Melting-refreezing at the glacier sole and the isotopic composition of the ice
A model for the isotopic composition in δD and δ18O of ice formed by refreezing at the glacier sole is developed. This model predicts relatively well the distribution of points representing samples from basal layers of an Arctic and an Alpine glacier on δD-δ18O a diagram. The frozen fraction which i...
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ftunivbruxelles:oai:dipot.ulb.ac.be:2013/173116 2023-05-15T14:58:20+02:00 Melting-refreezing at the glacier sole and the isotopic composition of the ice Jouzel, Jean Souchez, Roland 1982 No full-text files http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/173116 en eng http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/173116 Journal of Glaciology, 28 (98 Glaciologie info:eu-repo/semantics/article info:ulb-repo/semantics/articlePeerReview info:ulb-repo/semantics/openurl/article 1982 ftunivbruxelles 2022-06-12T20:35:45Z A model for the isotopic composition in δD and δ18O of ice formed by refreezing at the glacier sole is developed. This model predicts relatively well the distribution of points representing samples from basal layers of an Arctic and an Alpine glacier on δD-δ18O a diagram. The frozen fraction which is the part of the liquid that refreezes can be determined for each basal ice layer. This may have implications on the study of the ice-water system at the ice-rock interface. info:eu-repo/semantics/published Article in Journal/Newspaper Arctic Journal of Glaciology DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) Arctic |
institution |
Open Polar |
collection |
DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) |
op_collection_id |
ftunivbruxelles |
language |
English |
topic |
Glaciologie |
spellingShingle |
Glaciologie Jouzel, Jean Souchez, Roland Melting-refreezing at the glacier sole and the isotopic composition of the ice |
topic_facet |
Glaciologie |
description |
A model for the isotopic composition in δD and δ18O of ice formed by refreezing at the glacier sole is developed. This model predicts relatively well the distribution of points representing samples from basal layers of an Arctic and an Alpine glacier on δD-δ18O a diagram. The frozen fraction which is the part of the liquid that refreezes can be determined for each basal ice layer. This may have implications on the study of the ice-water system at the ice-rock interface. info:eu-repo/semantics/published |
format |
Article in Journal/Newspaper |
author |
Jouzel, Jean Souchez, Roland |
author_facet |
Jouzel, Jean Souchez, Roland |
author_sort |
Jouzel, Jean |
title |
Melting-refreezing at the glacier sole and the isotopic composition of the ice |
title_short |
Melting-refreezing at the glacier sole and the isotopic composition of the ice |
title_full |
Melting-refreezing at the glacier sole and the isotopic composition of the ice |
title_fullStr |
Melting-refreezing at the glacier sole and the isotopic composition of the ice |
title_full_unstemmed |
Melting-refreezing at the glacier sole and the isotopic composition of the ice |
title_sort |
melting-refreezing at the glacier sole and the isotopic composition of the ice |
publishDate |
1982 |
url |
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/173116 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Journal of Glaciology |
genre_facet |
Arctic Journal of Glaciology |
op_source |
Journal of Glaciology, 28 (98 |
op_relation |
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/173116 |
_version_ |
1766330421457453056 |