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An unknown source of reactor radionuclides in the Baltic Sea revealed by multi-isotope fingerprints
We present an application of multi-isotopic fingerprints (i.e., 236 U/ 238 U, 233 U/ 236 U, 236 U/ 129 I and 129 I/ 127 I) for the discovery of previously unrecognized sources of anthropogenic radioactivity. Our data indicate a source of reactor 236 U in the Baltic Sea in addition to inputs from the...
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Published in: | Nature communications 2021-02, Vol.12 (1), p.823-10, Article 823 |
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Main Authors: | , , , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | We present an application of multi-isotopic fingerprints (i.e.,
236
U/
238
U,
233
U/
236
U,
236
U/
129
I and
129
I/
127
I) for the discovery of previously unrecognized sources of anthropogenic radioactivity. Our data indicate a source of reactor
236
U in the Baltic Sea in addition to inputs from the two European reprocessing plants and global fallout. This additional reactor
236
U may come from unreported discharges from Swedish nuclear research facilities as supported by high
236
U levels in sediment nearby Studsvik, or from accidental leakages of spent nuclear fuel disposed on the Baltic seafloor, either reported or unreported. Such leakages would indicate problems with the radiological safety of seafloor disposal, and may be accompanied by releases of other radionuclides. The results demonstrate the high sensitivity of multi-isotopic tracer systems, especially the
233
U/
236
U signature, to distinguish environmental emissions of unrevealed radioactive releases for nuclear safeguards, emergency preparedness and environmental tracer studies.
Anthropogenic activities lead to the accumulation of radioactive substances in the environment. Here the authors use multi-isotopic fingerprints of uranium and iodine to discover a previously unknown source of reactor uranium in the Baltic Sea, likely sourced from a Swedish nuclear facility. |
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ISSN: | 2041-1723 2041-1723 |
DOI: | 10.1038/s41467-021-21059-w |