Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes
This study presents the solution to a simple model for deformations due to secondary creep in permafrost slopes. By introducing a constitutive relationship, or flow law, for ice into the model it is shown that significant creep deformations can occur in frozen slopes. Evidence is reviewed that sugge...
Published in: | Canadian Geotechnical Journal |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1975
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Online Access: | http://dx.doi.org/10.1139/t75-008 http://www.nrcresearchpress.com/doi/pdf/10.1139/t75-008 |
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crcansciencepubl:10.1139/t75-008 2023-12-17T10:31:29+01:00 Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes McRoberts, Edward C. 1975 http://dx.doi.org/10.1139/t75-008 http://www.nrcresearchpress.com/doi/pdf/10.1139/t75-008 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 12, issue 1, page 98-105 ISSN 0008-3674 1208-6010 Civil and Structural Engineering Geotechnical Engineering and Engineering Geology journal-article 1975 crcansciencepubl https://doi.org/10.1139/t75-008 2023-11-19T13:39:25Z This study presents the solution to a simple model for deformations due to secondary creep in permafrost slopes. By introducing a constitutive relationship, or flow law, for ice into the model it is shown that significant creep deformations can occur in frozen slopes. Evidence is reviewed that suggests that secondary creep in ice-rich soils may be faster than that of ice alone. Article in Journal/Newspaper Ice permafrost Canadian Science Publishing (via Crossref) Canadian Geotechnical Journal 12 1 98 105 |
institution |
Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
Civil and Structural Engineering Geotechnical Engineering and Engineering Geology |
spellingShingle |
Civil and Structural Engineering Geotechnical Engineering and Engineering Geology McRoberts, Edward C. Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes |
topic_facet |
Civil and Structural Engineering Geotechnical Engineering and Engineering Geology |
description |
This study presents the solution to a simple model for deformations due to secondary creep in permafrost slopes. By introducing a constitutive relationship, or flow law, for ice into the model it is shown that significant creep deformations can occur in frozen slopes. Evidence is reviewed that suggests that secondary creep in ice-rich soils may be faster than that of ice alone. |
format |
Article in Journal/Newspaper |
author |
McRoberts, Edward C. |
author_facet |
McRoberts, Edward C. |
author_sort |
McRoberts, Edward C. |
title |
Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes |
title_short |
Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes |
title_full |
Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes |
title_fullStr |
Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes |
title_full_unstemmed |
Some Aspects of a Simple Secondary Creep Model for Deformations in Permafrost Slopes |
title_sort |
some aspects of a simple secondary creep model for deformations in permafrost slopes |
publisher |
Canadian Science Publishing |
publishDate |
1975 |
url |
http://dx.doi.org/10.1139/t75-008 http://www.nrcresearchpress.com/doi/pdf/10.1139/t75-008 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
Canadian Geotechnical Journal volume 12, issue 1, page 98-105 ISSN 0008-3674 1208-6010 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/t75-008 |
container_title |
Canadian Geotechnical Journal |
container_volume |
12 |
container_issue |
1 |
container_start_page |
98 |
op_container_end_page |
105 |
_version_ |
1785584789334523904 |