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Reservoir Rock Properties

Rock Properties

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Page 1: Rock Properties

Reservoir Rock Properties

Page 2: Rock Properties

2

Scales of Geological Reservoir Heterogeneity

Fiel

d W

ide

Inte

rwel

lW

ell-B

ore

(modified from Weber, 1986)

Hand Lens orBinocular Microscope

Unaided Eye

Petrographic orScanning Electron

Microscope

DeterminedFrom Well Logs,Seismic Lines,

StatisticalModeling,

etc.

10-100'sµm

10-100'smm

1-10'sm

100'sm

10'sm

1-10 km

100's m

Well WellInterwell

Area

ReservoirSandstone

Page 3: Rock Properties

3

Gigascopic

Megascopic

Macroscopic

Microscopic

Well Test

Reservoir ModelGrid Cell

Wireline LogInterval

Core Plug

GeologicalThin Section

Relative Volume

1

1014

2 x 10 12

3 x 10 7

5 x 102

300 m

50 m

300 m

5 m 150 m

2 m1 m

cm

mm - µm

(modified from Hurst, 1993)

Scales of Investigation Used in Reservoir Characterization

Page 4: Rock Properties

4

Core Data

The core measures absolute permeability on an inch3 scale.

Core preparation may change some of the rock properties.

Core permeabilities may not reflect reservoir conditions.

The core measures absolute permeability on an inch3 scale. The flow in the reservoir is controlled by effective permeability on much larger scales. To estimate effective permeability at in situ conditions one must account for relative permeability effects and effect of net overburden.

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Permeability Estimates Based on Log Data

The log based methods measure permeability on a ft3 scale.Empirical correlation of core permeability with log porosity or other dataProduction logging MDT log - pressure buildup analysis

Several possible log-based estimates are possible including: An empirical correlation between core permeability and logging measurements such as porosity, Vsh, or

other petrophysical dataAn experimental technique is to estimate permeability using multiple logs and mud filtrate invasionA Nuclear Magnetism Log (NML) may give reasonable estimates of permeability in some formations.

Production logging provides information on what fraction of the total inflow comes from some specific depth of the formation. If total permeability is estimated from a well test or production data analysis, production logging will give an estimate of individual layer permeabilities.MDT is an open-hole wireline tool that provides accurate down-hole measurements of formation pressure. This pressure information can be analyzed to estimate k.

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Permeability Estimates Based on Welltest DataThe transient pressure testing measures permeability on a 106

ft3 scale.Test Types:

Short-term testing (DST)Conventional buildup testSpecial (pulse, interference)

All transient pressure methods involve abrupt changes in flow while recording the pressure response caused by the changes. The pressure responses are analyzed to help characterize the well and reservoir.A DST (drill-stem test) is typically performed on exploratory wells to confirm an initial log interpretation. The test typically involves two drawdowns and two build-ups.Conventional tests are drawdown and build-up.Advanced test techniques are beyond the scope of this course. The purpose of these tests is to gain additional information about the reservoir or the interwell communication.

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Permeability Estimates Based on Production DataThe methods based on analysis of production data measure permeability in a total drainage area, on a 106 - 108 ft3 scale.Analytical techniques (type-curve analysis) Reservoir simulation methods

Methods based on analysis of production data involve matching the observed well performance given the flowing pressure history. Analytical techniques (type-curve analyses) generate production forecasts using analytical, single phase solutions for assumed reservoir geometries. Reservoir simulation methods may be necessary when complex reservoir geometries are apparent or when multi-phase flow of fluids occur.

Page 8: Rock Properties

Fluid Saturations

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Definition of Fluid Saturation

Water saturation:

Oil saturation:

Gas saturation:

p

ww V

VS =

p

oo V

VS =

wog SS0.1S −−=

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10

Grain Water Gas Oil

Fluid Saturation

Initially, pore space filled 100% with water and wets the rock surfaceHydrocarbons migrate from source rock to the reservoir rock and displace portion of the waterHydrocarbons distributed by capillary forces and gravity

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Determining Fluid Saturations

Conventional core analysis

Capillary pressure measurements

log analysis

Page 12: Rock Properties

Rock Wettability

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Instructional Objectives

Define Wettability, interfacial tension, and adhesion tensionDefine & give examples of drainage and imbibition processesExplain the difference between water-wet and oil-wet rocksExplain the effects of wettability on waterflood performanceList the common laboratory methods to measure wettability

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DefinitionsWettability: Tendency of one fluid to spread on or adhere to a solid surface in the presence of other immiscible fluidsWettability refers to interaction between fluid and solid phases

Definition of Wettability

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Interfacial tension is the force per unit length required to create a

new surface

Interfacial tension is commonly expressed in Newtons/meter or dynes/cm.

Definition of Interfacial Tension

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Adhesion tension can be expressed as the difference between

two solid-fluid interfacial tensions

θσσσ cosowwsosTA =−=

Definition of Adhesion Tension

A negative adhesion tension indicates that the denser phase preferentially wets the solid surface.

An adhesion tension of zero indicates that both phases have an equal affinity for the surface.

Page 17: Rock Properties

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Solid

Water

Oil

Oil Oil

σos σws

σow

θ

Contact Angle

The contact angle, θ, is measured through the denser liquid phase.Contact angle ranges from 0o to 180o.Contact angle defines which fluid wets the solid surface.

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Solid surface is reservoir rock (i.e., sandstone, limestone, dolomite or mixtures of each)

Fluids are oil, water, and/or gas

In Hydrocarbon Reservoirs

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Wetting phase preferentially wets the solid rock surfaceBecause of attractive forces between rock and fluid, the wetting phase is drawn into smaller pore spaces of porous mediaWetting phase fluid often is not very mobileAttractive forces prohibit reduction in wetting phase saturationbelow some irreducible value (called irreducible wetting phase saturation)Many hydrocarbon reservoirs tend to be either totally or partially water wet

Wetting Phase Fluid

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Nonwetting phase does not preferentially wet the solid rock surfaceRepulsive forces between rock and fluid cause nonwetting phase to occupy largest pore spaces of porous mediaNonwetting phase fluid is often the most mobile fluid, especially at large nonwetting phase saturationsNatural gas is never the wetting phase in hydrocarbon reservoirs

Nonwetting Phase Fluid

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Reservoir rock is considered to be water-wet if water preferentially wets the rock surfaces

The rock is water-wet under the following conditions:σws > σos

AT < 0 (i.e., the adhesion tension is negative)0° < θ < 90°

If θ is close to 0°, the rock is considered to be “strongly water-wet”

Water-Wet Reservoir Rock

Page 22: Rock Properties

22

Solid

WaterOil

σos σws

σow

θ

Note: 0° < θ < 90°

Force Balance – Water Wet Rock

In water-wet rocks, contact angle, q, is less than 90o and the adhesion tension between water and the rock surface is larger than that between oil and the rock surface.

Page 23: Rock Properties

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Reservoir rock is considered to be oil-wet if oil preferentially wets the rock surfaces

The rock is oil-wet under the following conditions:σos > σws

AT > 0 (i.e., the adhesion tension is positive)90° < θ < 180°

If θ is close to 180°, the rock is considered to be “strongly oil-wet”

Oil-Wet Reservoir Rock

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Solid

Water

Oil

σos σws

σow

θ

Note: 90° < θ < 180°

Force Balance – Oil-Wet Rock

In oil-wet rocks, contact angle, q, is greater than 90o and less than 180o. The adhesion tension between water and the rock surface is less than that between oil and the rock surface.

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Fluid flow process in which the saturation of the wetting phase increases and the nonwetting phase saturation decreases

Mobility of wetting phase increases as wetting phase saturation increases

Imbibition

Example: Waterflooding of an oil reservoir in which the reservoir rock is preferentially water-wet

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Fluid flow process in which the saturation of the nonwetting phase increases

Mobility of nonwetting fluid phase increases as nonwetting phasesaturation increases

Drainage

Example:Waterflooding an oil reservoir in which the reservoir rock is preferentially oil-wetGas injection in an oil- or water-wet oil reservoirPressure maintenance or gas cycling by gas injection in a retrograde condensate reservoir

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Wettability affects the shape of the relative permeability curves.

Oil moves easier in water-wet rocks than oil-wet rocks.

Implication of Wettability

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Primary oil recovery is affected by the wettability of the system.

A water-wet system will exhibit greater primary oil recovery.

Implication of Wettability

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Oil recovery under waterflooding is affected by the wettability of the system.

A water-wet system will exhibit greater oil recovery under waterflooding.

Implication of Wettability

Page 30: Rock Properties

Capillary Pressure

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List four uses of capillary pressure data

Define hysteresis

Sketch capillary pressure curves for typical drainage and imbibition processes

Explain the relation between capillary pressure data and reservoir fluid saturation

Define oil-water and gas-oil transition zones

Instructional Objectives

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Determine initial (irreducible) water saturation in the reservoirDetermine fluid distribution in reservoir Determine residual oil saturation for water flooding applicationsDetermine pore size distribution index May help in identifying zones or rock types

Input for reservoir simulation calculations.

Uses of Capillary Pressure Data

(1) Capillary pressure measurements determine the initial water saturation. This is the saturation at which the increase in capillary pressure does not affect the saturation.(2) Capillary pressure data can also determine the vertical fluid distribution in the reservoir by establishing the relation between the capillary pressure and height above the free water level.(3) Imbibition capillary pressure measurements determine the residual oil saturation in water flooding operation.(4) We can infer the pore size distribution index, l, from capillary pressure data. This index can be used to calculate relative permeability using industry correlations.(5) Capillary pressure curves are similar for the same rock type. The shape also give indication about the rock permeability.(6) Capillary pressure curves are used to initialize simulation runs and in flow calculations between grid blocks.

Page 33: Rock Properties

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A B

ρo

ρw1

2

3Pc = 0

Pressure

Dep

th

ρw ρo

Capillary Pressure Concept

Water exists at all levels below 2, and both water and oil exist at all levels above 2.

Oil and water pressure gradients are different because their density is different.

At level 2, pressure in both the water and oil phases is the same.

At any level above 2, such as level 3, water and oil pressures are different.

This difference in pressure is called the capillary pressure.

Page 34: Rock Properties

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The pressure difference existing across the interface separating two immiscible fluids.

It is usually calculated as:

Pc = pnwt - pwt

Capillary Pressure Definition

One fluid wets the surfaces of the formation rock (wetting phase) in preference to the other (non-wetting phase).

Gas is always the non-wetting phase in both oil-gas and water-gas systems.

Oil is often the non-wetting phase in water-oil systems.

Page 35: Rock Properties

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Water

Airθ∆h

Capillary Tube Model – Air/Water System

aw

aw

grh

ρθσ

∆=∆

cos2

Upward force is due to adhesion tension

We can imagine the porous media as a collection of capillary tubes. This model is useful for providing insight into how fluids behave in the reservoir pore spaces.

Page 36: Rock Properties

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Air

Water

pa2

∆h

pa1

pw1

pw2

Capillary Tube Model – Air/Water System

gPhaw

c

ρ∆=∆

Page 37: Rock Properties

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Combining the two relations:

Results in the following expression:aw

aw

grh

ρθσ

∆=∆

cos2

rP awc

θσ cos2=

Capillary Pressure – Air/Water System

gPhaw

c

ρ∆=∆

Page 38: Rock Properties

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The height of water in a capillary tube is a function of

The adhesion tension between the air and water

The radius of the tube

The density difference between fluids

aw

aw

grh

ρθσ

∆=∆

cos2

Capillary Tube Model – Air/Water System**

Page 39: Rock Properties

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From a similar derivation, the equation for capillary pressure for an oil/water system is

rP owc

θσ cos2=

Capillary Pressure – Oil/Water System

Page 40: Rock Properties

40

A B

ρo

ρw1

2

3Pc = 0

PressureD

epth

ρw ρo

Capillary Pressure Concept

Page 41: Rock Properties

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The height of water is a function of

The adhesion tension between the oil and water

The radius of the tube

The density difference between fluids

ow

ow

grh

ρθσ

∆=∆

cos2

Capillary Tube Model- Oil/Water System

Page 42: Rock Properties

42

Free Water Level

Pc

Pd

Water-oil contactHd

Hei

ght A

bove

Fre

e W

ater

Lev

el (

Feet

)

0 50 100Sw (Percent)

0 50 100Sw (Percent)

0

Relation Between Capillary Pressure and Fluid Saturations

Page 43: Rock Properties

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Gas & Water

Gas density = ρg

Oil, Gas & Water

Oil & Water

Oil density = ρo

Water

Water density = ρw

‘A’

h1

h2

‘B’

Free Oil Level

Free Water Level

Capillary pressure difference between

oil and water phases in core ‘A’Pc = h1g (ρw-ρo)

Capillary pressure difference betweengas and oil phases in core ‘B’

Pc = h2g (ρo-ρg)

Fluid Distribution in Petroleum Reservoirs

Page 44: Rock Properties

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VCLdec0 1

0 VCL

VCL 1

ILDCohmm0.2 200

RHOCNus/f1.65 2.65

CNLLSS 0.6 0

DTCus/f135 55

RHOCN CNLLSS

GASus/f1 0

BVWdec1 0

OIL 1 0

BVWG 1 0

SWdec1 -1

10750

10800

Fluid Distribution

Page 45: Rock Properties

45

Drainage (1)

Imbibition (2)

Si Sm

Sw

Pd

Pc

0 0.5 1.0

Typical Drainage & Imbibition Pc Curves

Page 46: Rock Properties

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Fluid flow process in which the saturation of the nonwetting phase increases

Mobility of nonwetting fluid phase increases as nonwetting phasesaturation increases

Drainage Process

Page 47: Rock Properties

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Fluid flow process in which the saturation of the wetting phase increases and the nonwetting phase saturation decreases

Mobility of wetting phase increases as wetting phase saturation increases

Imbibition Process

Page 48: Rock Properties

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50

0

45

40

35

30

25

20

15

10

5

(1)

(2)

Sw

Pc , psi

0 0.5 1.00.25 0.75

Exercise 1The given figure is the result of core flood experiments on a water-wet rock. Answer the following questions:(1) What process does curve 1 represent?(2) What process does curve 2 represent?(3) What is the irreducible water saturation?(4) What is the residual oil saturation?(5) What is the displacement or threshold pressure?

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50

0

45

40

35

30

25

20

15

10

5

(1)

(2)

Sw

Pc , psi

0 0.5 1.00.25 0.75

Exercise 1 – Solution(1)What process does curve 1 represent?Drainage Process(2) What process does curve 2 represent?Imbibition Process(3) What is the irreducible Sw? Swirr = 0.25(4) What is the residual oil saturation? Sorw = 0.15(5) What is the displacement pressure? Pd = 12 psi

***

Page 50: Rock Properties

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Capillary pressure characteristics in reservoir are affected by

Variations in permeability

Grain size distribution

Saturation history

Contact angle

Interfacial tension

Density difference between fluids

Effect of Reservoir Properties on Pc

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DecreasingPermeability

A B

C

20

16

12

8

4

00 0.2 0.4 0.6 0.8 1.0

Water Saturation

Cap

illar

y Pr

essu

re

Effect of Permeability

***

Curves shift to the right (i.e., larger water saturations at a given value of capillary pressure) as the permeability decreases.Displacement pressure increases as permeability decreases.Minimum interstitial water saturation increases as permeability decreases.

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Well-sortedPoorly sorted

Cap

illar

y pr

essu

re, p

sia

Water saturation, %

Effect of Grain Size Distribution

Well-sorted grain sizesMajority of grain sizes are the same size. Minimum interstitial water saturation is lower.Displacement pressure is lower

Poorly sorted grain sizesSignificant variation in range of grain sizes. Minimum interstitial water saturation is higher.Displacement pressure is higher.

Page 53: Rock Properties

53

Water saturation, %

Cap

illar

y pr

essu

re, p

sia

Imbibition

Drainage

Effect of Saturation History

For the same saturation, capillary pressure is always higher for the drainage process (increasing the non-wetting phase saturation) than the imbibitionprocess (increasing the wetting phase saturation).

Page 54: Rock Properties

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Decreasing θR

θR = 30°

θR = 60°

θR = 0°

Cap

illar

y Pr

essu

reθR = 80°

20

16

12

8

4

00 0.2 0.4 0.6 0.8 1.0

Water Saturation

Effect of Contact Angle

Contact angle less than 90o indicates water-wet characteristics (refer to wettability notes).Curves shift to the right (i.e., larger water saturations at a given value of capillary pressure) as the contact angle decreases.Displacement pressure increases as contact angle decreases.Minimum interstitial water saturation increases as contact angle decreases.

Page 55: Rock Properties

55

Water Saturation

Hei

ght A

bove

Fre

e W

ater

Lev

el

High Tension

Low Tension

0 1.0

Effect of Interfacial Tension**

Low interfacial tension indicates higher tendency of phases to mix together.

With higher interfacial tension, transition zone is expected to be larger.

Page 56: Rock Properties

56

Water Saturation

Small Density Difference

LargeDensity

Difference

Hei

ght A

bove

Fre

e W

ater

Lev

el

0 1.0

Effect of Density Difference

Smaller density difference between fluids results in a larger transition zone (refer to Exercise 1).

Page 57: Rock Properties

Effective and Relative Permeabilities

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58

List 2 uses of relative permeability data

Define absolute permeability, effective permeability, and relative permeabilityList 3 parameters that affect relative permeabilityExplain hysteresis in two phase relative permeability data

Explain how the use of relative permeability curve is tied with the reservoir mechanism and/or the depletion process

List the common methods to measure two phase relative permeability

Instructional Objectives

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Reservoir simulation

Flow calculations that involve multi-phase flow in reservoirs

Estimation of residual oil (and/or gas) saturation

Uses of Relative Permeability

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Permeability is a property of the porous medium and is a measureof the capacity of the medium to transmit fluids

Permeability

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When the medium is completely saturated with one fluid, then the permeability measurement is often referred to as specific or absolute permeability

Absolute Permeability

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Absolute permeability is often calculated from the steady-state flow equation

LpAkq

µ∆

=

Calculating Absolute Permeability

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When the rock pore spaces contain more than one fluid, then the permeability to a particular fluid is called the effective permeability

Effective permeability is a measure of the fluid conductance capacity of a porous medium to a particular fluid when the medium is saturated with more than one fluid

Effective Permeability

Page 64: Rock Properties

64

Oil

Water

Gas

LpAkq

o

oeoo µ

∆=

LpAkq

w

weww µ

∆=

LpAk

qg

gegg µ

∆=

Calculating Effective Permeability

Page 65: Rock Properties

65

Relative permeability is defined as the ratio of the effective permeability to a fluid at a given saturation to a base permeability

The base permeability is commonly taken as the effective permeability to the fluid at 100% saturation (absolute permeability) or the effective non-wetting phase permeability at irreducible wetting phase saturation

Relative Permeability

Page 66: Rock Properties

66

Oil

Water

Gas

kkk eo

ro =

kkk ew

rw =

kk

k egrg =

Calculating Relative Permeability

Page 67: Rock Properties

67

Water phase

Water is located in smaller pore spaces and along sand grains

Therefore, relative permeability to water is a function of water saturation only (i.e., it does not matter what the relative amounts of oil and gas are)Thus, we can plot relative permeability to water against water saturation on Cartesian coordinate paper

Fundamental Concepts

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68

Oil phase

Oil is located between water and gas in the pore spaces, and to a certain extent, in the smaller pores

Thus, relative permeability to oil is a function of oil, water, and gas saturationsIf the water saturation can be considered constant (i.e., the minimum interstitial water saturation), then kro can be plotted against So on Cartesian coordinate paper

Fundamental Concepts

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69

Gas phase

Gas is located in the center of the larger pores

Therefore, the relative permeability to gas is a function of gassaturation only (i.e., it does not matter what the relative amounts of oil and water are)Thus ,we can plot krg against Sg (or Sw + So) on Cartesian coordinate paper

Fundamental Concepts

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70

Water-oil systemsOil-gas systemsWater-gas systemsThree phase systems (water, oil, and gas)

Common Multi-Phase Flow Systems

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71

What are the relative permeability data sets we need to use for the following situations?

Water flooding an oil reservoir above the bubble point

Production from an oil reservoir with a gas-cap and water aquifer

Exercise 2

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72

For water flooding an oil reservoir above the bubble point :Water-oil relative permeability

For three phase flow :Water-oil relative permeabilityGas-oil (or gas-liquid) relative permeability3 phase relative permeability

Exercise 2 – Solution**

Page 73: Rock Properties

73

40

0

20

400 1006020 80Water Saturation (%)

Rel

ativ

e Pe

rmea

bilit

y (%

)

100

60

80

Waterkrw @ Sor

Oil

Two-Phase FlowRegion

IrreducibleWater

Saturation

kro @ Swi

Residual OilSaturation

Oil – Water Relative Permeability

Page 74: Rock Properties

74

40

0

20

400 1006020 80Total Liquid Saturation - % of Pore Volume

Rel

ativ

e Pe

rmea

bilit

y (%

)

100

60

80

Gaskro

Oil

krg

SL = So + Swi

Oil – Gas Relative Permeability

Page 75: Rock Properties

75

Exercise 3

What do curves (1) and (2) represent?Estimate the following:

Irreducible water saturationResidual oil saturationRelative oil permeability at

irreducible water saturationRelative water permeability

at residual oil saturation

0.4

0

0.2

400 1006020 80

Water Saturation (% PV)

Rel

ativ

e Pe

rmea

bilit

y, F

ract

ion

1.0

0.6

0.8 (1)

(2)

The figure shows water-oil relative permeability data for a water-wet system.

Page 76: Rock Properties

76

Exercise 3 - Solution

Curve 1 represent KroCurve 2 represent Krw.

Swirr = 0.18Sorw = 0.20KroSwirr = Kro* = 1.0KrwSorw = Krw* = 0.32

0.4

0

0.2

400 1006020 80

Water Saturation (% PV)

Rel

ativ

e Pe

rmea

bilit

y, F

ract

ion

1.0

0.6

0.8 (1)

(2)

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77

Relative permeability data affect the flow characteristics of reservoir fluids.Relative permeability data affect the recovery of oil and/or gas.

Importance of Kr Data

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78

Exercise 4

The figure shown in the next slide presents two sets of water-oil relative permeability data. One set for rock type 1 is drawn with triangles, and another setfor rock type 2 is drawn with squares.

1. Explain why kro, is almost the same for the two sets, however, the water relative permeability, krw, is different?

2. State the impact of these two different sets of relative permeability data on oil recovery of a linear water flood?

Page 79: Rock Properties

79

0

20

40

60

80

100

0 20 40 60 80 100Water Saturation (%)

Rel

ativ

e Pe

rmea

bilit

y (%

) Rock Type 2Rock Type 1

Exercise 4

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80

Exercise 4 - Solution

In a water wet system:• Krw is more sensitive to grain size and grain size

distribution and sorting because water flows next to the walls of the pores,

• While Kro is not because oil flows at the middle of the pores.

**

Page 81: Rock Properties

81

0

20

40

60

80

100

0 2 4 6 8 10Pore Volumes Injected

Perc

ent o

f Rec

over

able

Oil

Rock Type 1Rock Type 2

Exercise 4 – Solution

than rock type 2 because of the shape of the Kr data.

Oil recovery for a process of water displacing oil can be 25 to 65% of the OOIP.

The recovery here is expressed in percentage of the recoverable oil, meaning that the Swirr has been excluded from the calculation.

Water flooding in rock type 1 is more efficient than rock type 2. In rock type 1, water breakthrough (water reaches the producer) occurs later in time

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82

Fluid saturations

Geometry of the rock pore spaces and grain size distribution

Rock wettability

Fluid saturation history (i.e., imbibition or drainage)

Factors Affecting Effective and Relative Permeabilities

Page 83: Rock Properties

83

0.4

0

0.2

400 1006020 80Water Saturation (% PV)

Rel

ativ

e Pe

rmea

bilit

y, F

ract

ion

1.0

0.6

0.8

Water

Oil

Strongly Water-Wet Rock

0.4

0

0.2

400 1006020 80Water Saturation (% PV)

Rel

ativ

e Pe

rmea

bilit

y, F

ract

ion

1.0

0.6

0.8

WaterOil

Strongly Oil-Wet Rock

Effect of Wettability on Kr Data***

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84

Types of relative permeability curvesDrainage curve

Wetting phase is displaced by the nonwetting phase, i.e., the wetting phase saturation is decreasing

Imbibition CurveNon-wetting phase is displaced by wetting phase, i.e., the wetting phase saturation is increasing

Effect of Saturation History

Page 85: Rock Properties

85

0

20

40

60

80

100

0 20 40 60 80 100

DrainageImbibition

Wetting Phase Saturation, % PV

Rel

ativ

e Pe

rmea

bilit

y, %

Residual non-wettingphase saturation

Interstitial wetting phase saturation

Effect of Saturation History**

Page 86: Rock Properties

86

When simulating the waterflood of a water-wet reservoir rock, imbibition relative permeability curves should be used. (Wetting phase saturation increasing)

When modeling gas injection into an oil reservoir, drainage relative permeability curves should be used. (Non-wetting phase saturation increasing)

Ref: Honarpour M, Koederitz L, Herbert A.: Relative Permeability of Petroleum Reservoirs

Choosing the Right Curve**