Each service company that offers pulsed neutron logs includes measurements based on the gamma rays from inelastic scattering. The gamma rays that originate from the high-energy neutrons that undergo inelastic scattering necessarily originate near the source. The number of these gamma rays that reach detectors relatively far from the source reflects the gamma ray scattering by and thus the density of the material between the scattered neutrons and the detector. Because there are many factors other than density that influence the number of gamma rays detected, service companies offer measurements based on inelastic scattering as empirical traces that are used in combination with measurements based on neutron scattering. Such combinations are useful primarily to recognize gas and distinguish gas from low porosity. One company offers a trace that represents density from the gamma rays due to inelastic scattering, but the process of deriving the density involves the very empirical step of subtracting different portions of the gamma rays attributed to factors other than inelastic scattering until a satisfactory approximation to density is achieved.
This paper presents a method for predicting the gamma rays from thermal neutrons to be subtracted from the total gamma rays measured during the neutron pulse and a comparison of the density-like trace so derived with open-hole density logs recorded in Cabinda, Angola, Africa.
The method presented for predicting gamma rays due to capture is based on representing the decay of gamma rays after the neutron burst by two exponential decays. The fraction of gamma rays due to thermal neutrons is different at different times during the pulse, but the overall effect is predicted from the amplitudes and decay times that fit the data used to represent sigma. While this removes variations in the fraction of capture gamma rays subtracted to create a density-like trace, the relationship between the amplitude of the trace and density is still determined empirically.
The comparison with open-hole logs makes use of the fact that many of the logs run were run to distinguish brine from oil through casing. This enables comparison of the densities derived from cased-hole logs to those recorded from open-hole logs under conditions where the open-hole logs still represent the reservoir. Some of the log data studied were from intervals where gas saturations changed between the open- and cased-hole logs, and these afford a chance to compare changes in density with changes in neutron porosities. Example comparison are presented and limitations discussed.