Triaxial stress path tests on artificially prepared analogue alpine permafrost soil

Some degrading rock glaciers have been exhibiting deepening depressions, accelerating strain rates, and, in some rare cases, sudden release of mass movements. Warming permafrost already mobilizes lower strength as temperatures rise; however, unusual stress paths with lateral stresses greater than ve...

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Bibliographic Details
Main Authors: Yamamoto, Yuko, Springman, Sarah M.
Format: Article in Journal/Newspaper
Language:English
French
Published: Canadian Science Publishing 2019
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/371438
https://doi.org/10.3929/ethz-b-000371438
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/371438
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/371438 2023-08-15T12:42:47+02:00 Triaxial stress path tests on artificially prepared analogue alpine permafrost soil Yamamoto, Yuko Springman, Sarah M. 2019-10 application/application/pdf https://hdl.handle.net/20.500.11850/371438 https://doi.org/10.3929/ethz-b-000371438 en fr eng fre Canadian Science Publishing info:eu-repo/semantics/altIdentifier/doi/10.1139/cgj-2017-0737 info:eu-repo/semantics/altIdentifier/wos/000488768000007 http://hdl.handle.net/20.500.11850/371438 doi:10.3929/ethz-b-000371438 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International Canadian Geotechnical Journal, 56 (10) permafrost frozen soil shear strength triaxial stress path testing acoustic emissions info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftethz https://doi.org/20.500.11850/37143810.3929/ethz-b-00037143810.1139/cgj-2017-0737 2023-07-23T23:46:31Z Some degrading rock glaciers have been exhibiting deepening depressions, accelerating strain rates, and, in some rare cases, sudden release of mass movements. Warming permafrost already mobilizes lower strength as temperatures rise; however, unusual stress paths with lateral stresses greater than vertical stresses, instead of vice versa, could exacerbate this condition with lower strength at failure, and hence higher vulnerability. This paper investigates the mechanical behaviour of artificially frozen soil specimens at temperatures between –3.0 and –0.3 °C under various stress paths: axial (A) and lateral (L), compression (C), and extension (E), for total stress paths AC, AE, LE, LC. Acoustic emissions were detected during shearing to expose how the deformation mechanisms develop from a microstructural point of view. Deviatoric stress mobilized in the stress path tests was linearly dependent on the temperature (within the ranges tested): a temperature increase resulted in a decrease in residual deviatoric stress. Comparison between the residual deviatoric stresses obtained from the different stress path tests indicates that (i) values mobilized with radial stress greater than axial stress were lower than vice versa, (ii) more strength was mobilized when changing lateral stress paths than axial, with (iii) the lowest strength mobilized in AE beneath a depression. ISSN:0008-3674 ISSN:1208-6010 Article in Journal/Newspaper permafrost ETH Zürich Research Collection
institution Open Polar
collection ETH Zürich Research Collection
op_collection_id ftethz
language English
French
topic permafrost
frozen soil
shear strength
triaxial stress path testing
acoustic emissions
spellingShingle permafrost
frozen soil
shear strength
triaxial stress path testing
acoustic emissions
Yamamoto, Yuko
Springman, Sarah M.
Triaxial stress path tests on artificially prepared analogue alpine permafrost soil
topic_facet permafrost
frozen soil
shear strength
triaxial stress path testing
acoustic emissions
description Some degrading rock glaciers have been exhibiting deepening depressions, accelerating strain rates, and, in some rare cases, sudden release of mass movements. Warming permafrost already mobilizes lower strength as temperatures rise; however, unusual stress paths with lateral stresses greater than vertical stresses, instead of vice versa, could exacerbate this condition with lower strength at failure, and hence higher vulnerability. This paper investigates the mechanical behaviour of artificially frozen soil specimens at temperatures between –3.0 and –0.3 °C under various stress paths: axial (A) and lateral (L), compression (C), and extension (E), for total stress paths AC, AE, LE, LC. Acoustic emissions were detected during shearing to expose how the deformation mechanisms develop from a microstructural point of view. Deviatoric stress mobilized in the stress path tests was linearly dependent on the temperature (within the ranges tested): a temperature increase resulted in a decrease in residual deviatoric stress. Comparison between the residual deviatoric stresses obtained from the different stress path tests indicates that (i) values mobilized with radial stress greater than axial stress were lower than vice versa, (ii) more strength was mobilized when changing lateral stress paths than axial, with (iii) the lowest strength mobilized in AE beneath a depression. ISSN:0008-3674 ISSN:1208-6010
format Article in Journal/Newspaper
author Yamamoto, Yuko
Springman, Sarah M.
author_facet Yamamoto, Yuko
Springman, Sarah M.
author_sort Yamamoto, Yuko
title Triaxial stress path tests on artificially prepared analogue alpine permafrost soil
title_short Triaxial stress path tests on artificially prepared analogue alpine permafrost soil
title_full Triaxial stress path tests on artificially prepared analogue alpine permafrost soil
title_fullStr Triaxial stress path tests on artificially prepared analogue alpine permafrost soil
title_full_unstemmed Triaxial stress path tests on artificially prepared analogue alpine permafrost soil
title_sort triaxial stress path tests on artificially prepared analogue alpine permafrost soil
publisher Canadian Science Publishing
publishDate 2019
url https://hdl.handle.net/20.500.11850/371438
https://doi.org/10.3929/ethz-b-000371438
genre permafrost
genre_facet permafrost
op_source Canadian Geotechnical Journal, 56 (10)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1139/cgj-2017-0737
info:eu-repo/semantics/altIdentifier/wos/000488768000007
http://hdl.handle.net/20.500.11850/371438
doi:10.3929/ethz-b-000371438
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_doi https://doi.org/20.500.11850/37143810.3929/ethz-b-00037143810.1139/cgj-2017-0737
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