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...

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Published in:Annals of Glaciology
Main Authors: Miyamoto, Atsushi, Narita, Hideki, Hondoh, Takeo, Shoji, Hitoshi, Kawada, Kunio, Watanabe, Okitsugu, Dahl-Jensen, Dorthe, Gundestrup, Niels Steen, Clausen, Henrik Brink, Duval, Paul
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
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
id ftcopenhagenunip:oai:pure.atira.dk:publications/be45faa0-74c8-11db-bee9-02004c4f4f50
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spelling 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
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