Numerical Analysis on Feasibility of Thermally Induced Pore Fluid Flow in Saturated Soils
Numerical Analysis on Feasibility of Thermally Induced Pore Fluid Flow in Saturated Soils
复制标题
饱和土中热致孔隙流体流动的可行性数值分析
DOI:
10.1061/9780784482124.009
复制
发表时间:
2019
期刊:
影响因子:
--
通讯作者:
Ghasemi-Fare, Omid
中科院分区:
文献类型:
--
作者:
Tamizdoust, Mohammadreza Mir;Ghasemi-Fare, Omid
The exact heat transfer mechanism in the soil media can be understood by analyzing the soil behavior surrounding the heat sources. In literature, heat conduction has been considered as a main heat transfer mechanism in soil, and less attention has been given to the natural heat convection in saturated soils. There is only limited research in the literature which shows the presence of thermally induced pore fluid flow in soil media. It has been observed that heat convection through pore fluid flow in sand facilitates heat transfer in the ground. Therefore, both heat conduction and heat convection must be considered to accurately model the heat transfer mechanism in soil. In this paper, the presence of natural convection of water in a 2D axisymmetric domain of soil with a vertical heat source has been numerically investigated in steady-state condition. The soil thermal response and heat transfer mechanism for different soil types are compared. Feasibility of thermally-induced pore fluid flow is analyzed for different soil types. The results determine the presence of thermally driven pore fluid flow in high permeability soil (e.g., coarse sand) and confirm that the effect of heat convection in low permeability silt and clay is negligible.
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DOI:
10.1108/09615530010338196
发表时间:
2000-01-01
影响因子:
4.2
作者:
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通讯作者:
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影响因子:
1.6
作者:
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通讯作者:
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DOI:
10.1061/9780784480472.012
发表时间:
2017-03
期刊:
--
影响因子:
--
作者:
Omid Ghasemi-Fare;P. Basu
通讯作者:
Omid Ghasemi-Fare;P. Basu
DOI:
10.1680/ijpmg.2004.040303
发表时间:
2004
影响因子:
1.9
作者:
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通讯作者:
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DOI:
--
发表时间:
2016
期刊:
影响因子:
--
作者:
Omid Ghasemi;P. Basu
通讯作者:
P. Basu