Creep behaviour of undisturbed clay permafrost

An in situ analysis of naturally occurring creep has been carried out at the proposed Canadian Arctic Gas pipeline crossing of Great Bear River in the Northwest Territories. This is the last of four papers that describe the study. Creep properties of natural and reconstituted frozen soils are briefl...

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Bibliographic Details
Published in:Canadian Geotechnical Journal
Main Authors: Savigny, K. W., Morgenstern, N. R.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1986
Subjects:
Ice
Online Access:http://dx.doi.org/10.1139/t86-081
http://www.nrcresearchpress.com/doi/pdf/10.1139/t86-081
id crcansciencepubl:10.1139/t86-081
record_format openpolar
spelling crcansciencepubl:10.1139/t86-081 2023-12-17T10:25:42+01:00 Creep behaviour of undisturbed clay permafrost Savigny, K. W. Morgenstern, N. R. 1986 http://dx.doi.org/10.1139/t86-081 http://www.nrcresearchpress.com/doi/pdf/10.1139/t86-081 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 23, issue 4, page 515-527 ISSN 0008-3674 1208-6010 Civil and Structural Engineering Geotechnical Engineering and Engineering Geology journal-article 1986 crcansciencepubl https://doi.org/10.1139/t86-081 2023-11-19T13:38:27Z An in situ analysis of naturally occurring creep has been carried out at the proposed Canadian Arctic Gas pipeline crossing of Great Bear River in the Northwest Territories. This is the last of four papers that describe the study. Creep properties of natural and reconstituted frozen soils are briefly reviewed. A laboratory programme to measure creep properties of undisturbed ice-rich glaciolacustrine clay samples from the Great Bear River site is described in detail. The results are analysed to determine empirical parameters for constitutive equations that describe the stress–strain–time behaviour of the material. Key words: Mackenzie Valley, pipelines, slopes, ice-rich, soils, permafrost, geotechnical, creep, laboratory. Article in Journal/Newspaper Arctic Ice Mackenzie Valley Northwest Territories permafrost Canadian Science Publishing (via Crossref) Arctic Northwest Territories Mackenzie Valley ENVELOPE(-126.070,-126.070,52.666,52.666) Great Bear River ENVELOPE(-125.604,-125.604,64.902,64.902) Canadian Geotechnical Journal 23 4 515 527
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
Savigny, K. W.
Morgenstern, N. R.
Creep behaviour of undisturbed clay permafrost
topic_facet Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
description An in situ analysis of naturally occurring creep has been carried out at the proposed Canadian Arctic Gas pipeline crossing of Great Bear River in the Northwest Territories. This is the last of four papers that describe the study. Creep properties of natural and reconstituted frozen soils are briefly reviewed. A laboratory programme to measure creep properties of undisturbed ice-rich glaciolacustrine clay samples from the Great Bear River site is described in detail. The results are analysed to determine empirical parameters for constitutive equations that describe the stress–strain–time behaviour of the material. Key words: Mackenzie Valley, pipelines, slopes, ice-rich, soils, permafrost, geotechnical, creep, laboratory.
format Article in Journal/Newspaper
author Savigny, K. W.
Morgenstern, N. R.
author_facet Savigny, K. W.
Morgenstern, N. R.
author_sort Savigny, K. W.
title Creep behaviour of undisturbed clay permafrost
title_short Creep behaviour of undisturbed clay permafrost
title_full Creep behaviour of undisturbed clay permafrost
title_fullStr Creep behaviour of undisturbed clay permafrost
title_full_unstemmed Creep behaviour of undisturbed clay permafrost
title_sort creep behaviour of undisturbed clay permafrost
publisher Canadian Science Publishing
publishDate 1986
url http://dx.doi.org/10.1139/t86-081
http://www.nrcresearchpress.com/doi/pdf/10.1139/t86-081
long_lat ENVELOPE(-126.070,-126.070,52.666,52.666)
ENVELOPE(-125.604,-125.604,64.902,64.902)
geographic Arctic
Northwest Territories
Mackenzie Valley
Great Bear River
geographic_facet Arctic
Northwest Territories
Mackenzie Valley
Great Bear River
genre Arctic
Ice
Mackenzie Valley
Northwest Territories
permafrost
genre_facet Arctic
Ice
Mackenzie Valley
Northwest Territories
permafrost
op_source Canadian Geotechnical Journal
volume 23, issue 4, page 515-527
ISSN 0008-3674 1208-6010
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/t86-081
container_title Canadian Geotechnical Journal
container_volume 23
container_issue 4
container_start_page 515
op_container_end_page 527
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