Neutron porosity based on one or more gamma ray detectors and a pulsed neutron source
A method for pulsed neutron well logging of a subsurface formation, includes irradiating the formation with a plurality of bursts of neutrons of a group of selected durations; detecting gamma rays resulting from interaction of the neutrons during a group of selected time gates which contains at least some early and late gamma ray counts. The gamma rays are detected at at least two axially spaced apart locations from a position of the irradiating. A weighted sum of the numbers of gamma rays detected in each of the time gates is calculated. A ratio of the weighted sum of detected gamma rays at a first axial spacing to the weighted sum at a second axial spacing is determined. The ratio is used to determine a hydrogen index of the subsurface formation.
1. A method for pulsed neutron well logging of a subsurface formation, comprising:
(a) irradiating the formation with a plurality of bursts of neutrons of a group of selected durations;
(b) detecting gamma rays resulting from interaction of the neutrons during a group of selected time gates which contains at least one early gamma ray count, comprising gamma rays detected between 0 and 70 microseconds from a neutron burst and at least one late gamma ray count consisting essentially of gamma rays detected between 70 and infinity microseconds from the neutron burst, the early and late gamma ray counts detected at at least two axially spaced apart locations from a position of the irradiating;
(c) in a computer, forming a weighted sum of the numbers of gamma rays detected in each of the time gates at each of the axially spaced apart locations;
(d) in the computer, determining a ratio of the weighted sum of detected gamma rays at a first axial spacing to the weighted sum at a second axial spacing; and
(e) in the computer, using the ratio to determine a hydrogen index of the subsurface formation, wherein the group of time gates, burst length, or number of bursts are optimized in a computer model to reduce the wellbore salinity effect on the ratio.
2. The method of claim 1 further comprising:
(f) repeating (a) and (b) for a selected number of times;
(g) in the computer, forming weighted sums of gamma rays detected in each of the time gates;
(h) in the computer, determining a ratio of the weighted-summed numbers of detected gamma rays at a first axial spacing to the weighted-summed numbers at a second axial spacing; and
(i) in the computer, using the ratio to determine a hydrogen index of the subsurface formation.
3. The method of claim 1 , in which the weights in the weighted sum are all equal.
4. The method of claim 1 , in which the group of selected time gates merges into a single time gate.
5. The method of claim 1 , in which at least one of the neutron burst lengths is shorter than 50 μs.
6. The method of claim 1 , in which the group of selected time gates is selected to be different for each detector before determining the ratio.
7. The method of claim 1 , in which weights used to compute the weighted sums are different for different detectors before determining the ratio.
8. The method of claim 1 , in which the early time gate may contains some inelastic gamma ray counts contamination, in which the total inelastic gamma ray counts are less than 5% of the total gamma ray counts in all the gates.