Radioactivity and geochemical characteristics of cryoconite on the Tien Shan glacier

The article reports on a study of the cryoconite contamination with anthropogenic and natural radionuclides, as well as ore caused elements, conducted on the Tuyuksu Glacier. The activity concentrations of anthropogenic radionuclides <sup>137</sup>Cs, <sup>239+240</sup>Pu, <sup>238</sup>Pu, and <sup>241</sup>Am were determined, with maximum values of about 2000 Bq kg<sup>-1</sup>, 35 Bq kg<sup>-1</sup>, 1 Bq kg<sup>-1</sup>, and 25 Bq kg<sup>-1</sup>, respectively. An analysis of the radionuclide activity concentration ratios indicates that global fallout is the main and likely the only source of anthropogenic radionuclides. Natural isotopes <sup>235</sup>U, <sup>238</sup>U, and <sup>232</sup>Th, along with their decay products were found to have a lithogenic origin. The study of the elemental composition of cryoconite sediments revealed significant accumulations of Cu, Mo, Sn, Zn, As, Co, Sb, Pb, and Se, which are characteristic of polymetallic and other ore deposits in this region. The Clarke values of concentrations for these elements exceed those of the Upper Continental Crust (UCC) by several times. We believe this reflects the combined influence of numerous large mining, processing, and metallurgical enterprises in Kazakhstan and neighboring countries.

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Journal
Scientific Reports
Published
2025-10-14
DOI
https://doi.org/10.1038/s41598-025-19680-6
Primary Topic
Radioactivity and Radon Measurements
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article
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article

Radioactivity and geochemical characteristics of cryoconite on the Tien Shan glacier

S. G. Lennik, V. S. Morenko, Enver Asadulin, Pavel Kharkin et al.
Scientific Reports
Radioactivity and Radon Measurements
article

Radioactivity and geochemical characteristics of cryoconite on the Tien Shan glacier

S. G. Lennik, V. S. Morenko, Enver Asadulin, Pavel Kharkin, А. С. Сериков, Mariya Severinenko, Alexander Kokarev, V. Yu. Fedulov, Olga Milts, V A Makarova, Vassiliy Kapitsa, Marina Krasnopyorova, Galina Nadyarnykh, D.S. Akhmetzhanova, Alexey Miroshnikov, Nikolay Kasatkin, Sayabek Sakhiev
article en

Abstract

The article reports on a study of the cryoconite contamination with anthropogenic and natural radionuclides, as well as ore caused elements, conducted on the Tuyuksu Glacier. The activity concentrations of anthropogenic radionuclides <sup>137</sup>Cs, <sup>239+240</sup>Pu, <sup>238</sup>Pu, and <sup>241</sup>Am were determined, with maximum values of about 2000 Bq kg<sup>-1</sup>, 35 Bq kg<sup>-1</sup>, 1 Bq kg<sup>-1</sup>, and 25 Bq kg<sup>-1</sup>, respectively. An analysis of the radionuclide activity concentration ratios indicates that global fallout is the main and likely the only source of anthropogenic radionuclides. Natural isotopes <sup>235</sup>U, <sup>238</sup>U, and <sup>232</sup>Th, along with their decay products were found to have a lithogenic origin. The study of the elemental composition of cryoconite sediments revealed significant accumulations of Cu, Mo, Sn, Zn, As, Co, Sb, Pb, and Se, which are characteristic of polymetallic and other ore deposits in this region. The Clarke values of concentrations for these elements exceed those of the Upper Continental Crust (UCC) by several times. We believe this reflects the combined influence of numerous large mining, processing, and metallurgical enterprises in Kazakhstan and neighboring countries.

Scientific ReportsVol. 15(1)
Institute of Oceanology. PP Shirshov Russian Academy of Sciences (RU), Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry (RU), National Nuclear Center of the Republic of Kazakhstan (KZ), Global Health Research Center of Central Asia (KZ)
Openalex Percentile: Top 58%
Radioactivity and Radon Measurements
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