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Zeitschriften
Geochronometria
Band 48 (2021): Heft 1 (January 2021)
Uneingeschränkter Zugang
The Application of Full Spectrum Analysis to NaI(Tl) Gamma Spectrometry for the Determination of Burial Dose Rates
Minqiang Bu
Minqiang Bu
,
Andrew S. Murray
Andrew S. Murray
,
Myungho Kook
Myungho Kook
,
Jan-Pieter Buylaert
Jan-Pieter Buylaert
und
Kristina J. Thomsen
Kristina J. Thomsen
| 31. Dez. 2021
Geochronometria
Band 48 (2021): Heft 1 (January 2021)
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Online veröffentlicht:
31. Dez. 2021
Seitenbereich:
161 - 170
Eingereicht:
15. Feb. 2019
Akzeptiert:
28. Okt. 2019
DOI:
https://doi.org/10.2478/geochr-2020-0009
Schlüsselwörter
NaI(Tl) detector
,
scintillation gamma spectrometry
,
full spectrum analysis (FSA)
,
minimum detection limit (MDL)
,
burial dose rate measurement
,
OSL dating
© 2019 Minqiang Bu et al., published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.
Fig. 1
Drift correction reference spectrum KUTh mix, and drift-corrected spectra from 40K, 238U and 232Th calibration standards and background.
Fig. 2
Illustration of the agreement of a calculated fitted spectrum with the original sample spectrum, together with fitting residuals in each channel.
Fig. 3
(a–c) Minimum detection limits (MDLs) for activities of 40K, 238U and 232Th, respectively, defined as random uncertainty approaching 30%, when random uncertainty is expressed as a function of expected activity (AEXP); (d–f) Comparison of measured 40K, 238U and 232Th activity concentration (AMEAS) and expected activity concentration (AEXP), showing the accuracy of measurement and FSA analysis. The error bars in panels (d-f) shows the random uncertainty.
Fig. 4
Normalized deviations between those activity concentrations for 40K, 238U and 232Th (a–c), and total (β + γ) dose rates (d) determined by the NaI(Tl) spectrometer and those determined by an HPGe spectrometer, for 20 geological samples. The shaded regions represent ±5% deviation in panels (a–c), and ±4% deviation in panel (d). The standard deviation for 20 data in each subpanel show a high measurement precision on NaI(Tl) spectrometer. All error bars in panel (a-c) and in panel (d) are derived from the total uncertainties of ACNaI and ACHPGe, and total uncertainties of DRNaI and DRHPGe, respectively.
Fig. 5
Activity concentrations (a-c) and total dose rate (d) of a natural sample (LD962) counted with different counting time on NaI(Tl spectrometer. The horizontal dashed line in the centre of shaded region in each subpanel represents the activity concentration (a-c) and total dose rate (d) from HPGe spectrometer. All error bars in panel (a-c) and in panel (d) denote the total uncertainties of ACNaI, and total uncertainties of DRNaI, respectively.
Fig. 6
Dependence of relative total dose rate uncertainty on counting time, for a sample containing 235, 8.6, and 8.3 Bq·kg−1 of 40K, 238U and 232Th, respectively and a total dose rate of 1.09 Gy·ka−1.
Average ratios of ACNaI/ACHPGe and DRNaI/DRHPGe (n = 20).
Average ratio
40
K
0.995 ± 0.005
238
U
0.984 ± 0.005
232
Th
1.005 ± 0.006
Total dose rate
0.993 ± 0.004
Updated 40K, 238U and 232Th activity concentration per ppm for dose rate derivation.
Radionuclide
Activity concentration (Bq·kg
−1
)
Uncertainty (Bq·kg
−1
)
40
K
317
3
238
U
12.922
0.025
232
Th
4.061
0.029
Comparison of MDLs (Bq·kg−1) from different studies.
Nuclide
NaI(Tl) spectrometer (Sample weight: 0.23 kg)
HPGe spectrometer (Sample weight: 0.25 kg)
FSA (This study)
3-Window (
Bu
et al.
, 2018
)
(
Murray
et al
., 2018
)
40
K
4.8
21
0.6
238
U
0.4
4.0
0.04
232
Th
0.3
2.1
0.03
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