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...

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Bibliographic Details
Published in:Canadian Geotechnical Journal
Main Author: McRoberts, Edward C.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1975
Subjects:
Ice
Online Access:http://dx.doi.org/10.1139/t75-008
http://www.nrcresearchpress.com/doi/pdf/10.1139/t75-008
id crcansciencepubl:10.1139/t75-008
record_format openpolar
spelling 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
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