Ice-sheet flow conditions deduced from mechanical tests of ice core
Uniaxial compression tests were performed on samples of the Greenland Ice Core Project (GRIP) deep ice core, both in the field and later in a cold-room laboratory, in order to understand the ice-flow behavior of large ice sheets. Experiments were conducted under conditions of constant strain rate (t...
Published in: | Annals of Glaciology |
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Language: | English |
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1999
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Online Access: | https://curis.ku.dk/portal/da/publications/icesheet-flow-conditions-deduced-from-mechanical-tests-of-ice-core(be45faa0-74c8-11db-bee9-02004c4f4f50).html https://doi.org/10.3189/172756499781820950 |
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ftcopenhagenunip:oai:pure.atira.dk:publications/be45faa0-74c8-11db-bee9-02004c4f4f50 2023-12-24T10:08:25+01:00 Ice-sheet flow conditions deduced from mechanical tests of ice core Miyamoto, Atsushi Narita, Hideki Hondoh, Takeo Shoji, Hitoshi Kawada, Kunio Watanabe, Okitsugu Dahl-Jensen, Dorthe Gundestrup, Niels Steen Clausen, Henrik Brink Duval, Paul 1999 https://curis.ku.dk/portal/da/publications/icesheet-flow-conditions-deduced-from-mechanical-tests-of-ice-core(be45faa0-74c8-11db-bee9-02004c4f4f50).html https://doi.org/10.3189/172756499781820950 eng eng info:eu-repo/semantics/restrictedAccess Miyamoto , A , Narita , H , Hondoh , T , Shoji , H , Kawada , K , Watanabe , O , Dahl-Jensen , D , Gundestrup , N S , Clausen , H B & Duval , P 1999 , ' Ice-sheet flow conditions deduced from mechanical tests of ice core ' , Annals of Glaciology , vol. 29 , no. 1 , pp. 179-183 . https://doi.org/10.3189/172756499781820950 article 1999 ftcopenhagenunip https://doi.org/10.3189/172756499781820950 2023-11-29T23:58:28Z Uniaxial compression tests were performed on samples of the Greenland Ice Core Project (GRIP) deep ice core, both in the field and later in a cold-room laboratory, in order to understand the ice-flow behavior of large ice sheets. Experiments were conducted under conditions of constant strain rate (type A) and constant load (type B). Fifty-four uniaxial-compression test specimens from 1327-2922 m were selected. Each test specimen (25 mm × 25 mm × 90 mm) was prepared with its uniaxial stress axis inclined 45° from the core axis in order to examine the flow behavior of strong single-maximum ice-core samples with basal planes parallel to the horizontal plane of the ice sheet. The ice-flow enhancement factors show a gradual increase with depth down to approximately 2000 m. These results can be interpreted in terms of an increase in the fourth-order Schmid factor. Below 2000 m depth, the flow-enhancement factor increases to about 20-30 with a relatively high variability. When the Schmid factor was > 0.46, the enhancement factor obtained was higher than expected from the c -axis concentrations measured. The higher values of flow-enhancement factor were obtained from specimens with a cloudy band structure. It was revealed that cloudy bands affect ice-deformation processes, but the details remain unclear. Udgivelsesdato: June Article in Journal/Newspaper Annals of Glaciology Greenland Greenland ice core Greenland Ice core Project GRIP ice core Ice Sheet University of Copenhagen: Research Greenland Annals of Glaciology 29 179 183 |
institution |
Open Polar |
collection |
University of Copenhagen: Research |
op_collection_id |
ftcopenhagenunip |
language |
English |
description |
Uniaxial compression tests were performed on samples of the Greenland Ice Core Project (GRIP) deep ice core, both in the field and later in a cold-room laboratory, in order to understand the ice-flow behavior of large ice sheets. Experiments were conducted under conditions of constant strain rate (type A) and constant load (type B). Fifty-four uniaxial-compression test specimens from 1327-2922 m were selected. Each test specimen (25 mm × 25 mm × 90 mm) was prepared with its uniaxial stress axis inclined 45° from the core axis in order to examine the flow behavior of strong single-maximum ice-core samples with basal planes parallel to the horizontal plane of the ice sheet. The ice-flow enhancement factors show a gradual increase with depth down to approximately 2000 m. These results can be interpreted in terms of an increase in the fourth-order Schmid factor. Below 2000 m depth, the flow-enhancement factor increases to about 20-30 with a relatively high variability. When the Schmid factor was > 0.46, the enhancement factor obtained was higher than expected from the c -axis concentrations measured. The higher values of flow-enhancement factor were obtained from specimens with a cloudy band structure. It was revealed that cloudy bands affect ice-deformation processes, but the details remain unclear. Udgivelsesdato: June |
format |
Article in Journal/Newspaper |
author |
Miyamoto, Atsushi Narita, Hideki Hondoh, Takeo Shoji, Hitoshi Kawada, Kunio Watanabe, Okitsugu Dahl-Jensen, Dorthe Gundestrup, Niels Steen Clausen, Henrik Brink Duval, Paul |
spellingShingle |
Miyamoto, Atsushi Narita, Hideki Hondoh, Takeo Shoji, Hitoshi Kawada, Kunio Watanabe, Okitsugu Dahl-Jensen, Dorthe Gundestrup, Niels Steen Clausen, Henrik Brink Duval, Paul Ice-sheet flow conditions deduced from mechanical tests of ice core |
author_facet |
Miyamoto, Atsushi Narita, Hideki Hondoh, Takeo Shoji, Hitoshi Kawada, Kunio Watanabe, Okitsugu Dahl-Jensen, Dorthe Gundestrup, Niels Steen Clausen, Henrik Brink Duval, Paul |
author_sort |
Miyamoto, Atsushi |
title |
Ice-sheet flow conditions deduced from mechanical tests of ice core |
title_short |
Ice-sheet flow conditions deduced from mechanical tests of ice core |
title_full |
Ice-sheet flow conditions deduced from mechanical tests of ice core |
title_fullStr |
Ice-sheet flow conditions deduced from mechanical tests of ice core |
title_full_unstemmed |
Ice-sheet flow conditions deduced from mechanical tests of ice core |
title_sort |
ice-sheet flow conditions deduced from mechanical tests of ice core |
publishDate |
1999 |
url |
https://curis.ku.dk/portal/da/publications/icesheet-flow-conditions-deduced-from-mechanical-tests-of-ice-core(be45faa0-74c8-11db-bee9-02004c4f4f50).html https://doi.org/10.3189/172756499781820950 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Annals of Glaciology Greenland Greenland ice core Greenland Ice core Project GRIP ice core Ice Sheet |
genre_facet |
Annals of Glaciology Greenland Greenland ice core Greenland Ice core Project GRIP ice core Ice Sheet |
op_source |
Miyamoto , A , Narita , H , Hondoh , T , Shoji , H , Kawada , K , Watanabe , O , Dahl-Jensen , D , Gundestrup , N S , Clausen , H B & Duval , P 1999 , ' Ice-sheet flow conditions deduced from mechanical tests of ice core ' , Annals of Glaciology , vol. 29 , no. 1 , pp. 179-183 . https://doi.org/10.3189/172756499781820950 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.3189/172756499781820950 |
container_title |
Annals of Glaciology |
container_volume |
29 |
container_start_page |
179 |
op_container_end_page |
183 |
_version_ |
1786199474245206016 |