AI Article Synopsis

  • This study surveyed the presence of both artificial (such as Cs, Am, Bi, Pu isotopes) and natural radionuclides (like Pb, Ac, Bi, K) in cryoconite from Norwegian glaciers.
  • Samples from the Blåisen Glacier showed extremely high activity concentrations of certain radionuclides, with cesium levels reaching as high as 25,000 Bq/kg, and notable amounts of organic matter, about 40% of total mass.
  • The study suggests that bioaccumulation in organic-rich cryoconite rather than rainfall was the key factor influencing these high radionuclide levels.

Article Abstract

This study is a first survey of the occurrence of artificial (Cs, Am, Bi, Pu isotopes) and natural (Pb, Ac, Bi, K) radionuclides in Norwegian cryoconite. Cryoconite samples were collected before (12 samples) and after (5 samples) a rainfall event, after which 7 cryoconite holes dissapeared. The concentrations of radionuclides in cryoconite samples from the Blåisen Glacier are compared with data from the Arctic and Alpine glaciers. Cryoconite samples from the studied glacier had extremely high activity concentrations of Cs, Am, Bi and Pu (up to 25,000 Bq/kg, 58 Bq/kg, 13 Bq/kg and 131 Bq/kg, respectively) and also high concentrations of organic matter (OM), comparing to other Scandinavian and Arctic glaciers, reaching up to ~40% of total mass. The outstandingly high concentrations of Cs, Am, Pu isotopes, and Bi on the Blåisen Glacier are primarily related to bioaccumulation of radionuclides in organic-rich cryoconite and might be enhanced by additional transfers of contamination from the tundra by lemmings during their population peaks. The presumed influence of intense rainfall on radionuclide concentrations in the cryoconite was not confirmed.

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http://dx.doi.org/10.1016/j.scitotenv.2021.152656DOI Listing

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