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Theory
• Emitted neutrons interact with matter by:
Elastic scattering
• Elastic collisions involving some loss of energy (small nucleus) and no
loss of energy(heavy nucleus)
Theory
• Emitted neutrons interact with matter by:
Inelastic scattering
• Inelastic scattering where target nucleus absorbs fast neutronsand
emits a slower neutron and gamma rays
Effect of target size on energy loss
• Energy lost by collisions is dependent on mass difference
• Hydrogen approximately same mass as neutron, thus highest loss of
energy (67%) per collision
• The heavier the nucleus, the less energy lost
Hydrogen content
– Water, oil HI = 1.0
– gas HI = 0.5 - 0.75
– shale HI = 0.17 - 0.42
– clean rock HI = 0.0
Principle of Operation
• Neutrons emitted from radioactive source
• Collide and lose energy (Billiard ball effect)
• Primarily dependent on hydrogen concentration or
index
• Detect either epithermal neutrons, thermal
neutrons, capture gamma rays or combination
• Thus, measures the formations ability to attenuate
the passage of neutrons
Types
• Two types of neutron logs are commonly used
1. Single Neutron Pad log (SNP)
2. Compensated Neutron Log (CNL)
Sidewall Neutron Porosity log (SNP)
• Tools:
Pad-type single detector.
• Detects:
Epithermal neutrons.
• Depth interval:
Shallow, 8”
Compensated Neutron Log (CNL)
• Tool:
Mandrel-type 2 detectors.
• Detects:
Thermal Neutrons
• Depth interval:
Deeper, 12”
Compensated Neutron Log (CNL)
Neutron log
Uses
1. Determination of porosity / Lithology.
2. Delineation of porous formations.
3. CNL can be used in cased hole
• Unit:
Neutron log is measured in count/minute
• Limitations:
1. In shale there is weak hydrogen bonding, so neutrons are captured
by hydrogen and loss of neutron occurred. This limitation are
overcome by knowledge of seismic log.
2. In case of gas in reservoir rock the gas molecules are too far from
one another so neutron are not lost shows low porosity then the
actual porosity. This limitation is overcome by the density log
identify the presence of gas.
3. In case of gypsum (CaSO4 .2H2O), water molecule are present in
gypsum. So neutron is captured by hydrogen show shows more
neutron log value but there is no fluid in the formation.
THANKS

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Neutron log

  • 1.
  • 2. Theory • Emitted neutrons interact with matter by: Elastic scattering • Elastic collisions involving some loss of energy (small nucleus) and no loss of energy(heavy nucleus)
  • 3. Theory • Emitted neutrons interact with matter by: Inelastic scattering • Inelastic scattering where target nucleus absorbs fast neutronsand emits a slower neutron and gamma rays
  • 4. Effect of target size on energy loss • Energy lost by collisions is dependent on mass difference • Hydrogen approximately same mass as neutron, thus highest loss of energy (67%) per collision • The heavier the nucleus, the less energy lost Hydrogen content – Water, oil HI = 1.0 – gas HI = 0.5 - 0.75 – shale HI = 0.17 - 0.42 – clean rock HI = 0.0
  • 5. Principle of Operation • Neutrons emitted from radioactive source • Collide and lose energy (Billiard ball effect) • Primarily dependent on hydrogen concentration or index • Detect either epithermal neutrons, thermal neutrons, capture gamma rays or combination • Thus, measures the formations ability to attenuate the passage of neutrons
  • 6. Types • Two types of neutron logs are commonly used 1. Single Neutron Pad log (SNP) 2. Compensated Neutron Log (CNL)
  • 7. Sidewall Neutron Porosity log (SNP) • Tools: Pad-type single detector. • Detects: Epithermal neutrons. • Depth interval: Shallow, 8”
  • 8. Compensated Neutron Log (CNL) • Tool: Mandrel-type 2 detectors. • Detects: Thermal Neutrons • Depth interval: Deeper, 12”
  • 11. Uses 1. Determination of porosity / Lithology. 2. Delineation of porous formations. 3. CNL can be used in cased hole
  • 12. • Unit: Neutron log is measured in count/minute • Limitations: 1. In shale there is weak hydrogen bonding, so neutrons are captured by hydrogen and loss of neutron occurred. This limitation are overcome by knowledge of seismic log. 2. In case of gas in reservoir rock the gas molecules are too far from one another so neutron are not lost shows low porosity then the actual porosity. This limitation is overcome by the density log identify the presence of gas. 3. In case of gypsum (CaSO4 .2H2O), water molecule are present in gypsum. So neutron is captured by hydrogen show shows more neutron log value but there is no fluid in the formation.