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Temporal variability of Pu signatures in a Pb-210-dated Sphagnum peat profile from the Northern Ural, Russian Federation

Temporal variability of Pu signatures in a Pb-210-dated Sphagnum peat profile from the Northern Ural, Russian Federation
Temporal variability of Pu signatures in a Pb-210-dated Sphagnum peat profile from the Northern Ural, Russian Federation

The peat archives are one of the stratigraphic records revealing clearly physical, chemical and biological signals of human influence on the Earth System since the 1950s, at least. The presented study was aimed mainly to identify the level and origin of anthropogenic radionuclides such as 238, 239, 240Pu in a 210Pb-dated peat profile derived from the Northern Ural, Russian Federation. As stated, the vertical variability of 240Pu/ 239Pu isotopic compositions reflects the nuclear weapons testing history with the maximum in the 1960s and small regional impact most likely of high-yielded tests in the 1950s as well as Chinese detonations in the 1970s. Peat accumulations rates were similar to those obtained in adjacent areas, whereas 210Pb flux slightly exceeded the reference level established for adequate latitude belt.

Antropocene, High-yielded nuclear tests, Pb-210 dating, Peat deposit, Plutonium isotopic composition, Ural mountains
0045-6535
Cwanek, A.
07b1c53d-1dd6-4aee-8072-70af29583768
Łokas, E.
029668d2-9da2-4aab-afe1-93df8c2e3943
Mitchell, E.A.D.
33f2099f-f073-4c69-bb14-5b072b54979f
Mazei, Y.
a94d31f7-366e-4109-a998-2b05714e152a
Gaca, P.
3d23473d-db81-436a-a12d-ad707db4abc8
Milton, J.A.
9e183221-d0d4-4ddb-aeba-0fdde9d31230
Cwanek, A.
07b1c53d-1dd6-4aee-8072-70af29583768
Łokas, E.
029668d2-9da2-4aab-afe1-93df8c2e3943
Mitchell, E.A.D.
33f2099f-f073-4c69-bb14-5b072b54979f
Mazei, Y.
a94d31f7-366e-4109-a998-2b05714e152a
Gaca, P.
3d23473d-db81-436a-a12d-ad707db4abc8
Milton, J.A.
9e183221-d0d4-4ddb-aeba-0fdde9d31230

Cwanek, A., Łokas, E., Mitchell, E.A.D., Mazei, Y., Gaca, P. and Milton, J.A. (2021) Temporal variability of Pu signatures in a Pb-210-dated Sphagnum peat profile from the Northern Ural, Russian Federation. Chemosphere, 281, [130962]. (doi:10.1016/j.chemosphere.2021.130962).

Record type: Article

Abstract

The peat archives are one of the stratigraphic records revealing clearly physical, chemical and biological signals of human influence on the Earth System since the 1950s, at least. The presented study was aimed mainly to identify the level and origin of anthropogenic radionuclides such as 238, 239, 240Pu in a 210Pb-dated peat profile derived from the Northern Ural, Russian Federation. As stated, the vertical variability of 240Pu/ 239Pu isotopic compositions reflects the nuclear weapons testing history with the maximum in the 1960s and small regional impact most likely of high-yielded tests in the 1950s as well as Chinese detonations in the 1970s. Peat accumulations rates were similar to those obtained in adjacent areas, whereas 210Pb flux slightly exceeded the reference level established for adequate latitude belt.

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More information

Published date: October 2021
Additional Information: Funding Information: The authors are thankful to Olga Smirnova, Alexey Aleynikov, Alexey Efimenko, Alexandr Laznikov, Pavel Dmitrovich and Natalie Lemonis for their help during the fieldwork. The Pu analysis was founded by the Institute of Nuclear Physics, Polish Academy of Sciences from statutory research resources. Publisher Copyright: © 2021 The Author(s) Copyright: Copyright 2021 Elsevier B.V., All rights reserved.
Keywords: Antropocene, High-yielded nuclear tests, Pb-210 dating, Peat deposit, Plutonium isotopic composition, Ural mountains

Identifiers

Local EPrints ID: 454124
URI: http://eprints.soton.ac.uk/id/eprint/454124
ISSN: 0045-6535
PURE UUID: b5e3a964-04cf-445d-8828-1d85e86f4ae3
ORCID for J.A. Milton: ORCID iD orcid.org/0000-0003-4245-5532

Catalogue record

Date deposited: 31 Jan 2022 17:51
Last modified: 06 Jun 2024 01:35

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Contributors

Author: A. Cwanek
Author: E. Łokas
Author: E.A.D. Mitchell
Author: Y. Mazei
Author: P. Gaca
Author: J.A. Milton ORCID iD

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