THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE
An account is given of ice deformation experiments in uniaxial compression. Samples studied include isotropic and anisotropic ice, laboratory prepared and from a core drilled at the summit of Law Dome, Antarctica. There are unexplained differences in the minimum strain rates attained by isotropic ic...
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1987
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Online Access: | https://hal.science/jpa-00226287 https://hal.science/jpa-00226287/document https://hal.science/jpa-00226287/file/ajp-jphyscol198748C141.pdf https://doi.org/10.1051/jphyscol:1987141 |
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ftccsdartic:oai:HAL:jpa-00226287v1 2023-11-12T04:08:20+01:00 THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE Gao, X. Jacka, T. 1987 https://hal.science/jpa-00226287 https://hal.science/jpa-00226287/document https://hal.science/jpa-00226287/file/ajp-jphyscol198748C141.pdf https://doi.org/10.1051/jphyscol:1987141 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.1051/jphyscol:1987141 jpa-00226287 https://hal.science/jpa-00226287 https://hal.science/jpa-00226287/document https://hal.science/jpa-00226287/file/ajp-jphyscol198748C141.pdf doi:10.1051/jphyscol:1987141 info:eu-repo/semantics/OpenAccess Journal de Physique Colloques https://hal.science/jpa-00226287 Journal de Physique Colloques, 1987, 48 (C1), pp.C1-289-C1-296. ⟨10.1051/jphyscol:1987141⟩ [PHYS.HIST]Physics [physics]/Physics archives info:eu-repo/semantics/article Journal articles 1987 ftccsdartic https://doi.org/10.1051/jphyscol:1987141 2023-10-21T23:42:00Z An account is given of ice deformation experiments in uniaxial compression. Samples studied include isotropic and anisotropic ice, laboratory prepared and from a core drilled at the summit of Law Dome, Antarctica. There are unexplained differences in the minimum strain rates attained by isotropic ices from the core and from the laboratory. Minimum strain rates for anisotropic ice are higher than for isotropic ice provided that the anisotropy is compatible with the stress configuration. In tertiary creep a constant strain rate is attained, associated with the development of a small circle girdle crystal orientation fabric, and an equilibrium crystal size. It is proposed that this tertiary creep is steady state. Article in Journal/Newspaper Antarc* Antarctic Antarctica Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Antarctic Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733) |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[PHYS.HIST]Physics [physics]/Physics archives |
spellingShingle |
[PHYS.HIST]Physics [physics]/Physics archives Gao, X. Jacka, T. THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE |
topic_facet |
[PHYS.HIST]Physics [physics]/Physics archives |
description |
An account is given of ice deformation experiments in uniaxial compression. Samples studied include isotropic and anisotropic ice, laboratory prepared and from a core drilled at the summit of Law Dome, Antarctica. There are unexplained differences in the minimum strain rates attained by isotropic ices from the core and from the laboratory. Minimum strain rates for anisotropic ice are higher than for isotropic ice provided that the anisotropy is compatible with the stress configuration. In tertiary creep a constant strain rate is attained, associated with the development of a small circle girdle crystal orientation fabric, and an equilibrium crystal size. It is proposed that this tertiary creep is steady state. |
format |
Article in Journal/Newspaper |
author |
Gao, X. Jacka, T. |
author_facet |
Gao, X. Jacka, T. |
author_sort |
Gao, X. |
title |
THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE |
title_short |
THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE |
title_full |
THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE |
title_fullStr |
THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE |
title_full_unstemmed |
THE APPROACH TO SIMILAR TERTIARY CREEP RATES FOR ANTARCTIC CORE ICE AND LABORATORY PREPARED ICE |
title_sort |
approach to similar tertiary creep rates for antarctic core ice and laboratory prepared ice |
publisher |
HAL CCSD |
publishDate |
1987 |
url |
https://hal.science/jpa-00226287 https://hal.science/jpa-00226287/document https://hal.science/jpa-00226287/file/ajp-jphyscol198748C141.pdf https://doi.org/10.1051/jphyscol:1987141 |
long_lat |
ENVELOPE(112.833,112.833,-66.733,-66.733) |
geographic |
Antarctic Law Dome |
geographic_facet |
Antarctic Law Dome |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
Journal de Physique Colloques https://hal.science/jpa-00226287 Journal de Physique Colloques, 1987, 48 (C1), pp.C1-289-C1-296. ⟨10.1051/jphyscol:1987141⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1051/jphyscol:1987141 jpa-00226287 https://hal.science/jpa-00226287 https://hal.science/jpa-00226287/document https://hal.science/jpa-00226287/file/ajp-jphyscol198748C141.pdf doi:10.1051/jphyscol:1987141 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1051/jphyscol:1987141 |
_version_ |
1782328660276019200 |