Short-Term Rheology of Polycrystalline Ice

Abstract Deformation characteristics of polycrystalline ice and their dependence on time, temperature, and stress have been analysed on the basis of a phenomenological relation which describes creep in terms of initial elastic, delayed elastic, and permanent strain. It is shown that the effective mo...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Sinha, N. K.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s002214300003361x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003361X
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spelling crcambridgeupr:10.1017/s002214300003361x 2024-05-19T07:43:13+00:00 Short-Term Rheology of Polycrystalline Ice Sinha, N. K. 1978 http://dx.doi.org/10.1017/s002214300003361x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003361X en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 457-474 ISSN 0022-1430 1727-5652 journal-article 1978 crcambridgeupr https://doi.org/10.1017/s002214300003361x 2024-05-02T06:51:17Z Abstract Deformation characteristics of polycrystalline ice and their dependence on time, temperature, and stress have been analysed on the basis of a phenomenological relation which describes creep in terms of initial elastic, delayed elastic, and permanent strain. It is shown that the effective modulus of ice observed in the laboratory or in the field can be examined on the basis of this model. The model also provides a basis on which the observed flow law of ice can be examined conveniently. Some apparent inconsistencies in the results of earlier investigations of the mechanical property of ice appear of be reconciled by the model. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 457 474
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Deformation characteristics of polycrystalline ice and their dependence on time, temperature, and stress have been analysed on the basis of a phenomenological relation which describes creep in terms of initial elastic, delayed elastic, and permanent strain. It is shown that the effective modulus of ice observed in the laboratory or in the field can be examined on the basis of this model. The model also provides a basis on which the observed flow law of ice can be examined conveniently. Some apparent inconsistencies in the results of earlier investigations of the mechanical property of ice appear of be reconciled by the model.
format Article in Journal/Newspaper
author Sinha, N. K.
spellingShingle Sinha, N. K.
Short-Term Rheology of Polycrystalline Ice
author_facet Sinha, N. K.
author_sort Sinha, N. K.
title Short-Term Rheology of Polycrystalline Ice
title_short Short-Term Rheology of Polycrystalline Ice
title_full Short-Term Rheology of Polycrystalline Ice
title_fullStr Short-Term Rheology of Polycrystalline Ice
title_full_unstemmed Short-Term Rheology of Polycrystalline Ice
title_sort short-term rheology of polycrystalline ice
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s002214300003361x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003361X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 457-474
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s002214300003361x
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 457
op_container_end_page 474
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