Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated Soils

Based on the thermodynamic and thermoelastic theory, the coupled governing equations of deformation, heat transfer, and moisture migration in unsaturated soils were given. The coupled calculation process was realized by the finite element method. The hydrothermal coupling characteristics of two case...

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Main Authors: Wei Wang, Jingjing Liu, Jing Chen
Format: Article
Language:English
Published: Wiley 2022-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2022/2867985
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author Wei Wang
Jingjing Liu
Jing Chen
author_facet Wei Wang
Jingjing Liu
Jing Chen
author_sort Wei Wang
collection DOAJ
description Based on the thermodynamic and thermoelastic theory, the coupled governing equations of deformation, heat transfer, and moisture migration in unsaturated soils were given. The coupled calculation process was realized by the finite element method. The hydrothermal coupling characteristics of two cases of unsaturated kaolin clay were studied by using a self-developed test device, and the test results were compared with the numerical results. The results showed that when the initial saturation of the soil is high, the volumetric water content of the measured point increases, and then it is in a stable state during the heating process. When the initial saturation is low, the volumetric water content near the heat source increases firstly and then decreases during the heating process. The rise and fall of temperature make the volumetric water content of the soil irreversible. The volumetric water content of each measured point is lower than the initial state. The closer it is to the internal measured heat source, the more obvious this phenomenon is; the lower the initial saturation is, the more obvious it is.
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institution Kabale University
issn 1687-8442
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publishDate 2022-01-01
publisher Wiley
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spelling doaj-art-23372d45547c4ca0bd03c5f7684d9d5b2025-02-03T06:05:32ZengWileyAdvances in Materials Science and Engineering1687-84422022-01-01202210.1155/2022/2867985Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated SoilsWei Wang0Jingjing Liu1Jing Chen2China Hebei Construction and Geotechnical Investigation Group Ltd.China Hebei Construction and Geotechnical Investigation Group Ltd.School of Civil EngineeringBased on the thermodynamic and thermoelastic theory, the coupled governing equations of deformation, heat transfer, and moisture migration in unsaturated soils were given. The coupled calculation process was realized by the finite element method. The hydrothermal coupling characteristics of two cases of unsaturated kaolin clay were studied by using a self-developed test device, and the test results were compared with the numerical results. The results showed that when the initial saturation of the soil is high, the volumetric water content of the measured point increases, and then it is in a stable state during the heating process. When the initial saturation is low, the volumetric water content near the heat source increases firstly and then decreases during the heating process. The rise and fall of temperature make the volumetric water content of the soil irreversible. The volumetric water content of each measured point is lower than the initial state. The closer it is to the internal measured heat source, the more obvious this phenomenon is; the lower the initial saturation is, the more obvious it is.http://dx.doi.org/10.1155/2022/2867985
spellingShingle Wei Wang
Jingjing Liu
Jing Chen
Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated Soils
Advances in Materials Science and Engineering
title Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated Soils
title_full Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated Soils
title_fullStr Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated Soils
title_full_unstemmed Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated Soils
title_short Thermo-Hydromechanical Coupling Responses Driven by a Central Heat Source in Unsaturated Soils
title_sort thermo hydromechanical coupling responses driven by a central heat source in unsaturated soils
url http://dx.doi.org/10.1155/2022/2867985
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AT jingjingliu thermohydromechanicalcouplingresponsesdrivenbyacentralheatsourceinunsaturatedsoils
AT jingchen thermohydromechanicalcouplingresponsesdrivenbyacentralheatsourceinunsaturatedsoils