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inelastic gamma rays

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Journal Article
Published: 01 December 2010
Russ. Geol. Geophys. (2010) 51 (12): 1295–1303.
... the moment of neutron emission from the device to the moment the device records the gamma rays from neutron inelastic scattering (inelastic gamma rays, IGRs) in the formation. The time interval characterizes the distance to the point of origin of a gamma ray, and the energy of a gamma ray passing through...
FIGURES
Journal Article
Journal: Geophysics
Published: 22 May 2023
Geophysics (2023) 88 (4): D259–D269.
... and the gamma transport theory, the distribution of capture gamma rays is described. A new neutron-gamma porosity measurement method is developed based on inelastic and capture gamma-ray distribution. The applicability of the new method in different environments is analyzed using the Monte Carlo method...
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Image
Tally, material, and cutoff cards used to model inelastic gamma-ray counts for the Longhorn NGD LWD logging tool in MCNP.
Published: 08 January 2019
Figure 11. Tally, material, and cutoff cards used to model inelastic gamma-ray counts for the Longhorn NGD LWD logging tool in MCNP.
Journal Article
Journal: Geophysics
Published: 09 November 2020
Geophysics (2020) 85 (6): D219–D232.
... of the factors influencing the accuracy of the results, which should be considered. We have adopted a method, based on the difference between the inelastic gamma-ray response of high- and low-energy windows, to reduce the impact of pair production upon calculating the bulk density. A new density estimation...
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Journal Article
Journal: Geophysics
Published: 08 January 2019
Geophysics (2019) 84 (1): D39–D56.
...Figure 11. Tally, material, and cutoff cards used to model inelastic gamma-ray counts for the Longhorn NGD LWD logging tool in MCNP. ...
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Image
Description of the nuclear interactions contributing to NGD measurements, including fast neutron transport and gamma-ray transport. Secondary gamma rays are emitted during fast neutron transport through inelastic scattering or (n,x) interactions, where (n,x) interactions include, for example, (n,2n), (n,α), (n,n′α), (n,p), (n,n′p), or (n,d) interactions. During gamma-ray transport, secondary gamma rays are generated through Compton scattering, pair production, annihilation, and bremsstrahlung interactions.
Published: 08 January 2019
Figure 3. Description of the nuclear interactions contributing to NGD measurements, including fast neutron transport and gamma-ray transport. Secondary gamma rays are emitted during fast neutron transport through inelastic scattering or ( n , x ) interactions, where ( n , x
Journal Article
Journal: Geophysics
Published: 20 July 2015
Geophysics (2015) 80 (5): D501–D523.
...Oyinkansola Ajayi; Carlos Torres-Verdín; William E. Preeg ABSTRACT Neutron-induced gamma-ray spectroscopy measurements originate from inelastic neutron scattering and thermal neutron capture of chemical elements excited by neutrons; they are widely used to quantify in situ elemental and mineral...
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Journal Article
Journal: Geophysics
Published: 01 November 1980
Geophysics (1980) 45 (11): 1667–1684.
... contributions; the neutron die-away log allows determination of saturation through casing; inelastic and capture gamma-ray spectroscopy provide various elemental determinations, including C/O and Si/Ca logs; and activation logging promises to furnish additional elemental measurements. A new log of photoelectric...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1985
AAPG Bulletin (1985) 69 (9): 1442.
... Office of the Department of Energy, and the development, by USGS and Princeton Gamma-Tech, of the melting-cryogen-cooled high-purity germanium borehole gamma-ray detector. A technique of relating mass fractions to measured gamma-ray intensities, which eliminates the need for detailed knowledge...
Journal Article
Journal: Geophysics
Published: 16 November 2015
Geophysics (2016) 81 (1): D9–D34.
... conditions. borehole geophysics logging log analysis inversion algorithm Spectroscopy logs measure gamma-ray counts as a function of energy. Gamma rays are emitted during high-energy inelastic neutron scattering or thermal-neutron capture. Elemental relative yields and weight concentrations...
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Image
Impact of variations in migration length on formation spectra and neutron FSFs for inelastic and capture spectra; (a and d) show inelastic and capture spectra, respectively; (b and e) show radially and azimuthally integrated inelastic and capture neutron FSFs along the tool, respectively, where purple lines at S and SS identify the pulsed-neutron source, short-spaced detector, and long-spaced detector positions along the tool, respectively; (c and f) show vertically and azimuthally integrated inelastic and capture neutron FSFs as a function of radial distance into the formation, respectively. The transition from blue to red colors indicates an increase in migration length. Note: the vertical axis on panels (a, b, d, and e) is not shown because the spectroscopy count data, location of the neutron source, and gamma-ray detectors of the commercial tool under study are confidential.
Published: 20 July 2015
, respectively. The transition from blue to red colors indicates an increase in migration length. Note: the vertical axis on panels (a, b, d, and e) is not shown because the spectroscopy count data, location of the neutron source, and gamma-ray detectors of the commercial tool under study are confidential.
Image
Comparison of (a) vertical resolution and (b) radial length of investigation between inelastic and capture measurements in 25-porosity-units (p.u.) freshwater-saturated sandstone formation. Panel (a) shows radially and azimuthally integrated inelastic and capture neutron FSFs along the tool, where the gray solid lines at S and SS identify the pulsed-neutron source and short-spaced detector positions along the tool, respectively, and panel (b) shows the cumulative vertically integrated FSF (radial geometric factor). The depth of investigation of the tool is defined by 90% of the radial geometric factor, and it is shown in panel (b) as the black dashed and black solid lines for capture and inelastic measurements, respectively. Note: The vertical axis in panel (a) is not shown because the locations of the neutron source and short-spaced gamma-ray detector of the commercial tool under study are confidential.
Published: 16 November 2015
% of the radial geometric factor, and it is shown in panel (b) as the black dashed and black solid lines for capture and inelastic measurements, respectively. Note: The vertical axis in panel (a) is not shown because the locations of the neutron source and short-spaced gamma-ray detector of the commercial tool
Journal Article
Journal: Geophysics
Published: 01 August 1960
Geophysics (1960) 25 (4): 883–890.
.... These improvements plus future developments in gamma-ray spectral logs, neutron-gamma spectral logs, neutron activation logs, and neutron inelastic scattering logs promise a bright future for radioactivity logging. GeoRef, Copyright 2008, American Geological Institute. Reference includes data from Bibliography...
Image
MDPNT quality control, showing. the tool operating parameters in tracks 1 and 2. Track 1 also includes the measured gamma ray response. Track 3 shows the measured sigma from the three detectors. The capture and inelastic counts for all the detectors are shown in tracks 4 and 5, respectively. Track 6 shows the oxygen ratios for all the three detectors.
Published: 16 January 2015
Figure 4. MDPNT quality control, showing. the tool operating parameters in tracks 1 and 2. Track 1 also includes the measured gamma ray response. Track 3 shows the measured sigma from the three detectors. The capture and inelastic counts for all the detectors are shown in tracks 4 and 5
Journal Article
Journal: Geophysics
Published: 01 February 2022
Geophysics (2022) 87 (2): D21–D31.
.../10.1016/j.jappgeo.2011.06.034 . JAGPEA 0926-9851 Roscoe B. A. Grau J. A. , 1988 , Response of the carbon/oxygen measurement for an inelastic gamma ray spectroscopy tool : SPE Formation Evaluation , 3 , 76 – 80 , doi: http://dx.doi.org/10.2118/14460-PA . SFEVEG 0885-923X Sa...
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Journal Article
Journal: Geophysics
Published: 10 December 2018
Geophysics (2018) 83 (6): D231–D246.
... 20.72 0.60 k 1 () − 0.51 − 0.31 − 12.57 − 6.00 k 2 () − 7.96 0.33 − 16.14 − 21.11 At gamma-ray detectors, inelastic gamma-ray counts G R are approximated with ∑ m = 0...
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Journal Article
Journal: Interpretation
Published: 30 December 2014
Interpretation (2015) 3 (1): SA135–SA142.
... their energy drops to the same level as the surrounding environment (thermal energy level), they get captured by the surrounding atoms. The neutron interactions of interest for pulsed-neutron logging are the inelastic and capture interactions. The energy and intensity of the gamma rays that are emitted...
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Journal Article
Journal: Interpretation
Published: 18 April 2016
Interpretation (2016) 4 (2): SF93–SF111.
... in petrophysical parameters between formations indicates that each formation is best analyzed individually. A comprehensive set of elemental dry weights was obtained using a new neutron-induced capture and inelastic gamma ray spectroscopy device ( Radtke et al., 2012 ). Laboratory wave-length-dispersive XRF...
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Journal Article
Journal: Interpretation
Published: 16 January 2015
Interpretation (2015) 3 (1): SA159–SA166.
...Figure 4. MDPNT quality control, showing. the tool operating parameters in tracks 1 and 2. Track 1 also includes the measured gamma ray response. Track 3 shows the measured sigma from the three detectors. The capture and inelastic counts for all the detectors are shown in tracks 4 and 5...
FIGURES | View All (6)
Journal Article
Published: 01 February 2016
Vadose Zone Journal (2016) 15 (2): vzj2015.04.0056.
... was used for carbon content measurement while accounting for the system background interference. Accounting for Si-28 γ ray contributions to the carbon peak can be done by evaluating the intensity of 1.78-MeV γ rays due to INS on Si-28. Gamma rays with energies of 1.78 MeV due to Al-28 decay...
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