Creep Characteristic Test and Creep Model of Frozen Soil

In order to research the creep deformation characteristics of frozen soil and the effect of various influencing factors on creep, indoor uniaxial creep tests were carried out on frozen soil specimens at temperatures of −5, −4, −3 and −2 °C under loads of 0.25, 0.5, and 0.75 σt, respectively. The cre...

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Published in:Sustainability
Main Authors: Yawu Shao, Yonglu Suo, Jiang Xiao, Yuan Bai, Tao Yang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Ice
Online Access:https://doi.org/10.3390/su15053984
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spelling ftmdpi:oai:mdpi.com:/2071-1050/15/5/3984/ 2023-08-20T04:07:07+02:00 Creep Characteristic Test and Creep Model of Frozen Soil Yawu Shao Yonglu Suo Jiang Xiao Yuan Bai Tao Yang agris 2023-02-22 application/pdf https://doi.org/10.3390/su15053984 EN eng Multidisciplinary Digital Publishing Institute Hazards and Sustainability https://dx.doi.org/10.3390/su15053984 https://creativecommons.org/licenses/by/4.0/ Sustainability; Volume 15; Issue 5; Pages: 3984 frozen soil creep properties decay creep creep constitutive equation Text 2023 ftmdpi https://doi.org/10.3390/su15053984 2023-08-01T08:56:18Z In order to research the creep deformation characteristics of frozen soil and the effect of various influencing factors on creep, indoor uniaxial creep tests were carried out on frozen soil specimens at temperatures of −5, −4, −3 and −2 °C under loads of 0.25, 0.5, and 0.75 σt, respectively. The creep deformation characteristics of frozen soil under different temperatures and load conditions are analyzed under unconfined conditions. The results show that under the uniaxial creep test conditions, when the load is low, there is no accelerated creep stage in the creep curve, which belongs to the decaying type creep; when the load is 0.75 σt, the creep curve enters the stage of accelerated creep, and the creep turns non-attenuated; temperature is the most important external factor affecting permafrost soil creep, and the proportion of ice is the key internal factor for affecting permafrost soil creep, the temperature is negatively correlated with the proportion of ice and the sensitivity of creep rate to temperature and load increases with the decrease of the proportion of ice; the damage variable D is introduced to modify the creep constitutive equation of the frozen soil, the creep process of frozen soil is well described by the modified creep constitutive equation for frozen soil. Text Ice permafrost MDPI Open Access Publishing Sustainability 15 5 3984
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic frozen soil
creep properties
decay creep
creep constitutive equation
spellingShingle frozen soil
creep properties
decay creep
creep constitutive equation
Yawu Shao
Yonglu Suo
Jiang Xiao
Yuan Bai
Tao Yang
Creep Characteristic Test and Creep Model of Frozen Soil
topic_facet frozen soil
creep properties
decay creep
creep constitutive equation
description In order to research the creep deformation characteristics of frozen soil and the effect of various influencing factors on creep, indoor uniaxial creep tests were carried out on frozen soil specimens at temperatures of −5, −4, −3 and −2 °C under loads of 0.25, 0.5, and 0.75 σt, respectively. The creep deformation characteristics of frozen soil under different temperatures and load conditions are analyzed under unconfined conditions. The results show that under the uniaxial creep test conditions, when the load is low, there is no accelerated creep stage in the creep curve, which belongs to the decaying type creep; when the load is 0.75 σt, the creep curve enters the stage of accelerated creep, and the creep turns non-attenuated; temperature is the most important external factor affecting permafrost soil creep, and the proportion of ice is the key internal factor for affecting permafrost soil creep, the temperature is negatively correlated with the proportion of ice and the sensitivity of creep rate to temperature and load increases with the decrease of the proportion of ice; the damage variable D is introduced to modify the creep constitutive equation of the frozen soil, the creep process of frozen soil is well described by the modified creep constitutive equation for frozen soil.
format Text
author Yawu Shao
Yonglu Suo
Jiang Xiao
Yuan Bai
Tao Yang
author_facet Yawu Shao
Yonglu Suo
Jiang Xiao
Yuan Bai
Tao Yang
author_sort Yawu Shao
title Creep Characteristic Test and Creep Model of Frozen Soil
title_short Creep Characteristic Test and Creep Model of Frozen Soil
title_full Creep Characteristic Test and Creep Model of Frozen Soil
title_fullStr Creep Characteristic Test and Creep Model of Frozen Soil
title_full_unstemmed Creep Characteristic Test and Creep Model of Frozen Soil
title_sort creep characteristic test and creep model of frozen soil
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/su15053984
op_coverage agris
genre Ice
permafrost
genre_facet Ice
permafrost
op_source Sustainability; Volume 15; Issue 5; Pages: 3984
op_relation Hazards and Sustainability
https://dx.doi.org/10.3390/su15053984
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/su15053984
container_title Sustainability
container_volume 15
container_issue 5
container_start_page 3984
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