Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ...
Permafrost in the Arctic is decreasing in extent and the depth of the seasonally thawed layer, the active layer, is increasing. Increased exposure to water is increasing fluxes of organic and inorganic solutes with potential impacts for the global carbon cycle and downstream ecosystems. Understandin...
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Online Access: | https://dx.doi.org/10.17863/cam.30423 https://www.repository.cam.ac.uk/handle/1810/283061 |
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ftdatacite:10.17863/cam.30423 2024-02-04T09:57:45+01:00 Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ... Hindshaw, RS Aciego, SM Tipper, ET 2018 https://dx.doi.org/10.17863/cam.30423 https://www.repository.cam.ac.uk/handle/1810/283061 en eng Frontiers Media SA open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 permafrost Arctic lithium isotopes uranium isotopes geochemistry weathering active-layer glacier Article ScholarlyArticle JournalArticle article-journal 2018 ftdatacite https://doi.org/10.17863/cam.30423 2024-01-05T10:03:29Z Permafrost in the Arctic is decreasing in extent and the depth of the seasonally thawed layer, the active layer, is increasing. Increased exposure to water is increasing fluxes of organic and inorganic solutes with potential impacts for the global carbon cycle and downstream ecosystems. Understanding the relationship between solute release and active layer depth will be critical for modeling environmental impact, especially in inaccessible regions where there is a lack of data. In this study, we focus on the potential for the isotopes of lithium (Li) and uranium (U) to track active layer extent in two permafrost-dominated catchments in Svalbard: one glaciated and one unglaciated. These isotope systems can be measured to a much higher precision than concentration measurements and act as sensitive tracers of environmental change. The extent of Li isotope fractionation provides information on the balance between dissolution of primary phases and formation of secondary phases, such as clay minerals and oxides. ... Article in Journal/Newspaper Arctic glacier permafrost Svalbard DataCite Metadata Store (German National Library of Science and Technology) Arctic Svalbard |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
permafrost Arctic lithium isotopes uranium isotopes geochemistry weathering active-layer glacier |
spellingShingle |
permafrost Arctic lithium isotopes uranium isotopes geochemistry weathering active-layer glacier Hindshaw, RS Aciego, SM Tipper, ET Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ... |
topic_facet |
permafrost Arctic lithium isotopes uranium isotopes geochemistry weathering active-layer glacier |
description |
Permafrost in the Arctic is decreasing in extent and the depth of the seasonally thawed layer, the active layer, is increasing. Increased exposure to water is increasing fluxes of organic and inorganic solutes with potential impacts for the global carbon cycle and downstream ecosystems. Understanding the relationship between solute release and active layer depth will be critical for modeling environmental impact, especially in inaccessible regions where there is a lack of data. In this study, we focus on the potential for the isotopes of lithium (Li) and uranium (U) to track active layer extent in two permafrost-dominated catchments in Svalbard: one glaciated and one unglaciated. These isotope systems can be measured to a much higher precision than concentration measurements and act as sensitive tracers of environmental change. The extent of Li isotope fractionation provides information on the balance between dissolution of primary phases and formation of secondary phases, such as clay minerals and oxides. ... |
format |
Article in Journal/Newspaper |
author |
Hindshaw, RS Aciego, SM Tipper, ET |
author_facet |
Hindshaw, RS Aciego, SM Tipper, ET |
author_sort |
Hindshaw, RS |
title |
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ... |
title_short |
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ... |
title_full |
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ... |
title_fullStr |
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ... |
title_full_unstemmed |
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments ... |
title_sort |
li and u isotopes as a potential tool for monitoring active layer deepening in permafrost dominated catchments ... |
publisher |
Frontiers Media SA |
publishDate |
2018 |
url |
https://dx.doi.org/10.17863/cam.30423 https://www.repository.cam.ac.uk/handle/1810/283061 |
geographic |
Arctic Svalbard |
geographic_facet |
Arctic Svalbard |
genre |
Arctic glacier permafrost Svalbard |
genre_facet |
Arctic glacier permafrost Svalbard |
op_rights |
open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.30423 |
_version_ |
1789962086596476928 |