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...

Full description

Bibliographic Details
Main Authors: Hindshaw, RS, Aciego, SM, Tipper, ET
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media SA 2018
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.30423
https://www.repository.cam.ac.uk/handle/1810/283061
id ftdatacite:10.17863/cam.30423
record_format openpolar
spelling 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