Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada

Determinations of the tritium (3H) content of ground ice collected near Mayo, Yukon Territory, indicate that since the mid-1950s atmospheric water has infiltrated permafrost to depths of up to 50cm. The rate of tritium infiltration into permafrost at two plots irrigated with tritiated water in 1983...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Burn, C. (Christopher R.), Michel, F.A. (F. A.)
Format: Article in Journal/Newspaper
Language:English
Published: 1988
Subjects:
Ice
Online Access:https://ir.library.carleton.ca/pub/22842
https://doi.org/10.1139/e88-087
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spelling ftcarletonunivir:oai:carleton.ca:22842 2023-05-15T16:36:39+02:00 Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada Burn, C. (Christopher R.) Michel, F.A. (F. A.) 1988-01-01 https://ir.library.carleton.ca/pub/22842 https://doi.org/10.1139/e88-087 en eng https://ir.library.carleton.ca/pub/22842 doi:10.1139/e88-087 Canadian Journal of Earth Sciences vol. 25 no. 6, pp. 909-915 info:eu-repo/semantics/article 1988 ftcarletonunivir https://doi.org/10.1139/e88-087 2022-02-06T21:51:35Z Determinations of the tritium (3H) content of ground ice collected near Mayo, Yukon Territory, indicate that since the mid-1950s atmospheric water has infiltrated permafrost to depths of up to 50cm. The rate of tritium infiltration into permafrost at two plots irrigated with tritiated water in 1983 suggests that tritium movement is principally due to temperature-induced mass transport rather than molecular diffusion. -Authors Article in Journal/Newspaper Ice Mayo permafrost Yukon Carleton University's Institutional Repository Yukon Canada Canadian Journal of Earth Sciences 25 6 909 915
institution Open Polar
collection Carleton University's Institutional Repository
op_collection_id ftcarletonunivir
language English
description Determinations of the tritium (3H) content of ground ice collected near Mayo, Yukon Territory, indicate that since the mid-1950s atmospheric water has infiltrated permafrost to depths of up to 50cm. The rate of tritium infiltration into permafrost at two plots irrigated with tritiated water in 1983 suggests that tritium movement is principally due to temperature-induced mass transport rather than molecular diffusion. -Authors
format Article in Journal/Newspaper
author Burn, C. (Christopher R.)
Michel, F.A. (F. A.)
spellingShingle Burn, C. (Christopher R.)
Michel, F.A. (F. A.)
Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada
author_facet Burn, C. (Christopher R.)
Michel, F.A. (F. A.)
author_sort Burn, C. (Christopher R.)
title Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada
title_short Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada
title_full Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada
title_fullStr Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada
title_full_unstemmed Evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near Mayo, Yukon Territory, Canada
title_sort evidence for recent temperature-induced water migration into permafrost from the tritium content of ground ice near mayo, yukon territory, canada
publishDate 1988
url https://ir.library.carleton.ca/pub/22842
https://doi.org/10.1139/e88-087
geographic Yukon
Canada
geographic_facet Yukon
Canada
genre Ice
Mayo
permafrost
Yukon
genre_facet Ice
Mayo
permafrost
Yukon
op_source Canadian Journal of Earth Sciences vol. 25 no. 6, pp. 909-915
op_relation https://ir.library.carleton.ca/pub/22842
doi:10.1139/e88-087
op_doi https://doi.org/10.1139/e88-087
container_title Canadian Journal of Earth Sciences
container_volume 25
container_issue 6
container_start_page 909
op_container_end_page 915
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