Analysis of Influence Factors of Pore Water Pressure Change in Frozen Soil

In this article, changes of pore water pressures (PWP) in silty clay subjected to freezing and thawing were measured under an open-system condition. A total of five soil samples were tested, with water contents of 10.70%, 18.28%, 23.98%, 31.00%, and 37.65%, respectively. Each experienced a first-ste...

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Main Authors: Kun Zhang, Lianhai Zhang
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2021/3290831
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author Kun Zhang
Lianhai Zhang
author_facet Kun Zhang
Lianhai Zhang
author_sort Kun Zhang
collection DOAJ
description In this article, changes of pore water pressures (PWP) in silty clay subjected to freezing and thawing were measured under an open-system condition. A total of five soil samples were tested, with water contents of 10.70%, 18.28%, 23.98%, 31.00%, and 37.65%, respectively. Each experienced a first-step freezing stage, a thawing stage, and a second-step freezing stage. The results showed that changes in PWP depended on the water content, soil type, salinity, ice content, air, pressure, temperature, and others. The PWP minimum with initial water content has a “w-shaped double-valley” characteristic, which described two PWP minima existing in two optimum water contents as initial water content increased. An influence-factor analysis of PWP was proposed and gave a reasonable interpretation on the “w-shaped double-valley” characteristic of PWP. In addition, the tensiometer method to measure PWP in frozen soil was further discussed with regard to its advantages and disadvantages.
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spelling doaj-art-53631fd88a5d422ba2edfa35642864c42025-02-03T01:24:51ZengWileyAdvances in Materials Science and Engineering1687-84341687-84422021-01-01202110.1155/2021/32908313290831Analysis of Influence Factors of Pore Water Pressure Change in Frozen SoilKun Zhang0Lianhai Zhang1Gansu Transportation Research Institute Group Co.,Ltd., Lanzhou 730000, ChinaState Key Laboratory of Frozen Soil Engineering, Chinese Academy of Sciences, Lanzhou 730000, ChinaIn this article, changes of pore water pressures (PWP) in silty clay subjected to freezing and thawing were measured under an open-system condition. A total of five soil samples were tested, with water contents of 10.70%, 18.28%, 23.98%, 31.00%, and 37.65%, respectively. Each experienced a first-step freezing stage, a thawing stage, and a second-step freezing stage. The results showed that changes in PWP depended on the water content, soil type, salinity, ice content, air, pressure, temperature, and others. The PWP minimum with initial water content has a “w-shaped double-valley” characteristic, which described two PWP minima existing in two optimum water contents as initial water content increased. An influence-factor analysis of PWP was proposed and gave a reasonable interpretation on the “w-shaped double-valley” characteristic of PWP. In addition, the tensiometer method to measure PWP in frozen soil was further discussed with regard to its advantages and disadvantages.http://dx.doi.org/10.1155/2021/3290831
spellingShingle Kun Zhang
Lianhai Zhang
Analysis of Influence Factors of Pore Water Pressure Change in Frozen Soil
Advances in Materials Science and Engineering
title Analysis of Influence Factors of Pore Water Pressure Change in Frozen Soil
title_full Analysis of Influence Factors of Pore Water Pressure Change in Frozen Soil
title_fullStr Analysis of Influence Factors of Pore Water Pressure Change in Frozen Soil
title_full_unstemmed Analysis of Influence Factors of Pore Water Pressure Change in Frozen Soil
title_short Analysis of Influence Factors of Pore Water Pressure Change in Frozen Soil
title_sort analysis of influence factors of pore water pressure change in frozen soil
url http://dx.doi.org/10.1155/2021/3290831
work_keys_str_mv AT kunzhang analysisofinfluencefactorsofporewaterpressurechangeinfrozensoil
AT lianhaizhang analysisofinfluencefactorsofporewaterpressurechangeinfrozensoil