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Nuclear Magnetic Resonance (NMR) Logging BY MARIE WALKER

Nuclear magnetic resonance

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Page 1: Nuclear magnetic resonance

Nuclear Magnetic Resonance (NMR) Logging

BY MARIE WALKER

Page 2: Nuclear magnetic resonance

Outline

• Introduction• Principles of NMR• Interpretations of Raw Data• The NMR Log• NMR Tools• Advantages and Disadvantages of NMR Logging• Advances in NMR Logging• Future of NMR Logging• Summary

Page 3: Nuclear magnetic resonance

Introduction• Nuclear Magnetic Resonance (NMR) is the phenomenon

whereby a magnetic nuclei absorbs and emits energy in the presence of a magnetic field

• The first NMR Logging Tools were developed in the early 1960’s

• Plagued with problems so it was retired in the 1980’s • Re-emerged with the advent of pulsed tools• NMR allows for the calculation of:

Porosity Permeability Pore-space distributions Producible fluids and Irreducible Fluids Reservoir Quality Hydrocarbon Quality

Page 4: Nuclear magnetic resonance

Principles of NMR• All subatomic particles (neutrons, protons,

electrons) have the intrinsic property of spin• This spin corresponds to a small magnetic

moment• In the absence of a magnetic field the moments

are randomly aligned• When a static magnetic field, Bo is applied this

field acts as a turning force that aligns the nuclear spin axis of magnetic nuclei with the direction of the applied field

Page 5: Nuclear magnetic resonance

Principles of NMR con’t

• When a torque is applied to a spinning object, the axis of the object moves perpendicularly to the applied torque in motion called precession

• So the nucleus will precesses around Bo with a frequency called the Lamour frequency

• This proton can be in 2 energy states depending on the orientation of the axis

• The difference between the number of protons in each state gives the bulk magnetization which provides the signal measured by NMR devices

Page 6: Nuclear magnetic resonance

Principles of NMR con’t• The alignment of these protons is called polarization but

this does not happen immediately it grows with a time constant called longitudinal relaxation time T1

• After T1 an oscillating magnetic field is applied, sending

pulses of radio-frequency energy into the formation• The initial pulse is perpendicular to Bo and aligns the

spins in the transverse direction in phase with one another

• As the pulse dies, the magnetisation caused buy the precession decreases as the spins return out of phase and the signal seen in the receiver decays

• This very rapid decay is referred to as free induction decay (FID)

Page 7: Nuclear magnetic resonance

Spin-Echo Detection• To re-phase the protons a 180° pulse can be

applied• This pulse re-energizes the spins until a peak

magnetization signal is achieved called a spin echo.

• A series of these 180° pulses is sent into the formation at a fixed time interval called TE

• The spin echo signal decreases with each pulse. • This decay of the series called a CPMG series

(Carr-Purcell-Meiboom-Gill) is referred to as transverse relaxation time, T2

Page 8: Nuclear magnetic resonance

Interpretations of Raw Data• Total Porosity

Initial amplitude of the decay curve is a measure of the amount of polarized hydrogen in the pore fluid

• Pore size distribution T2 is smaller at surface area of grains than in pore

space therefore smaller T2 values mean smaller grain sizes

• Producible porosity and Bulk Volume Irreducible Assuming that producible fluids reside in large

pores and non-producible in small pores, T2 distribution curves can give the values for producible porosity of a formation

Page 9: Nuclear magnetic resonance

• Permeability Based on scientific models that show

permeability increases with porosity combined with core data

• Properties of Reservoir Fluids Based on T1 and T2 times which indicates pore

sizes. Clay-bound water, capillary-bound water, movable water, brine, hydrocarbons can all be differentiated based on various pore sizes

Coates Model:

Perm= [total porosity/C)2(producible porosity/Bulk irreducible volume)]2

Page 10: Nuclear magnetic resonance

Sandy Interval

The NMR Log

Page 11: Nuclear magnetic resonance

Magnetic Resonance Imaging (MRIL) Logging• Introduced by Numar in 1991• Composed of a permanent magnet and antennae • Magnet generates a static magnetic field • Antennae sends bursts of radio-frequency energy

into the formation in the form of an oscillating magnetic field

• Antennae acts as a receiver for decaying echo signal

Page 12: Nuclear magnetic resonance

Schlumberger Combinable Magnetic Resonance (CRM) tool

• Introduced by Schlumberger in 1995• Uses a bowstring to press against borehole • Antennae sandwiched between two permanent

magnets • Creates a sensitive zone of about 6 by 1 inches in

the formation• Used for high resolution data and high-precision

Page 13: Nuclear magnetic resonance

Advantages of NMR

• Only fluids are visible to NMR technology so porosity measurement is independent of the lithology

• Producible zones with high percentage of clay-bound water can be identified

• A better measurement of permeability is possible than traditional plots

• In-situ measurement of oil viscosity• Differentiation of oil/gas zones

Page 14: Nuclear magnetic resonance

Disadvantages of NMR Tools

• Any diamagnetic or paramagnetic ions present in the formation can affect the tool response

• Expensive• Slower logging speeds• Slimhole tools are not available• Shallow depth of penetration• Permeability measurement is actually an

empirical measurement and should only be used to compare to permeabilities

Page 15: Nuclear magnetic resonance

Advances in NMR• Schlumberger MRX eXpert

Contains multiple antennae that enable multiple depths-of-investigation over a broad range and it has a magnetic field gradient

Eliminates the need for multiple passes through zones of interest

Suitable for carbonate formations and low-resistivity pay zones

Page 16: Nuclear magnetic resonance

Advances in NMR• High- Resolution NMR- allows for the evaluation of

producibility of thinly laminated beds• Lithology Independent NMR Total Porosity- NMR is

the most accurate tool for measuring the porosity of heterogeneous formations

• Density/ Magnetic-Resonance Method- combines density and NMR log to predict gas-bearing formation total porosities

• Multi-dimensional NMR Fluid Characterization- composes 2D and 3D maps used to visually identify fluids present in the reservoir on the basis of contrasts in relaxation time

Page 17: Nuclear magnetic resonance

Future Research• Imaging reservoirs the same way MR is used to

image the human body• Inferring rock wettability from NMR • Pressure/Volume/Temperature properties of

reservoirs• Define rock/pore-space connectivity and structure

Page 18: Nuclear magnetic resonance

Summary

• NMR Logging uses the energy given off from hydrogen protons as they precess in a magnetic field to infer measurements of a formation’s porosity, permeability, pore space distribution, etc.

• Logs can be used to interpret zones of high porosity and producibility

• Main tools used are the Halliburton’s MRIL and Schlumberger’s CMR tool

• Gives lithology independent porosities but is more expensive than conventional tools

Page 19: Nuclear magnetic resonance

Questions?

Page 20: Nuclear magnetic resonance

Sources• Coates, G. R., Xiao, L. and Prammer, M. G. - NMR

Logging Principles and Applications• Darling, Toby-Well Logging and Formation

Evaluation• David Allen et al- Trends in NMR Logging• David Allen et al- How to Use Borehole Nuclear

Magnetic Resonance• Ellis, Darwin V. and Julian M. Singer- Well-Logging

for Earth Scientists• Freedman, Robert- Advances in NMR Logging