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BY MARIE WALKER
•   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
• 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
• 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
• 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
• 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)
• 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
• 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
• Permeability
    Based on scientific models that show permeability
      increases with porosity combined with core data
• PropertiesCoates Model:
             of Reservoir Fluids
    Based on T1 and T2 times which indicates pore
      sizes. Clay-bound water, capillary-bound
      water,Perm= [total brine, hydrocarbons can all be
              movable water,
      differentiated based 2(producible sizes
             porosity/C) on various pore
           porosity/Bulk irreducible
           volume)]2
The NMR Log




Sandy
Interval
• 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
• 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
• 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
• 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
• 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
• 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
• 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
• 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
• 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

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NMR Logging Reveals Reservoir Properties

  • 2. 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
  • 3. • 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
  • 4. • 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
  • 5. • 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
  • 6. • 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)
  • 7. • 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
  • 8. • 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
  • 9. • Permeability  Based on scientific models that show permeability increases with porosity combined with core data • PropertiesCoates Model: of Reservoir Fluids  Based on T1 and T2 times which indicates pore sizes. Clay-bound water, capillary-bound water,Perm= [total brine, hydrocarbons can all be movable water, differentiated based 2(producible sizes porosity/C) on various pore porosity/Bulk irreducible volume)]2
  • 11. • 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
  • 12. • 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
  • 13. • 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
  • 14. • 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
  • 15. • 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
  • 16. • 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
  • 17. • 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
  • 18. • 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
  • 19.
  • 20. • 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

Editor's Notes

  1. Source: advances in NMR Logging, Robert Freedman