Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw Cycles

Due to climate warming and large-scale engineering activities, the embankment engineering risk in the permafrost and seasonally frozen regions caused by water content change in the soil has become more and more serious. To study the moisture migration law in the embankment under the vehicle load act...

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Main Authors: Yongting Huang, Wei Ma, Donghui Xiao, Yuezhen Xu
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2021/5541130
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author Yongting Huang
Wei Ma
Donghui Xiao
Yuezhen Xu
author_facet Yongting Huang
Wei Ma
Donghui Xiao
Yuezhen Xu
author_sort Yongting Huang
collection DOAJ
description Due to climate warming and large-scale engineering activities, the embankment engineering risk in the permafrost and seasonally frozen regions caused by water content change in the soil has become more and more serious. To study the moisture migration law in the embankment under the vehicle load action and periodic variation of temperature, a series of temperature-controlled model tests under the dynamic load condition were carried out, the dynamic load was imposed by an air hammer connecting a vibration plate, which was installed on the top surface of the soil, and the variation law of the temperature and moisture fields in the model was analyzed. The test results show that the moisture field in the soil sample changes obviously with the increasing freeze-thaw cycles under the no-load condition, especially after nine freeze-thaw cycles, two moisture accumulation areas appear in the range of 8–15 cm from the soil surface; the dynamic load has an inhibitory effect on the moisture migration within 5 cm below the vibration plate and has a promoting effect on the range of 10–30 cm below the vibration plate. With the increase in the number of freeze-thaw cycles, three high-water content areas are gradually formed and approximately uniformly distributed within the 10–25 cm depth range of the soil, which has an important impact on the stability of the soil. The water content of the moisture accumulation areas during freezing is greater than that during thawing under the no-load condition, while the water content of the moisture accumulation areas during freezing is less than that during thawing under dynamic load. The research results can provide references for the embankment design and disease treatment in cold regions.
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spelling doaj-art-80e1b7c99e294560b709d95a1bcdbd652025-08-20T03:35:07ZengWileyAdvances in Materials Science and Engineering1687-84422021-01-01202110.1155/2021/5541130Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw CyclesYongting Huang0Wei Ma1Donghui Xiao2Yuezhen Xu3State Key Laboratory of Frozen Soil EngineeringState Key Laboratory of Frozen Soil EngineeringPoly Changda Engineering Company LimitedState Key Laboratory of Frozen Soil EngineeringDue to climate warming and large-scale engineering activities, the embankment engineering risk in the permafrost and seasonally frozen regions caused by water content change in the soil has become more and more serious. To study the moisture migration law in the embankment under the vehicle load action and periodic variation of temperature, a series of temperature-controlled model tests under the dynamic load condition were carried out, the dynamic load was imposed by an air hammer connecting a vibration plate, which was installed on the top surface of the soil, and the variation law of the temperature and moisture fields in the model was analyzed. The test results show that the moisture field in the soil sample changes obviously with the increasing freeze-thaw cycles under the no-load condition, especially after nine freeze-thaw cycles, two moisture accumulation areas appear in the range of 8–15 cm from the soil surface; the dynamic load has an inhibitory effect on the moisture migration within 5 cm below the vibration plate and has a promoting effect on the range of 10–30 cm below the vibration plate. With the increase in the number of freeze-thaw cycles, three high-water content areas are gradually formed and approximately uniformly distributed within the 10–25 cm depth range of the soil, which has an important impact on the stability of the soil. The water content of the moisture accumulation areas during freezing is greater than that during thawing under the no-load condition, while the water content of the moisture accumulation areas during freezing is less than that during thawing under dynamic load. The research results can provide references for the embankment design and disease treatment in cold regions.http://dx.doi.org/10.1155/2021/5541130
spellingShingle Yongting Huang
Wei Ma
Donghui Xiao
Yuezhen Xu
Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw Cycles
Advances in Materials Science and Engineering
title Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw Cycles
title_full Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw Cycles
title_fullStr Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw Cycles
title_full_unstemmed Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw Cycles
title_short Influence of Dynamic Load on Soil Moisture Field in the Process of Freeze-Thaw Cycles
title_sort influence of dynamic load on soil moisture field in the process of freeze thaw cycles
url http://dx.doi.org/10.1155/2021/5541130
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AT weima influenceofdynamicloadonsoilmoisturefieldintheprocessoffreezethawcycles
AT donghuixiao influenceofdynamicloadonsoilmoisturefieldintheprocessoffreezethawcycles
AT yuezhenxu influenceofdynamicloadonsoilmoisturefieldintheprocessoffreezethawcycles