Krypton-85 chronometry of spent nuclear fuel

Abstract. We describe the use of the radionuclide 85Kr, which is produced by nuclear fission and has a half-life of 10.76 years, to determine the age of spent nuclear fuel. The method is based on mass-spectrometric measurement of the relative abundance of fissiogenic Kr isotopes extracted from a fuel sample, and we show that it can be applied to micron-scale particles of spent fuel that are analogous to particles that have been released into the environment from various nuclear facilities in the past. 85Kr chronometry is potentially valuable for identifying and attributing nuclear materials, grouping samples into collections of common origin that can be used to reconstruct the origin and irradiation history of the material, and verifying declared nuclear activities in the context of international monitoring programs.

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Publication Details

Journal
Geochronology
Published
2024-10-25
DOI
https://doi.org/10.5194/gchron-6-571-2024
Citations
2
Primary Topic
Radioactive contamination and transfer
Type
article
Field-Weighted Citation Impact
0.57

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article

Krypton-85 chronometry of spent nuclear fuel

Andrew Conant, Chelsea D. Willett, Brett H. Isselhardt, Dallin Barton et al.
2 citations
Geochronology
Radioactive contamination and transfer
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article

Krypton-85 chronometry of spent nuclear fuel

Andrew Conant, Chelsea D. Willett, Brett H. Isselhardt, Dallin Barton, Greg Balco, Dallas D. Reilly
article en
2 citations

Abstract

Abstract. We describe the use of the radionuclide 85Kr, which is produced by nuclear fission and has a half-life of 10.76 years, to determine the age of spent nuclear fuel. The method is based on mass-spectrometric measurement of the relative abundance of fissiogenic Kr isotopes extracted from a fuel sample, and we show that it can be applied to micron-scale particles of spent fuel that are analogous to particles that have been released into the environment from various nuclear facilities in the past. 85Kr chronometry is potentially valuable for identifying and attributing nuclear materials, grouping samples into collections of common origin that can be used to reconstruct the origin and irradiation history of the material, and verifying declared nuclear activities in the context of international monitoring programs.

GeochronologyVol. 6(4)
Lawrence Livermore National Laboratory (US), Oak Ridge National Laboratory (US), Pacific Northwest National Laboratory (US)
U.S. Department of Energy
Openalex Percentile: Top 33%
Radioactive contamination and transfer
0.57
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