The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas

Over the recent few decades, due to climate warming and the continuing exploration of Arctic seas’ mineral resources, the scientific interest in contamination problems has deepened significantly. In this study, for the first time, we characterize the distribution features of 47 elements (major and t...

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Published in:Minerals
Main Authors: Dmitry F. Budko, Liudmila L. Demina, Anna V. Travkina, Dina P. Starodymova, Tatiyana N. Alekseeva
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
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Online Access:https://doi.org/10.3390/min12030328
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spelling ftmdpi:oai:mdpi.com:/2075-163X/12/3/328/ 2023-08-20T04:04:56+02:00 The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas Dmitry F. Budko Liudmila L. Demina Anna V. Travkina Dina P. Starodymova Tatiyana N. Alekseeva agris 2022-03-06 application/pdf https://doi.org/10.3390/min12030328 EN eng Multidisciplinary Digital Publishing Institute Mineral Geochemistry and Geochronology https://dx.doi.org/10.3390/min12030328 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 12; Issue 3; Pages: 328 Barents Sea Kara Sea Laptev Sea East Siberian Sea bottom sediments radionuclides major and trace elements criteria of contamination potential ecological risk Text 2022 ftmdpi https://doi.org/10.3390/min12030328 2023-08-01T04:22:42Z Over the recent few decades, due to climate warming and the continuing exploration of Arctic seas’ mineral resources, the scientific interest in contamination problems has deepened significantly. In this study, for the first time, we characterize the distribution features of 47 elements (major and trace elements, including heavy metals, metalloid As, and Cs-137 technogenic radionuclide) in surface bottom sediments from some areas of the Barents, Kara, Laptev, and East-Siberian Seas. The lithogenic material was the main factor that controlled variability in many elements (Be, Al, Ti, Cr, Ga, Rb, Sr, Y, Zr, Nb, Ba, REE, Pb, Th, U, W, and Cs). Among the hydrogenic processes, the formation of Fe and Mn oxyhydroxides has the greatest impact on the Mn, Fe, Co, Ni, Cu, Ge, and Mo, and insignificantly V and Sb, variability in sediments. These, along with minor to moderate values of enrichment factor (EF) for most elements, allowed us to conclude that the observed element distribution is related to predominantly natural processes of thermal abrasion, river-run, and atmospheric input. The exception is As, which exhibited the elevated EF (up to 20) in the western and central Kara Sea, as well as in the Vilkitsky Strait. Since no significant relationship between As and Fe andMn oxyhydroxides distribution was found, we may assume primarily an anthropogenic source of As, related to the peat and/or coal combustion. According to the criteria of Ecological Risks assessment, all the examined areas have a low degree of risk. Data on the specific activity of Cs-137 correspond to the background average values characteristic for these regions. The highest levels of Cs-137 concentration (Bq/kg) were detected in the sediments of the Ob and Yenisei Rivers’ estuaries. Text Arctic Barents Sea East Siberian Sea Kara Sea Kara-Laptev laptev Laptev Sea MDPI Open Access Publishing Arctic Barents Sea Laptev Sea Kara Sea East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) Minerals 12 3 328
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Barents Sea
Kara Sea
Laptev Sea
East Siberian Sea
bottom sediments
radionuclides
major and trace elements
criteria of contamination
potential ecological risk
spellingShingle Barents Sea
Kara Sea
Laptev Sea
East Siberian Sea
bottom sediments
radionuclides
major and trace elements
criteria of contamination
potential ecological risk
Dmitry F. Budko
Liudmila L. Demina
Anna V. Travkina
Dina P. Starodymova
Tatiyana N. Alekseeva
The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas
topic_facet Barents Sea
Kara Sea
Laptev Sea
East Siberian Sea
bottom sediments
radionuclides
major and trace elements
criteria of contamination
potential ecological risk
description Over the recent few decades, due to climate warming and the continuing exploration of Arctic seas’ mineral resources, the scientific interest in contamination problems has deepened significantly. In this study, for the first time, we characterize the distribution features of 47 elements (major and trace elements, including heavy metals, metalloid As, and Cs-137 technogenic radionuclide) in surface bottom sediments from some areas of the Barents, Kara, Laptev, and East-Siberian Seas. The lithogenic material was the main factor that controlled variability in many elements (Be, Al, Ti, Cr, Ga, Rb, Sr, Y, Zr, Nb, Ba, REE, Pb, Th, U, W, and Cs). Among the hydrogenic processes, the formation of Fe and Mn oxyhydroxides has the greatest impact on the Mn, Fe, Co, Ni, Cu, Ge, and Mo, and insignificantly V and Sb, variability in sediments. These, along with minor to moderate values of enrichment factor (EF) for most elements, allowed us to conclude that the observed element distribution is related to predominantly natural processes of thermal abrasion, river-run, and atmospheric input. The exception is As, which exhibited the elevated EF (up to 20) in the western and central Kara Sea, as well as in the Vilkitsky Strait. Since no significant relationship between As and Fe andMn oxyhydroxides distribution was found, we may assume primarily an anthropogenic source of As, related to the peat and/or coal combustion. According to the criteria of Ecological Risks assessment, all the examined areas have a low degree of risk. Data on the specific activity of Cs-137 correspond to the background average values characteristic for these regions. The highest levels of Cs-137 concentration (Bq/kg) were detected in the sediments of the Ob and Yenisei Rivers’ estuaries.
format Text
author Dmitry F. Budko
Liudmila L. Demina
Anna V. Travkina
Dina P. Starodymova
Tatiyana N. Alekseeva
author_facet Dmitry F. Budko
Liudmila L. Demina
Anna V. Travkina
Dina P. Starodymova
Tatiyana N. Alekseeva
author_sort Dmitry F. Budko
title The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas
title_short The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas
title_full The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas
title_fullStr The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas
title_full_unstemmed The Features of Distribution of Chemical Elements, including Heavy Metals and Cs-137, in Surface Sediments of the Barents, Kara, Laptev and East Siberian Seas
title_sort features of distribution of chemical elements, including heavy metals and cs-137, in surface sediments of the barents, kara, laptev and east siberian seas
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/min12030328
op_coverage agris
long_lat ENVELOPE(166.000,166.000,74.000,74.000)
geographic Arctic
Barents Sea
Laptev Sea
Kara Sea
East Siberian Sea
geographic_facet Arctic
Barents Sea
Laptev Sea
Kara Sea
East Siberian Sea
genre Arctic
Barents Sea
East Siberian Sea
Kara Sea
Kara-Laptev
laptev
Laptev Sea
genre_facet Arctic
Barents Sea
East Siberian Sea
Kara Sea
Kara-Laptev
laptev
Laptev Sea
op_source Minerals; Volume 12; Issue 3; Pages: 328
op_relation Mineral Geochemistry and Geochronology
https://dx.doi.org/10.3390/min12030328
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/min12030328
container_title Minerals
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