Effect of moisture content on frozen ground strength

The authors of this paper have investigated the effect of total moisture content on the uniaxial compressive strength of three frozen soils (supes, suglinok and clay) under short- term loading at temperatures between -10 degrees C and -55 degrees C. Polycrystalline ice specimens were also tested und...

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Bibliographic Details
Main Authors: Shusherina, E. P., Bobkov, Y. P., National Research Council Of Canada. Division Of Building Research
Format: Report
Language:English
Published: National Research Council of Canada 1978
Subjects:
permafrost
soils
frozen soils
moisture content
compressive strength
low degree
pergélisol
sol
sol gelé
degré hygrométrique
résistance à la compression
bas degré
Ice
Online Access:https://dx.doi.org/10.4224/20358850
https://nrc-publications.canada.ca/eng/view/object/?id=61aac962-d4bd-40d9-93fb-cd4e5f24b7bc
id ftdatacite:10.4224/20358850
record_format openpolar
spelling ftdatacite:10.4224/20358850 2023-05-15T16:37:17+02:00 Effect of moisture content on frozen ground strength Shusherina, E. P. Bobkov, Y. P. National Research Council Of Canada. Division Of Building Research 1978 https://dx.doi.org/10.4224/20358850 https://nrc-publications.canada.ca/eng/view/object/?id=61aac962-d4bd-40d9-93fb-cd4e5f24b7bc en eng National Research Council of Canada permafrost soils frozen soils moisture content compressive strength low degree pergélisol sol sol gelé degré hygrométrique résistance à la compression bas degré Text Report report ScholarlyArticle 1978 ftdatacite https://doi.org/10.4224/20358850 2021-11-05T12:55:41Z The authors of this paper have investigated the effect of total moisture content on the uniaxial compressive strength of three frozen soils (supes, suglinok and clay) under short- term loading at temperatures between -10 degrees C and -55 degrees C. Polycrystalline ice specimens were also tested under similar conditions. Report Ice permafrost pergélisol DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic permafrost
soils
frozen soils
moisture content
compressive strength
low degree
pergélisol
sol
sol gelé
degré hygrométrique
résistance à la compression
bas degré
spellingShingle permafrost
soils
frozen soils
moisture content
compressive strength
low degree
pergélisol
sol
sol gelé
degré hygrométrique
résistance à la compression
bas degré
Shusherina, E. P.
Bobkov, Y. P.
National Research Council Of Canada. Division Of Building Research
Effect of moisture content on frozen ground strength
topic_facet permafrost
soils
frozen soils
moisture content
compressive strength
low degree
pergélisol
sol
sol gelé
degré hygrométrique
résistance à la compression
bas degré
description The authors of this paper have investigated the effect of total moisture content on the uniaxial compressive strength of three frozen soils (supes, suglinok and clay) under short- term loading at temperatures between -10 degrees C and -55 degrees C. Polycrystalline ice specimens were also tested under similar conditions.
format Report
author Shusherina, E. P.
Bobkov, Y. P.
National Research Council Of Canada. Division Of Building Research
author_facet Shusherina, E. P.
Bobkov, Y. P.
National Research Council Of Canada. Division Of Building Research
author_sort Shusherina, E. P.
title Effect of moisture content on frozen ground strength
title_short Effect of moisture content on frozen ground strength
title_full Effect of moisture content on frozen ground strength
title_fullStr Effect of moisture content on frozen ground strength
title_full_unstemmed Effect of moisture content on frozen ground strength
title_sort effect of moisture content on frozen ground strength
publisher National Research Council of Canada
publishDate 1978
url https://dx.doi.org/10.4224/20358850
https://nrc-publications.canada.ca/eng/view/object/?id=61aac962-d4bd-40d9-93fb-cd4e5f24b7bc
genre Ice
permafrost
pergélisol
genre_facet Ice
permafrost
pergélisol
op_doi https://doi.org/10.4224/20358850
_version_ 1766027585586724864

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