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Neutron Log

Neutron Log
Neutron Log

Theory Behind Neutron Logging

In neutron logging, three processes are essential:

  1. Neutron Emission:

    • Neutron tools emit high-energy (4.5 MeV) neutrons from a radioactive source comprising an alpha emitter (e.g., radium, plutonium, or americium) and beryllium-9.
    • Alpha particles interact with beryllium-9, producing carbon-12, fast neutrons, and gamma rays.
  2. Neutron Scattering:

    • Fast neutrons undergo elastic scattering with atomic nuclei, losing energy and slowing down.
    • Energy loss is most efficient when colliding with nuclei of similar mass, notably hydrogen.
    • Neutrons slow from fast (>0.5 MeV) to thermal energies (

    Energy loss per collision depends on the target nucleus's relative mass and the scattering cross section.

    Efficiency of hydrogen, silicon, and oxygen atoms in slowing down fast neutrons in a clean sandstone (φ = 0.15).

  3. Neutron Absorption:

    • Thermal and epithermal neutrons are absorbed by formation nuclei.
    • Hydrogen and chlorine are significant neutron absorbers in formations.
    • Neutron absorption leads to gamma-ray emission, detectable by some neutron logging tools.


Neutron Logs and Their Main Applications

Neutron logs are primarily used for:

  • Porosity Determination: Often combined with the density tool.
  • Gas Detection: In conjunction with density or sonic tools.
  • Shale Volume Estimation: Alongside the density tool.
  • Lithology Indication: Using both neutron and density or sonic logs.
  • Formation Fluid Typing
  • Applicable in Open and Cased Hole Logging

The amount of energy lost at each collision depends on the relative mass of the target nucleus and the scattering cross section.

Note: Hydrogen plays a crucial role in slowing down neutrons due to its similar size, causing significant energy loss during collisions.


Types of Neutron Logging Tools

There are three main types of neutron tools:

  1. Gamma Ray/Neutron Tool (GNT):

    • Equipped with a neutron source and a single detector sensitive to high-energy capture gamma rays and thermal neutrons.
    • Can be run in both open and cased holes, typically centered.
    • Tool diameters: 3-3/8 inches for open holes; 1-11/16 or 2 inches for cased holes.
    • Source-to-detector spacing ranges from 15.5 to 19.5 inches, depending on the manufacturer.
  2. Sidewall Neutron Porosity Tool (SNP):

    • Designed exclusively for open holes.
    • Features a source and a single detector with a 16-inch spacing.
    • Mounted on a skid pressed against the borehole wall to reduce mud and mudcake effects.
    • Detector sensitive to epithermal neutrons, unaffected by chlorine in high-salinity muds and formation fluids.
  3. Compensated Neutron Log (CNL):

    • Sensitive to thermal neutrons with two detectors at 15 and 25 inches from the source; affected by the chlorine effect.
    • Run eccentered in the hole using an arm to press against the borehole wall, minimizing mud type influence.

Factors Affecting Neutron Logs

  1. Chlorine Effect:
    • Thermal neutron tools measure neutrons and gamma rays from neutron capture.
    • Hydrogen and chlorine significantly contribute to neutron absorption.
    • High chloride content in drilling mud or formation fluids reduces the detected neutron flux, leading to overestimated porosity.
  2. Shale Effect:
    • Shales contain clays with bound water, increasing hydrogen content despite low porosity.
    • Neutron logs in shales read higher apparent porosity than actual.
  3. Gas Effect:
    • Gas-filled porosity lowers the hydrogen density.
    • Neutron tools interpret gas zones as lower hydrogen content, resulting in abnormally low porosity readings in gas-bearing formations.

Accelerator Porosity Sonde

This tool combines responses from multiple detectors to compensate for lithology and matrix density effects:

  1. Near-to-Far Measurement:
    • Exhibits greater sensitivity to shale and gas effects.
    • Provides a response similar to conventional compensated neutron tools.
  2. Near-to-Array Measurement:
    • Used to determine formation porosity.
    • Offers a vertical resolution of 1 foot.
  3. Epithermal Array Detectors:
    • Monitor and correct for tool standoff effects.
  4. Thermal Detector:
    • Determines porosity by detecting neutrons rather than gamma rays, unlike conventional pulsed neutron tools.