Theoretical and numerical analyses of pore-fluid flow focused heat transfer around geological faults and large cracks
Theoretical and numerical analyses of pore-fluid flow focused heat transfer around geological faults and large cracks
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DOI:
10.1016/j.compgeo.2007.06.011
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发表时间:
2008-05
影响因子:
5.3
通讯作者:
Chong-bin Zhao;Chong-bin Zhao;B. Hobbs;A. Ord;P. Hornby;H. Muhlhaus;S. Peng
中科院分区:
文献类型:
--
作者:
Chong-bin Zhao;Chong-bin Zhao;B. Hobbs;A. Ord;P. Hornby;H. Muhlhaus;S. Peng
In this paper, theoretical and numerical methods are used to investigate pore-fluid flow focused temperature distribution patterns around geological faults and cracks of any length-scales in hydrothermal systems. If the far field inflow is uniform and the long axis of an elliptical fault of any length-scale is parallel to the far field inflow direction, a complete set of analytical solutions has been presented for the pore-fluid velocity, stream function and excess pore-fluid pressure around the elliptical fault embedded in fluid-saturated porous media. Because the analytical solutions are explicitly expressed in the conventional Cartesian coordinate system, not only can they be used to gain a theoretical insight into the pore-fluid flow patterns around geological faults and large cracks, but also they can be used as valuable benchmark solutions for validating any numerical methods. After a finite element computational model is validated by comparing the numerical solutions with the present analytical solutions, it is used to investigate pore-fluid flow focused heat transfer around geological faults in hydrothermal systems. Some interesting conclusions in relation to the effects of geological faults on pore-fluid flow focused heat transfer have been made through both the theoretical and the numerical analyses.