Fully coupled thermo-hydro-mechanical modeling and simulation of a fluid-saturated porous medium under local thermal non-equilibrium condition

被引:10
|
作者
Li, Peichao [1 ]
Yue, Feilong [1 ]
Wang, Keyong [1 ]
Zhang, Hengyun [1 ]
Huang, Haibo [2 ]
Kong, Xiangyan [2 ]
机构
[1] Shanghai Univ Engn Sci, Sch Mech & Automot Engn, Shanghai 201620, Peoples R China
[2] Univ Sci & Technol China, Dept Modern Mech, Hefei 230026, Peoples R China
基金
上海市自然科学基金;
关键词
Fluid-saturated porous media; Compressible porous media; Fully coupled THM model; Local thermal non-equilibrium; Numerical analysis; DEVELOPING FORCED-CONVECTION; HEAT-TRANSFER; THERMOPOROELASTIC RESPONSE; VARIABLE POROSITY; CIRCULAR TUBE; EQUILIBRIUM; DISPERSION; BOREHOLE; ANNULUS; FLOW;
D O I
10.1016/j.ijheatmasstransfer.2022.123195
中图分类号
O414.1 [热力学];
学科分类号
摘要
This paper presents a fully coupled thermo-hydro-mechanical (THM) model of a fluid-saturated and compressible porous medium under local thermal non-equilibrium (LTNE) condition and carries out the corresponding numerical simulation. First, the coupling among the temperature field, the pore fluid pressure field, and the solid stress/displacement field is fulfilled by means of strong explicit coupling of governing equations in this study. Then, the presented model is applied to the THM coupling problem in an infinite porous medium with a cylindrical borehole subjected to uniform fluid pressure and temperature at the borehole boundary. Subsequently, the partial differential equations (PDEs) module in COMSOL Multiphysics software is employed to numerically solve the studied problem. Consequently, the finite element solutions of the pore fluid pressure field, the strain/stress fields and the two temperature fields of pore fluid and skeleton solid are obtained, and the spatial-temporal distribution characteristics of the above multi-physical fields are investigated. Finally, the corresponding parametric studies are carried out. The numerical results show that the stress decreases with the increase of the bulk volumetric thermal expansion coefficient of porous media. And the pore pressure decreases when the pore fluid mobility increases. Meanwhile, it is found in this work that the solid temperature is always higher than that of pore fluid due to the LTNE effect. Besides, with increasing the specific solid-fluid interfacial heat transfer coefficient, the solid temperature decreases, while the temperature of pore fluid increases. Accordingly, the temperature difference between the solid and the pore fluid diminishes. In addition, the thermal conductivity of solid grains has a greater impact on the solid temperature but has a limited impact on the temperature of pore fluid, and vice versa. The findings in this work are of benefit to obtain in-depth understanding of THM fully coupling mechanism and LTNE effect in a fluid-saturated porous medium. (C) 2022 Elsevier Ltd. All rights reserved.
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页数:15
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