Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes
In natural water, as a rule, there is a violation of radioactive equilibrium in the chain 238 U … → 234 U → 230 Th →. Groundwater usually has a 234 U/ 238 U ratio in the range of 0.8–3.0 (by activity). However, in some regions, the 234 U/ 238 U ratio reaches >10 and up to 50. Ultrahigh excesses o...
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ftdoajarticles:oai:doaj.org/article:dda64165690e4d17ae1bed4fed07c1ff 2023-05-15T17:57:09+02:00 Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes Igor Tokarev Evgeny Yakovlev 2021-12-01T00:00:00Z https://doi.org/10.3390/w13243514 https://doaj.org/article/dda64165690e4d17ae1bed4fed07c1ff EN eng MDPI AG https://www.mdpi.com/2073-4441/13/24/3514 https://doaj.org/toc/2073-4441 doi:10.3390/w13243514 2073-4441 https://doaj.org/article/dda64165690e4d17ae1bed4fed07c1ff Water, Vol 13, Iss 3514, p 3514 (2021) non-equilibrium uranium 234 U/ 238 U ratio climate variations permafrost World Ocean Lake Baikal Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 article 2021 ftdoajarticles https://doi.org/10.3390/w13243514 2022-12-31T12:43:59Z In natural water, as a rule, there is a violation of radioactive equilibrium in the chain 238 U … → 234 U → 230 Th →. Groundwater usually has a 234 U/ 238 U ratio in the range of 0.8–3.0 (by activity). However, in some regions, the 234 U/ 238 U ratio reaches >10 and up to 50. Ultrahigh excesses of 234 U can be explained by climatic variations. During a cold period, minerals accumulate 234 U as a normal component of the radioactive chain, and after the melting of permafrost, it is lost from the mineral lattice faster than 238 U due to its higher geochemical mobility. This hypothesis was tested using data on the isotopic composition of uranium in the chemo- and bio-genic formations of the World Ocean and large lakes, which are reservoirs that accumulate continental runoff. The World Ocean has the most significant 234 U enrichments in the polar and inland seas during periods of climatic warming in the Late Pleistocene and Holocene. In the bottom sediments of Lake Baikal, the 234 U/ 238 U ratio also increases during warm periods and significantly exceeds the 234 U excess of the World Ocean. Furthermore, the 234 U/ 238 U ratio in the water of Lake Baikal and its tributaries increases from north to south following a decrease in the area of the continuous permafrost and has a seasonal variation with a maximum 234 U/ 238 U ratio in summer. The behavior of 234 U in large water reservoirs is consistent with the hypothesis about the decisive influence of permafrost degradation on the anomalies in 234 U/ 238 U ratios in groundwater. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Water 13 24 3514 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
non-equilibrium uranium 234 U/ 238 U ratio climate variations permafrost World Ocean Lake Baikal Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 |
spellingShingle |
non-equilibrium uranium 234 U/ 238 U ratio climate variations permafrost World Ocean Lake Baikal Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 Igor Tokarev Evgeny Yakovlev Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes |
topic_facet |
non-equilibrium uranium 234 U/ 238 U ratio climate variations permafrost World Ocean Lake Baikal Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 |
description |
In natural water, as a rule, there is a violation of radioactive equilibrium in the chain 238 U … → 234 U → 230 Th →. Groundwater usually has a 234 U/ 238 U ratio in the range of 0.8–3.0 (by activity). However, in some regions, the 234 U/ 238 U ratio reaches >10 and up to 50. Ultrahigh excesses of 234 U can be explained by climatic variations. During a cold period, minerals accumulate 234 U as a normal component of the radioactive chain, and after the melting of permafrost, it is lost from the mineral lattice faster than 238 U due to its higher geochemical mobility. This hypothesis was tested using data on the isotopic composition of uranium in the chemo- and bio-genic formations of the World Ocean and large lakes, which are reservoirs that accumulate continental runoff. The World Ocean has the most significant 234 U enrichments in the polar and inland seas during periods of climatic warming in the Late Pleistocene and Holocene. In the bottom sediments of Lake Baikal, the 234 U/ 238 U ratio also increases during warm periods and significantly exceeds the 234 U excess of the World Ocean. Furthermore, the 234 U/ 238 U ratio in the water of Lake Baikal and its tributaries increases from north to south following a decrease in the area of the continuous permafrost and has a seasonal variation with a maximum 234 U/ 238 U ratio in summer. The behavior of 234 U in large water reservoirs is consistent with the hypothesis about the decisive influence of permafrost degradation on the anomalies in 234 U/ 238 U ratios in groundwater. |
format |
Article in Journal/Newspaper |
author |
Igor Tokarev Evgeny Yakovlev |
author_facet |
Igor Tokarev Evgeny Yakovlev |
author_sort |
Igor Tokarev |
title |
Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes |
title_short |
Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes |
title_full |
Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes |
title_fullStr |
Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes |
title_full_unstemmed |
Non-Equilibrium Uranium as an Indicator of Global Climate Variations—The World Ocean and Large Lakes |
title_sort |
non-equilibrium uranium as an indicator of global climate variations—the world ocean and large lakes |
publisher |
MDPI AG |
publishDate |
2021 |
url |
https://doi.org/10.3390/w13243514 https://doaj.org/article/dda64165690e4d17ae1bed4fed07c1ff |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Water, Vol 13, Iss 3514, p 3514 (2021) |
op_relation |
https://www.mdpi.com/2073-4441/13/24/3514 https://doaj.org/toc/2073-4441 doi:10.3390/w13243514 2073-4441 https://doaj.org/article/dda64165690e4d17ae1bed4fed07c1ff |
op_doi |
https://doi.org/10.3390/w13243514 |
container_title |
Water |
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13 |
container_issue |
24 |
container_start_page |
3514 |
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1766165519678832640 |