Direct shear tests of materials from a cold glacier: Implications for landform development

The mechanical properties of materials at the ice-bed interface exert a major control on glacier behaviour and define the nature and rate of subglacial erosion. This paper presents new data on the strength and behaviour of basal ice and substrate of the Suess Glacier, south Victoria Land, Antarctica...

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Main Authors: Fitzsimons, Sean, McManus, Kevin J, Sirota, Paul, Lorrain, Reginald
Format: Article in Journal/Newspaper
Language:English
Published: 2001
Subjects:
Online Access:http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/94724
https://dipot.ulb.ac.be/dspace/bitstream/2013/94724/1/Elsevier_73518.pdf
id ftunivbruxelles:oai:dipot.ulb.ac.be:2013/94724
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spelling ftunivbruxelles:oai:dipot.ulb.ac.be:2013/94724 2023-05-15T13:35:46+02:00 Direct shear tests of materials from a cold glacier: Implications for landform development Fitzsimons, Sean McManus, Kevin J Sirota, Paul Lorrain, Reginald 2001 1 full-text file(s): application/pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/94724 https://dipot.ulb.ac.be/dspace/bitstream/2013/94724/1/Elsevier_73518.pdf en eng uri/info:doi/10.1016/S1040-6182(01)00055-6 uri/info:pii/S1040618201000556 uri/info:scp/0035652489 https://dipot.ulb.ac.be/dspace/bitstream/2013/94724/1/Elsevier_73518.pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/94724 1 full-text file(s): info:eu-repo/semantics/restrictedAccess Quaternary international, 86 Glaciologie info:eu-repo/semantics/article info:ulb-repo/semantics/articlePeerReview info:ulb-repo/semantics/openurl/article 2001 ftunivbruxelles 2022-06-12T20:30:28Z The mechanical properties of materials at the ice-bed interface exert a major control on glacier behaviour and define the nature and rate of subglacial erosion. This paper presents new data on the strength and behaviour of basal ice and substrate of the Suess Glacier, south Victoria Land, Antarctica which is a small alpine dry-based glacier that has a basal temperature of -17°C. A tunnel excavated in the glacier revealed a substrate composed of frozen sand and gravel and a basal zone that was 3.8-m-thick. From bottom to top, the basal zone was composed of 1.8 m of stratified, complexly deformed layers of ice and debris-laden ice that was overlain by a 0.9-m-thick layer of frozen sediment and a 0.8-m-thick layer of discoloured ice that lies immediately beneath clean glacier ice. Direct shear tests were performed in the field on 36 samples using a strain rate of 0.85 mm/h and on replicate samples in a laboratory at strain rates of 0.08 and 0.01 mm/h. The experiments performed in the field show that the average peak shear strength of substrate samples was 2.53 MPa, which is almost twice as strong as the average value for basal ice (1.28 MPa), and the glacier ice samples (1.39 MPa). The laboratory experiments show that the behaviour and peak strength of samples sheared at the higher strain rates are considerably greater than the peak and residual strengths measured during the lower strain rate tests. The direct shear tests suggest that the glacier substrate is unlikely to deform at the current temperature. © 2001 Published by Elsevier Science Ltd. SCOPUS: ar.j info:eu-repo/semantics/published Article in Journal/Newspaper Antarc* Antarctica Suess Glacier Victoria Land DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) Suess Glacier ENVELOPE(162.667,162.667,-77.633,-77.633) Victoria Land
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
Fitzsimons, Sean
McManus, Kevin J
Sirota, Paul
Lorrain, Reginald
Direct shear tests of materials from a cold glacier: Implications for landform development
topic_facet Glaciologie
description The mechanical properties of materials at the ice-bed interface exert a major control on glacier behaviour and define the nature and rate of subglacial erosion. This paper presents new data on the strength and behaviour of basal ice and substrate of the Suess Glacier, south Victoria Land, Antarctica which is a small alpine dry-based glacier that has a basal temperature of -17°C. A tunnel excavated in the glacier revealed a substrate composed of frozen sand and gravel and a basal zone that was 3.8-m-thick. From bottom to top, the basal zone was composed of 1.8 m of stratified, complexly deformed layers of ice and debris-laden ice that was overlain by a 0.9-m-thick layer of frozen sediment and a 0.8-m-thick layer of discoloured ice that lies immediately beneath clean glacier ice. Direct shear tests were performed in the field on 36 samples using a strain rate of 0.85 mm/h and on replicate samples in a laboratory at strain rates of 0.08 and 0.01 mm/h. The experiments performed in the field show that the average peak shear strength of substrate samples was 2.53 MPa, which is almost twice as strong as the average value for basal ice (1.28 MPa), and the glacier ice samples (1.39 MPa). The laboratory experiments show that the behaviour and peak strength of samples sheared at the higher strain rates are considerably greater than the peak and residual strengths measured during the lower strain rate tests. The direct shear tests suggest that the glacier substrate is unlikely to deform at the current temperature. © 2001 Published by Elsevier Science Ltd. SCOPUS: ar.j info:eu-repo/semantics/published
format Article in Journal/Newspaper
author Fitzsimons, Sean
McManus, Kevin J
Sirota, Paul
Lorrain, Reginald
author_facet Fitzsimons, Sean
McManus, Kevin J
Sirota, Paul
Lorrain, Reginald
author_sort Fitzsimons, Sean
title Direct shear tests of materials from a cold glacier: Implications for landform development
title_short Direct shear tests of materials from a cold glacier: Implications for landform development
title_full Direct shear tests of materials from a cold glacier: Implications for landform development
title_fullStr Direct shear tests of materials from a cold glacier: Implications for landform development
title_full_unstemmed Direct shear tests of materials from a cold glacier: Implications for landform development
title_sort direct shear tests of materials from a cold glacier: implications for landform development
publishDate 2001
url http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/94724
https://dipot.ulb.ac.be/dspace/bitstream/2013/94724/1/Elsevier_73518.pdf
long_lat ENVELOPE(162.667,162.667,-77.633,-77.633)
geographic Suess Glacier
Victoria Land
geographic_facet Suess Glacier
Victoria Land
genre Antarc*
Antarctica
Suess Glacier
Victoria Land
genre_facet Antarc*
Antarctica
Suess Glacier
Victoria Land
op_source Quaternary international, 86
op_relation uri/info:doi/10.1016/S1040-6182(01)00055-6
uri/info:pii/S1040618201000556
uri/info:scp/0035652489
https://dipot.ulb.ac.be/dspace/bitstream/2013/94724/1/Elsevier_73518.pdf
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/94724
op_rights 1 full-text file(s): info:eu-repo/semantics/restrictedAccess
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