Identification of neutron capture from a pulsed neutron logging tool
The present disclosure is intended to overcome the problem of hydrogen contamination of the density signal. The approach is to compute the neutron capture portion of the total gamma ray counts and subtract it from the total counts resulting in a pure inelastic gamma ray measurement.
1. A method, comprising:
disposing a logging tool in a borehole in a formation, the logging tool comprising a pulsed neutron source, and a gamma-ray detector configured to detect counts of inelastic gamma-rays that form when neutrons are inelastically scattered by the formation;
emitting a burst of neutrons into the formation with the pulsed neutron source;
determining an epithermal neutron capture count for the burst, and
determining stand-off of the logging tool based on a slowing-down-time of the epithermal neutron capture count.
2. The method according to claim 1 , further comprising subtracting the epithermal neutron capture count from a total count rate to determine a pure inelastic gamma-ray signal relating to density of the formation.
3. The method according to claim 1 , further comprising computing a hydrogen index measurement based on the epithermal neutron capture count.
4. The method according to claim 1 , further comprising computing a neutron porosity measurement based on the epithermal neutron capture count.
5. The method according to claim 1 , wherein the neutrons emitted have an energy level of at least 2 MeV.
6. The method according to claim 1 , wherein disposing the logging tool in the borehole comprises conveying the logging tool on a wireline, a slickline, coiled tubing, or a drillstring in logging-while-drilling operations.
7. The method according to claim 1 , wherein determining the epithermal neutron capture count for the burst is based on a rate of thermal creation for the burst.
8. The method according to claim 1 , wherein determining the epithermal neutron capture count for the burst further comprises fitting a sum of exponentials with a plurality of amplitudes and decay times for an “off” interval following the burst to construct the epithermal neutron capture for the burst.
9. The method according to claim 1 , wherein determining the epithermal neutron capture count for the burst further comprises fitting a square pulse for an “on” interval for the burst and a first exponential build-up function relating to an epithermal neutron capture component of a total count rate and a second exponential build-up function relating to a thermal neutron capture component of the total count rate.
10. The method according to claim 1 , wherein determining the epithermal neutron capture count for the burst is based on a total thermal count rate.
11. The method according to claim 1 , wherein determining the epithermal neutron capture count for the burst further comprises fitting predetermined spectra for each element of the formation that will contribute inelastic gamma-rays to a spectra obtained during the burst and subtracting out the spectra contributed by each element of the formation to result in a fraction of the spectra obtained during the burst that is due to epithermal capture.
12. A method, comprising:
disposing a logging tool in a borehole in a formation, the logging tool comprising a pulsed neutron source, and a gamma-ray detector configured to detect counts of inelastic gamma-rays that form when neutrons are inelastically scattered by the formation;
emitting a burst of neutrons into the formation with the pulsed neutron source; and
determining an epithermal neutron capture count for the burst based on a rate of thermal creation for the burst or a total thermal count rate.
13. The method according to claim 12 , further comprising subtracting the epithermal neutron capture count from a total count rate to determine a pure inelastic gamma-ray signal relating to density of the formation.
14. The method according to claim 12 , further comprising determining stand-off of the logging tool based on a slowing-down-time of the epithermal neutron capture count.
15. The method according to claim 12 , further comprising computing a hydrogen index measurement and/or a neutron porosity measurement based on the epithermal neutron capture count.
16. A method, comprising:
disposing a logging tool in a borehole in a formation, the logging tool comprising a pulsed neutron source, and a gamma-ray detector configured to detect counts of inelastic gamma-rays that form when neutrons are inelastically scattered by the formation;
emitting a burst of neutrons into the formation with the pulsed neutron source; and
determining an epithermal neutron capture count for the burst by one or more of:
fitting a sum of exponentials with a plurality of amplitudes and decay times for an “off” interval following the burst to construct the epithermal neutron capture for the burst;
fitting a square pulse for an “on” interval for the burst and a first exponential build-up function relating to an epithermal neutron capture component of a total count rate and a second exponential build-up function relating to a thermal neutron capture component of the total count rate; and
fitting predetermined spectra for each element of the formation that will contribute inelastic gamma-rays to a spectra obtained during the burst and subtracting out the spectra contributed by each element of the formation to result in a fraction of the spectra obtained during the burst that is due to epithermal capture.
17. The method according to claim 16 , further comprising subtracting the epithermal neutron capture count from a total count rate to determine a pure inelastic gamma-ray signal relating to density of the formation.
18. The method according to claim 16 , further comprising determining stand-off of the logging tool based on a slowing-down-time of the epithermal neutron capture count.
19. The method according to claim 16 , further comprising computing a hydrogen index measurement and/or a neutron porosity measurement based on the epithermal neutron capture count.