Nuclear Logging Tools and Applications Thereof

Abstract

A nuclear logging tool has a housing, one or more neutron sources, one or more shields, and two or more detectors disposed about the housing. Each of the one or more neutron sources is configured to generate neutrons in pulses or continuously and each of the two or more detectors is operable to detect neutrons and gamma rays. The two or more detectors include a first detector disposed at a first distance from a first neutron source and a second detector disposed at a second distance from the first neutron source. The first distance is shorter than the second distance. The first distance and the second distance is measured in the longitudinal direction of the housing. Each shield is operable to absorb neutrons and gamma rays and is disposed inside the housing between one of the one or more neutron source and one of the one or more detectors.

Claims

1. A nuclear logging tool, comprising: a housing, one or more neutron sources, one or more shields, and two or more detectors disposed about the housing, wherein each of the one or more neutron sources is configured to generate neutrons in pulses or continuously and each of the two or more detectors is operable to detect neutrons and gamma rays, wherein the two or more detectors include a first detector disposed at a first distance from a first neutron source and a second detector disposed at a second distance from the first neutron source, wherein the first distance is shorter than the second distance, wherein each of the first distance and the second distance is in a longitudinal direction of the housing, and wherein each shield is operable to absorb neutrons and gamma rays and is disposed inside the housing between one of the one or more neutron source and one of the one or more detectors.

2. The nuclear logging tool of claim 1, wherein each of the one or more neutron sources is independently a Deuterium-Tritium (D-T) neutron generator, a Deuterium-Deuterium (D-D) neutron generator, or a radioisotope neutron source.

3. The nuclear logging tool of claim 1, further comprises a third detector disposed at a third distance from the first neutron source in the longitudinal direction of the housing, and the third distance is larger than the second distance.

4. The nuclear logging tool of claim 1, wherein each of the two or more detectors comprises a scintillator made of Cs.sub.2LiYCl.sub.6 or Cs.sub.2LiLaBr.sub.6.

5. The nuclear logging tool of claim 1, further comprising a second neutron source disposed about the housing, wherein the second neutron source is spaced away from the first neutron source in the longitudinal direction of the housing.

6. The nuclear logging tool of claim 5, wherein the two or more detectors are disposed between the first neutron source and the second neutron source.

7. The nuclear logging tool of claim 1, further comprising two or more detectors disposed at substantially the first distance from the first detector or at substantially the second distance from the second detector.

8. The nuclear logging tool of claim 1, wherein the one or more neutron sources include an isotope neutron source and a pulsed neutron generator.

9. The nuclear logging tool of claim 1, wherein at least two of the two or more detectors are installed at different radial directions about the housing and have different toolface angles when the nuclear logging tool is deployed in a subterranean formation.

10. The nuclear logging tool of claim 9, wherein at least one of the two or more detectors is located on an axis or off the axis of the logging tool.

11. The nuclear logging tool of claim 1, wherein the shield is made of a material selected from gadolinium (Gd), samarium (Sm), tungsten borides, an alloy containing Gd, an alloy containing Sm, Gd.sub.2O.sub.3, Sm.sub.2O.sub.3, B.sub.2O.sub.3, and mixtures thereof.

12. The nuclear logging tool of claim 11, wherein a portion of a casing of at least one among the two or more detectors is made of the shield material.

13. A method for measuring subterranean formation properties, comprising: deploying the nuclear logging tool of claim 1 into a subterranean formation; causing the one or more neutron sources to emit neutrons into the subterranean formation; converting neutrons and gamma rays from the subterranean formation received by the two or more detectors to electric signals; and analyzing electric signals to obtain a plurality of formation properties.

14. The method of claim 13, wherein the nuclear logging tool comprises a second neutron source disposed about the housing, wherein the second neutron source is spaced away from the first neutron source in the longitudinal direction of the housing, and wherein the one or more detectors are disposed between the first neutron source and the second neutron source.

15. The method of claim 13, wherein the plurality of formation properties include formation density, formation porosity, gas and oil saturation, and/or formation element concentration.

16. A downhole drilling system, comprising: a drill string having a bottom hole assembly (BHA) disposed at a lower part thereof; a kelly drive configured to deliver the drill string into a borehole; a top drive configured to rotate the drill string; and a controller, wherein the BHA comprises a drill bit disposed at an end portion of the BHA, a downhole motor, and a measurement sub configured to measure subterranean formation properties and operational parameters, wherein the measurement sub comprises the nuclear logging tool of claim 1.

17. The drilling system of claim 16, wherein the nuclear logging tool comprises a second neutron source disposed about the housing, wherein the second neutron source is spaced away from the first neutron source in the longitudinal direction of the housing, and wherein the one or more detectors are disposed between the first neutron source and the second neutron source.

18. The drilling system of claim 16, wherein each of the one or more neutron sources in the nuclear logging tool is independently a Deuterium-Tritium (D-T) neutron generator, a Deuterium-Deuterium (D-D) neutron generator, or a radioisotope neutron source.

19. A wireline logging tool, comprising the nuclear logging tool of claim 1 connected to an electric cable.

20. The wireline logging tool of claim 19, the nuclear logging tool comprises a second neutron source disposed about the housing, wherein the second neutron source is spaced away from the first neutron source in the longitudinal direction of the housing, and wherein the one or more detectors are disposed between the first neutron source and the second neutron source.

Description

BRIEF DESCRIPTION OF THE DRAWINGS

[0030] The teachings of the present invention can be readily understood by considering the following detailed description in conjunction with the accompanying drawings.

[0031] FIG. 1A, FIG. 1B, FIG. 1C, and FIG. 1D illustrate four exemplary configurations of a nuclear logging tool having one neutron source (S1) and three detectors (D1, D2, and D3) disposed along the longitudinal direction of the housing of the tool.

[0032] FIG. 2A, FIG. 2B, and FIG. 2C show cross-sectional views of exemplary nuclear logging tools having S1, D1, D2, and D3.

[0033] FIG. 3A and FIG. 3B show cross-sectional views of exemplary nuclear logging tools having four and five detectors, respectively.

[0034] FIG. 4A is an embodiment of the nuclear logging tool having two neutron sources (S1, S2) and two detectors (D1, D2); FIG. 4B and FIG. 4C provide cross-sectional views of exemplary configurations of this embodiment.

[0035] FIG. 5A is a further exemplary embodiment of the nuclear logging tool having two neutron sources (S1, S2) and four detectors (D11, D12, D21, D22); FIG. 5B provides cross-sectional views of this embodiment.

[0036] FIG. 6 is a block diagram of an exemplary drilling system that implements an embodiment of the current disclosure.

[0037] FIG. 7 shows schematics of neutron pulses, neutron count rates, as well as inelastic spectrum and capture spectrum of neutron-induced gamma rays.

[0038] FIG. 8 is a flow diagram showing exemplary methods to obtain various formation parameters.

[0039] Throughout the drawings and the detailed description, unless otherwise described, the same drawing reference numerals will be understood to refer to the same elements, features, and structures. The relative size and depiction of these elements may be exaggerated for clarity, illustration, and convenience.

DETAILED DESCRIPTION

[0040] The following detailed description is provided to assist the reader in gaining a comprehensive understanding of the methods, apparatuses, and/or systems described herein. References are made in detail to embodiments of the present disclosure, examples of which are illustrated in the accompanying drawings. Similar or like reference numbers may be used in the drawings and may indicate similar or like elements.

[0041] The features described herein may be embodied in different forms and are not to be construed as being limited to the embodiments described herein. Rather, the embodiments described herein and depicted in the drawings have been provided so that this disclosure will be thorough and complete and will convey the full scope of the disclosure to one of ordinary skill in the art, who may readily recognize from the following description that alternative embodiments exist without departing from the general principles of the disclosure.

[0042] Therefore, the scope of the disclosure is defined not by the detailed description, but by the claims and their equivalents, and all variations within the scope of the claims and their equivalents are to be construed as being included in the disclosure.

[0043] In this disclosure, unless otherwise noted, a detector in refers to a dual-function detector that can detect both neutrons and gamma rays. Such a detector employs scintillation crystals such as Cs.sub.2LiYCl.sub.6 (CLYC) or Cs.sub.2LiLaBr.sub.6 (CLLB) and associated electronics, e.g., PMT. The detectors may be actively cooled or not actively cooled when deployed downhole. For example, a detector using CLLB and high-temperature PMT can be used at a high temperature without additional cooling.

[0044] FIGS. 1A to 1D are schematic illustrations (not to scale) of four exemplary configurations of a cylindrical nuclear logging tool 200 having a neutron source (S1) and three dual-function detectors (D1, D2, D3) disposed along the housing of the logging tool suitable for logging-while-drilling (LWD) operations. A mud channel (MC) is disposed along the axis of the logging tool while the detectors are eccentrically disposed along the longitudinal direction of the tool. FIG. 1 A also shows a high voltage power supply (HV), an electronic instrument, e.g., a controller, for sending instructions, receiving and processing data from the neutron source and the detectors, as well as a telemetry for transmitting data between the logging tool and surface. The high voltage power supply provides power to detectors (D1, D2, D3) and to the pulsed neutron source (S1). The power supply, the electronic instrument, and telemetry are required but not shown in FIGS. 1B-1D for simplicity.

[0045] As shown in the figures, D1 is the near detector that has the shortest distance in longitudinal direction to the neutron source, D3 is the far detector having the longest longitudinal distance to the neutron source, and D2 is the middle detector that has a longitudinal distance that is in the middle.

[0046] In FIG. 1A, all three detectors reside on one side of the neutron source along the logging tool 200. The one side can be either the proximal side or the distal side of the neutron source. The proximal side is the side of the nuclear logging tool 200 that is closer to the surface when it is deployed downhole while the distal side is farther away from the surface. The high voltage power supply provides power to detectors (D1, D2, D3) and to the pulsed neutron source (S1). The signals from detectors are processed by the electronic instruments and measurements/data are collected and transmitted by telemetry. In FIGS. 1B, 1C, and 1D, both the distal side and the proximal side of the neutron source has at least one detector disposed thereto.

[0047] In wireline logging, the tool can be installed in a sonde, which does not contain a mud channel. Detectors can be installed either along or off the axis of the tool body. Power and control signals can also be provided to the logging tool from the surface while data from the logging tool can be transmitted to the surface via the wireline cable.

[0048] The neutron source S1 in each logging tool depicted in FIGS. 1A to 1D is a pulsed neutron generator. However, an isotope neutron source can be used as well. The pulsed neutron source may be a Deuterium-Tritium (D-T) pulsed neutron generator, which can be operated in a variety of pulse schematics (e.g., frequency, duty time) in a pulse mode. For example, the frequency of neutron pulses may be about 10 kHz (the period is 100 μs) and the neutron duty time may be about 20 μs. In another embodiment, the frequency of neutron pulses may be about 1 kHz (the period is 1000 μs) and neutron duty time may be 50 μs. Depending on the methods and measurements, the D-T neutron generator may also be operated in a continuous mode. In that case, the neutron generator is activated frequent enough so that neutrons are emitted continuously. Neutrons from a D-T neutron generator has an initial energy of about 14.1 MeV.

[0049] The pulsed neutron source may also be a Deuterium-Deuterium (D-D) pulsed neutron generator, which can be operated in different pulse schematics (e.g., frequency, duty time) in pulsed mode. For example, the frequency of neutron pulses may be about 20 kHz (the period is 50 μs) and neutron duty time may be about 20 μs. Alternatively, the frequency of neutron pulses may be about 1 kHz (the period is 1000 μs) and neutron duty time may be 40 μs. Depending on the methods and measurements, the D-D neutron generator may also be operated in a continuous mode. Neutrons from a D-D neutron generator has an initial energy of about 2.5 MeV.

[0050] An isotope neutron source, such as Am—Be, Pu—Be, Cf-252, may also be used in the place of the pulsed neutron source, depending on the target formation parameters and measurement methods. Neutrons from these isotope neutron sources have different energy spectra. For an example, the energy of neutrons emitted from an Am—Be source is from 0 MeV to about 10 MeV with an average energy of about 4.2 MeV.

[0051] The neutron source S1 and detectors D1, D2, and D3 as depicted in FIGS. 1A-1D only show their relative positions along the longitudinal direction of the housing of the tool 200 but not their positions in the radial direction in a cross-section of the tool housing.

[0052] In certain embodiments, S1, D1, D2, and D3 can be disposed at the same radial or different directions, i.e., having the same or different toolface angles when deployed in the formation. FIGS. 2A, 2B, and 2C show exemplary cross-sectional views in the directions of A-A, B-B, C-C, and D-D as shown in FIGS. 1A to 1D. S1, D1, D2, and D3 in FIG. 2A are disposed at same toolface angle. In FIG. 2B, however, S1, D1, and D3 have the same toolface angle while D2 is at a different toolface angle. In FIG. 2C, S1 and D1 have the same toolface angle while each of D2 and D3 has a different toolface angle.

[0053] Other embodiments of the logging tool may have more than three detectors. For example, FIG. 3A depicts a variation of the logging tool in FIG. 1A that has four detectors—D1, D2, D31, and D32. D31 and D32 have approximately the same distance from S1 but are disposed at two different toolface angles. Likewise, FIG. 3B depicts another variation of tool in FIG. 1A, which has six detectors—D1, D21, D22, D31, D32, and D33. In this embodiment, D21 and D22 are disposed opposite to each other on the cross-sectional area of the logging tool, i.e., the toolface angle of D21 and D22 is 0° and 180°, respectively. D31, D32, and D33 are disposed 120° apart on the cross-sectional area of the logging tool, i.e., a difference in the toolface angles of any two among D31, D32, and D33 is 120°. Having different toolface angles allows detectors to preferentially receive neutrons and gamma-rays at certain incident angles from the formation. It also increases the detection efficiency of neutrons and gamma rays by increasing the total count rate of all the detectors.

[0054] Further, in FIG. 3A, D31 and D32 in have substantially the same distance from S1. In FIG. 3B, middle detectors D21 and D22 have substantially the same distance from S1 while far detectors D31, D32, and D33 have substantially the same distance from S1. “Substantially the same distance” means the distances from S1 to the center of scintillators of the detectors (e.g., D31 and D32) is about the same. For example, the difference is less than ½″ or ¼″. By this arrangement, the middle detectors as a whole and far detectors as a whole have higher count rates than when one only middle detector or only one far detector is used. Accordingly, the neutron generator S1 can be of a less powerful source, which may not be subject to stringent regulations as more powerful neutron sources are subject to. In addition, the count rate of individual detectors can separately be recorded and processed. The differences of various detectors in distance and in toolface angles can be used to obtain formation information in specific azimuthal directions.

[0055] In some embodiments, the logging tool 200 have multiple shields that can absorb neutrons and gamma-rays (not shown). The shields can be placed in the logging tool between the neutron source and the detectors so that the detectors receive neutrons and gamma-rays coming from the formation rather than traveling through the logging tool itself. Alternatively, the detectors can also be partially shielded by the shield material that absorb neutrons and gamma rays from certain directions.

[0056] The shield is made of or contains one or more materials that can effectively attenuate both thermal neutrons and gamma rays. The shield material can contain materials chosen from heavy elements having high thermal neutron absorption cross sections, including metals such as gadolinium (Gd), samarium (Sm), metal oxides such as Gd.sub.2O.sub.3, Sm.sub.2O.sub.3, B.sub.2O.sub.3, alloys containing Gd or Sm with other heavy metals Fe, Pb, or W, or materials containing boron, such as tungsten borides (WB, WB.sub.2, etc.).

[0057] The shield may be a stand-alone metal piece inserted in the logging tool, or an integral part of the detector casing. For example, the portion of the detector casing facing inward to the logging tool can be made of the shield material while the portion facing the formation is made of a material that is transparent to neutrons and gamma rays, forming a window that neutrons and gamma rays can travel through. As such, neutrons and gamma-rays from certain incident angles may be absorbed by the shield material while those travel through the window are received by the detector. Therefore, the detector can be more sensitive to certain incident angles by adjusting the size and orientation of the window in the detector casing. During operation, data collected by various detectors may produce direction-specific formation properties, which can be used to guide directional drilling.

[0058] The nuclear logging tool may have more than one neutron sources. FIG. 4A shows a further embodiment of the logging tool having two neutron sources (S1 and S2), one at the proximal end and the other at the distal end while two detectors (D1 and D2) are arranged between S1 and S2. Alternatively, S1 and S2 can be arranged in tandem and disposed near one end of the logging tool while D1 and D2 arranged in tandem near the other end, as the engineering considerations require. In both embodiments, the distance between S1 and D1 is d.sub.1, the distance between S1 and D2 is d.sub.2, the distance between S2 and D2 is d.sub.3, while the distance between S2 to D1 is d.sub.4. When S1 and S2 are both pulsed neutron generators, they can be alternately turned ON or OFF, thereby inducing neutrons and gamma-rays from the formation alternately, which are received by D1 and D2. Since there are four different source-to-detector distances (d.sub.1 to d.sub.4), the data generated in D1 and D2 may be better compensated than tools with only two or three source-to-detector distances for near wellbore effects, such as borehole size, tool standoff, mud weight and/or salinity, casing size, cement thickness, etc. As a result, the obtained formation parameters could be more accurate.

[0059] FIG. 4B and FIG. 4C illustrate two exemplary embodiments of this design, where the two sources and two detectors can be arranged in same toolface angle or in different toolface angles. When, as in FIG. 4B, the sources and detectors have the same toolface angle, the measurement covers the same sector in the formation at any given time. When, as in FIG. 4A, the sources and detectors may have different toolface angles, the data generated in D1 and D2 reflect different sectors of the formation, which can reveal differences amongst various formation sectors at any given time by comparing the measurements from D1 and D2.

[0060] FIGS. 5A and 5B illustrate a logging tool that has four detectors (D11, D12, D21, D22) and two neutron sources (S1 and S2). Note that the pair of detectors D11 and D12 (as well as D21 and D22) are disposed at substantially the same distance from S1 or S2. As indicated before, having more than one detectors at a certain distance increase the count rate at that distance so that a less powerful neutron source may be viable. The count rate of one far detector may be too low to provide reliable measurement data. By using two or more far detectors, the count rate can be significantly increased so that reliable measurement results can be obtained by processing data from the multiple far detectors as a whole.

[0061] In some embodiments, S1 and S2 can be turned ON or OFF simultaneously. Doing so increases the count rate of D1 and D2, thereby reducing the statistical measurement uncertainty.

[0062] In still another embodiment, S1 and S2 are both isotope neutron sources. Compared with pulsed neutron sources, isotope neutron sources do not need power supply so that the logging tool can be more compact. Moreover, the isotope neutron source has a longer lifetime and is more reliable. For example, the half-life of an isotope Am—Be neutron source has a half-life of 432 years, much longer than the average tube lifetime of a neutron generator of 500 hours to 4000 hours.

[0063] In yet another embodiments, Si and S2 can be two different types of neutron sources. For example, Si can be a D-T neutron generator while S2 can be an Am—Be neutron source. In the field, the D-T neutron generator can be turned off, leaving the Am—Be neutron source working by itself to perform the neutron porosity log. Alternatively, the Am—Be neutron source can be taken out from the logging tool so that the D-T neutron generator alone emits neutron pulses into the surrounding formation. In this case, one may obtain the neutron porosity log as well as other measurements (density, oil and gas saturation, etc.) using the D-T neutron generator.

[0064] The porosity logs obtained using the Am—Be source and the D-T source differ slightly. By comparing these porosity logs of the same well obtained using two different neutron sources, one may obtain the correlation between these two logs. As historical porosity logs were mainly obtained using isotope neutron sources, such correlations may help updating the historical porosity logs so that they become comparable with new logs obtained using pulsed neutron sources. Likewise, the new pulsed neutron porosity logs can be converted to match historical porosity logs to continuously use the reservoir models already built using historical logs in production predictions.

[0065] The logging tool 200 can be a part of a wireline logging tool or be included in a downhole assembly as a LWD logging tool in a drilling operation. FIG. 6 is a diagram of an oil drilling system 10 used in the directional drilling of borehole 16. The oil drilling system 10 may be used for drilling on land as well as beneath the water. The borehole 16 is drilled into the earth formation using a rotary drilling rig that includes a derrick 12, drill floor 14, draw works 18, traveling block 20, hook 22, swivel joint 24, kelly joint 26 and rotary table 28. A drill string 100 includes a plurality of drill pipes that are serially connected and secured to the bottom of the kelly joint 26 at the surface. The rotary table 28 is used to rotate the entire drill string 100 while the draw works 18 is used to lower the drill string 100 into the bore hole 16 and apply controlled axial compressive loads. The bottom whole assembly 150 is disposed at the distal end of the drill string 100.

[0066] The drilling fluid (also referred to as mud) is usually stored in mud pits or mud tanks 46, and is transferred using a mud pump 38, which forces the drilling fluid to flow through a surge suppressor 40, then through a kelly hose 42, and through the swivel joint 24 and into the top of the drill string 100. The drilling fluid flows through the drill string 100 at about 150 gallons per minute to about 600 gallons per minute and flows into the bottom whole assembly 150. The drilling fluid then returns to the surface by traveling through the annular space between the outer surface of the drill string 100 and the bore hole 16. When the drilling fluid reaches the surface, it is diverted through a mud return line 44 back to the mud tanks 46.

[0067] The pressure required to keep the drilling fluid in circulation is measured by a pressure sensitive transducer 48 on the kelly hose 42. The pressure sensitive transducer detects changes in pressure caused by the pressure pulses generated by a pulser. The magnitude of the pressure wave from the pulser may be up to 500 psi or more. The measured pressure is transmitted as electrical signals through transducer cable 50 to a surface computer 52, which decodes and displays the transmitted information. Alternatively, the measured pressure is transmitted as electrical signals through transducer cable 50 to a decoder which decodes the electrical signals and transmits the decoded signals to a surface computer 52 which displays the data on a display screen.

[0068] As indicated above, the lower part (“distal part”) of the drill string 100 includes the bottom hole assembly (BHA) 150, which includes a non-magnetic drill collar with a MWD system (MWD assembly or MWD tool) 160 installed therein, logging-while drilling (LWD) instruments sub 165 containing LWD instruments, a downhole motor 170, a near-bit measurement sub 175, and the drill bit 180 having drilling nozzles (not shown). The drilling fluid flows through the drill string 100 and is output through the drilling nozzles of the drill bit 180. During the drilling operation, the drilling system 10 may operate in the rotary mode, in which the drill string 100 is rotated from the surface either by the rotary table 28 or a motor in the traveling block 20 (i.e., a top drive). The drilling system 10 may also operate in a sliding mode, in which the drill string 100 is not rotated from the surface but is driven by the downhole motor 170 rotating the drill bit 180. The drilling fluid is pumped from the surface through the drill string 100 to the drill bit 180, being injected into an annulus between the drill string 100 and the wall of the bore hole 16. The drilling fluid carries the cuttings up from the bore hole 16 to the surface.

[0069] In one or more embodiments, the MWD system 160 may include a pulser sub, a pulser driver sub, a battery sub, a central storage unit, a master board, a power supply sub, a directional module sub, and other sensor boards. In some embodiments, some of these devices may be located in other areas of the BHA 150. One or more of the pulser sub and pulser driver sub may communicate with the pulser 300, which may be located below the MWD system 160. The MWD system 160 can transmit data to the pulser 300 so that the pulser 300 generates pressure pulses.

[0070] The non-magnetic drill collar houses the MWD system 160, which includes a package of instruments for measuring inclination, azimuth, well trajectory (bore hole trajectory), etc. The nuclear logging tool 200 and associated electronic components may be located in LWD instrument sub 165. The nuclear logging tool 200 and other well logging instruments may be electrically or wirelessly coupled together, powered by a battery pack or a power generator driven by the drilling fluid. All information gathered may be transmitted to the surface via in the form of pressure pulses generated by the pulser 300 through the mud column in the drill string.

[0071] The near-bit measurement sub 175 may be disposed between the downhole motor 170 and drill bit 180. The nuclear logging tool 200 may alternatively been installed in the near-bit measure sub 175 to provide more accurate real-time formation parameters to guide directional drilling. The data may be transmitted through the cable embedded in the downhole motor 170 to the MWD system 160 in the bottom whole assembly 150.

[0072] In one embodiment of the current disclosure, a variety of formation parameters obtained using a logging tool having a D-T neutron generator and three dual-function detectors. FIG. 7 shows schematics of neutron pulses, neutron count rates, as well as inelastic spectrum and capture spectrum of neutron-induced gamma rays. The frequency of neutron pulses is 10 kHz (the period is 100 μs) and the neutron duty time is 20 μs, as shown in FIG. 7, panel (b).

[0073] The neutron count rates measured from each of the three detectors, shown in FIG. 7, panel (a), are utilized to obtain formation porosity. Neutrons from three detectors may be further separated according to whether the neutron pulse is ON or OFF, which serves as a coincident or anti-coincident signal to neutrons from the three detectors so that during the neutron pulses (neutron pulse is ON), neutrons are recorded mainly as fast neutrons. Between the neutron pulses (neutron pulse is OFF), neutrons are recorded as thermal neutrons. Fast neutrons and thermal neutrons recorded at three detectors can be used to obtain fast neutron space distribution and thermal neutron space distribution. The neutrons from each detector may also be recorded together. In that case, all neutrons (from thermal neutrons to fast neutrons) are used to obtain the neutron space distribution.

[0074] Gamma rays from three detectors may be further separated according to whether the neutron pulse is ON or OFF, which serves as a coincident or anti-coincident signal to gamma rays from the three detectors so that during the neutron pulses (neutron pulse is ON), gamma rays are mainly recorded as inelastic spectrum, shown in FIG. 7, panel (c). Between the neutron pulses (neutron pulse is OFF), gamma rays are recorded as capture spectrum, shown in FIG. 7, panel (d). Proper time windows are selected so that gamma rays measured in the capture time window are from thermal neutron capture reactions and most gamma rays measured in the inelastic time window are from fast neutron inelastic scattering.

[0075] Backgrounds at detectors may be measured while the neuron generator is OFF for some time and can be subtracted from the total signals of either neutrons or gamma rays. Neutron background measured during the neutron pulses may be further subtracted to get “pure” fast neutrons by using a small percentage of the measured neutrons between the neutron pulses. Similarly, the capture gamma rays measured during the neutron pulses may be further subtracted to get “pure” inelastic spectrum by using a small percentage of the measured capture spectrum between neutron pulses.

[0076] Gamma rays detected by each detector can also be recorded in one energy spectrum (e.g., a total energy spectrum), regardless whether they are initiated from neutron inelastic scattering or neutron capture reactions. In this way, several formation measurements are feasible, such as the formation porosity, elemental concentrations, and formation oil/gas saturation, but one may not be able to get formation density, as the spectrum of inelastic gamma rays are needed to obtain the formation density for a D-T pulsed neutron generator-based measurement system.

[0077] FIG. 8 is an exemplary workflow showing the steps in the processing of data from the logging tool 200 having one D-T neutron generator and three detectors—the near detector, the middle detector, and the far detector. First, signals of from neutrons and neutron-induced gamma rays from three detectors are distinguished using a pulse shape discrimination (PSD) technique. The neutron signals from the three detectors are then utilized to obtain the total count rates (CRN.sub.n, CRN.sub.m, CRN.sub.f), fast neutron count rates (CRFN.sub.n, CRFN.sub.m, CRFN.sub.f), thermal neutron count rates (CRTN.sub.n, CRTN.sub.m, CRTN.sub.f), which are further utilized to obtain the neutron porosity by using three ratios (Rn.sub.f/m, Rn.sub.f/n, Rn.sub.m/n), and fast neutron distribution (e.g., Rfn.sub.f/m, Rfn.sub.f/n, Rfn.sub.m/n) and thermal neutron distribution (e.g., Rtn.sub.f/m, Rtn.sub.f/n, Rtn.sub.m/n).

[0078] The fast neutron space distribution and thermal neutron space distribution may be utilized in the calculation of formation element concentrations using inelastic spectrum and capture spectrum. They may also be utilized to obtain more accurate oil and gas saturations. Examples for obtaining formation porosity, density, element concentrations, as well as gas and oil saturations are provided below.

[0079] As shown in FIG. 8, the count rates of neutrons (CRN) measured during and between neutron pulses from the near detector, the middle detector, and the far detector (CRN.sub.n, CRN.sub.m, CRN.sub.f) are utilized to obtain the formation porosity (ϕ) by using the ratios of the count rates.

[0080] The far-to-middle ratio (Rn.sub.f/m), the far-to-near ratio (Rn.sub.f/n) and the middle-to-near ratio (Rn.sub.m/n) can be obtained by using Equations 1, 2, and 3, respectively. Since the three detectors are placed at different distances from the neutron source, they have different depth of investigations. As a result, near-wellbore environments, such as borehole fluid, cement, etc., have different impacts on the three ratios. The Rn.sub.f/m is more sensitive to the formation, Rn.sub.m/n is more sensitive to the near-wellbore changes and Rn.sub.f/m is sensitive to both.

[00001]$\begin{array}{cc}R{n}_{f/m}=\frac{CR{N}_f}{CR{N}_m}& \left(1\right)\end{array}$$\begin{array}{cc}{\mathrm{Rn}}_{f/n}=\frac{CR{N}_f}{CR{N}_n}& \left(2\right)\end{array}$$\begin{array}{cc}R{n}_{m/n}=\frac{CR{N}_m}{CR{N}_n}& \left(3\right)\end{array}$

[0081] The formation porosity ϕ.sub.n can be obtained by first using Rn.sub.m/n and/or Rn.sub.f/n to correct Rn.sub.f/m, and then use the corrected far-to-middle ratio Rnc.sub.f/m to obtain the formation porosity for a specific formation, e.g., sandstone, limestone or dolomite. Equations (4)-(6) illustrate this algorithm, ΔR being the correction value.

Rnc.sub.f/m=Rn.sub.f/m+ΔR   (4)

ΔR=f.sub.1(Rn.sub.f/m, Rn.sub.f/m, Rn.sub.m/n)   (5)

Φ.sub.n=f.sub.2(Rnc.sub.f/m)   (6)

[0082] The formation porosity Φ.sub.n may also be obtained using the three ratios of count rates of capture gamma rays count rates obtained by the three detectors, according to an algorithm similar to that described in Equations 1-6.

[0083] The formation porosity Φ.sub.n may also be obtained by combining the two porosities obtained by neutrons and capture gamma rays, respectively. Or obtained directly from the three ratios of neutrons and three ratios of capture gamma rays using other methodologies.

[0084] Mineralogy measurement can be obtained by measuring the energy spectrum of gamma rays from both neutron inelastic scattering and neutron capture reactions, using the same tool.

[0085] The gamma rays detected by each detector may be recorded either in two separate spectra (inelastic spectrum and capture spectrum) or in one spectrum (a total spectrum). In either case, the elements can be identified, relative yields of characteristic gamma rays from those elements can be obtained, so as the element concentrations.

[0086] Since the three detectors in the logging tool 200 detect both neutrons and gamma rays simultaneously at three different locations, one may obtain a more precise neutron space distributions (both fast neutron space distribution and thermal neutron space distribution) using the neutron count rates from three detectors. The measured neutron space distributions can then be utilized to get a more accurate calculation of the concentrations of elements such as C, O, H, Cl, Si, etc.

[0087] The count rates of backscattered inelastic gamma rays from the middle detector and the far detector (CRBS.sub.m, CRBS.sub.f) can be used to obtain apparent middle density (ρ.sub.am) and apparent far density (ρ.sub.af), after CRBS.sub.m and CRBS.sub.f are compensated by total initial inelastic gamma rays count rate (CRIN.sub.n) obtained from the near detector, for example, according to Equations 7 and 8. The two apparent densities can then be used to obtain the true formation density (ρ.sub.t), using equations 11 and 12 as an example.

[00002]$\begin{array}{cc}{\rho }_{am}=\frac{1}{{\alpha }_m}\ln \left(\frac{{\beta }_m}{\frac{{\mathrm{CRBS}}_m}{{\mathrm{CRIN}}_n}}\right)& \left(7\right)\end{array}$$\begin{array}{cc}{\rho }_{af}=\frac{1}{{\alpha }_f}\ln \left(\frac{{\beta }_f}{\frac{CRB{S}_f}{{\mathrm{CRIN}}_n}}\right)& \left(8\right)\end{array}$$\begin{array}{cc}{\rho }_t={\rho }_{af}+\mathrm{\Delta \rho }& \left(11\right)\end{array}$$\begin{array}{cc}\mathrm{\Delta \rho }=f\left({\rho }_{\mathrm{am}},{\rho }_{af}\right)& \left(12\right)\end{array}$

[0088] α.sub.m, ρ.sub.m, α.sub.f, β.sub.f are calibration parameters for the middle detector and the far detector, respectively.

[0089] Formation gas saturation measurement can also be obtained using the logging tool 200. Fast neutrons emitted from a neutron source in a tool are quickly slowed down to thermal neutrons by formation. Hydrogen is most effective in slowing down fast neutrons. Some thermal neutrons are captured by formation elements and capture gamma rays are initiated. Both thermal neutrons and capture gamma rays may be scattered back to the three detectors and get detected.

[0090] The count rates at detectors are highly dependent upon downhole formation pores, which are filled by gas, oil, water, or their mixture. All of them are rich in hydrogen. While water and oil have about same hydrogen atomic densities, gas has much lower hydrogen atomic density. As a result, the further away a detector from the neutron source, the detector is more sensitive to gas saturation change. When gas saturation increases, there will be more thermal neutrons and therefore more capture gamma rays at detectors. And the increases of thermal neutrons or capture gamma rays are more in the far detector than in the near detector. Therefore, by utilizing either the ratio of thermal neutron count rate (Rtn.sub.n/f) or the ratio of capture gamma ray count rate (Rg.sub.n/f) from the near and far detectors, together with formation porosity (ϕ), one can obtain the formation gas saturation.

[0091] As the near detector and the far detector in tool 200 can detect both thermal neutrons and capture gamma rays and separate each other, one can obtain the ratio of count rates of thermal neutrons (Rt.sub.n) at the two detectors, as well as the ratio of count rates of the capture gamma rays (R.sub.g) at the two detectors. From them two apparent gas saturations, namely, Sg.sub.n from thermal neutrons and Sg.sub.g from capture gamma rays, the true gas saturation Sg can be obtained independently. The true gas saturation is a function of Sg.sub.n and Sg.sub.g. The exemplary algorithm to obtain formation gas saturation is summarized in Equations 13 through 15.

Sg.sub.n=f.sub.1(Rtn.sub.n/, Φ)   (13)

Sg.sub.g=f.sub.2(Rg.sub.n/f, Φ)   (14)

Sg=f.sub.3(Sg.sub.n, Sg.sub.g)   (15)

[0092] Oil saturation can also be obtained using the ratio of count rates of fast neutron inelastic gamma rays from carbon and oxygen (C/O ratios) in the formation. The gamma rays form fast neutron inelastic scattering on carbon and oxygen can be obtained by fitting and stripping the gamma ray spectra from either the inelastic spectrum or the total spectrum. The neutron source can be either a D-T neutron generator, operated in either pulsed mode or in continuous mode or an isotope neutron source, such as Am—Be, Pu—Be, Cf-252 etc.

[0093] An exemplary algorithm calculates the apparent oil saturations from the three detectors—So.sub.n, So.sub.m, So.sub.f is shown by using Equations 16 through 18, respectively. The apparent oil saturations can be used to obtain the corrected oil saturation (So) using Equation 19.

So.sub.n=f.sub.1(Rg.sub.n,c/o, Φ)   (16)

So.sub.m=f.sub.2(Rg.sub.m,c/o, Φ)   (17)

So.sub.f=f.sub.3(Rg.sub.f,c/o, Φ)   (18)

So=f.sub.4(So.sub.n, So.sub.m, So.sub.f)   (19)

[0094] The corrected oil saturation may also be obtained by using the C/O ratios (Rg.sub.n,c/o, Rg.sub.m,c/o, Rg.sub.f,c/o), formation porosity (ϕ) and fast neutron space distribution (Rfn.sub.f/m, Rfn.sub.f/n, Rfn.sub.m/n) from the three directors, shown in Equation

So=f.sub.5(Rg.sub.n,c/o, Rg.sub.m,c/o, Rg.sub.f,c/o, Φ, Rfn.sub.f/m, Rfn.sub.f/n, Rfn.sub.m/n)   (20)

[0095] While in the foregoing specification this disclosure has been described in relation to certain preferred embodiments thereof, and many details have been set forth for purpose of illustration, it will be apparent to those skilled in the art that the disclosure is susceptible to alteration and that certain other details described herein can vary considerably without departing from the basic principles of the disclosure. In addition, it should be appreciated that structural features or methodologies shown or described in any one embodiment herein can be used in other embodiments as well.