methods necessary to prepare a well for the production oand gas; the method by which a flow line for hydrocarbons is established betwthe reservoir and the surface. The method of well completion used by the opedepends on the individual characteristics of the producing formation or formations. These techniques include open-hole completions, sand exclusioncompletions, tubingless completions, multiple completions, and miniaturized completions.

wellhead n: the equipment installed at the surface of the wellbore. A wellhead includes equipment as the casing head and tubing head. adj pertaining to the wellhead (as wellhead pressure).

well logging n: the recording of information about subsurface geologic formations. Logginmethods include records kept by the driller, mud and cutting analyses, core analysis, drill stem tests, and electric and radioactivity procedures. See electric well log, mud logging, radioactivity well logging, and sonic logging.

well stimulation n: any of several operations used to increase the production of a well. See acidize and formation fracturing.

whipstock n: a long, steel casing that uses an inclined plane to cause the bit to deflect fthe original borehole at a slight angle. Whipstocks are sometimes used in controlled directional drilling, to straighten crooked boreholes, and to sidetracavoid unretrieved fish. See directional drilling, fish, and sidetrack.

wildcat n: 1. a well drilled in an area where no oil or gas production exists. With present-day exploration methods and equipment, about one wildcat out of evnine proves to be productive although not necessary profitable. 2. (nautical) ageared sheave of a windlass used to pull anchor chain. v: to drill wildcat wells.

wireline n: a slender, rodlike or threadlike piece of metal, usually small in diameter, thused for lowering special tools (such as logging sondes, perforating guns, anforth) into the well. Compare wire rope.

wire rope n: a cable composed of steel wires twisted around a central core of hemp or fiber to create a rope of great strength and considerable flexibly. Wire rope is as drill line (in rotary and cable-tool rigs), coring line, servicing line, winch linand so on. It is often called cable or wireline; however, wireline is a single, slemetal rod, usually very flexible. Compare wireline.


Appendix G

WOC abbr: waiting on cement.

worm n: a new and inexperienced worker on a drilling rig.


Appendix G


Documents

Halliburton - Surface Data Logging Manual