Precise Solution to 3D Coupled Thermohydromechanical Problems of Layered Transversely Isotropic Saturated Porous Media

被引:21
作者
Ai, Zhi Yong [1 ]
Wang, Lu Jun [1 ,2 ]
机构
[1] Tongji Univ, Dept Geotech Engn, Coll Civil Engn, Key Lab Geotech & Underground Engn,Minist Educ, 1239 Siping Rd, Shanghai 200092, Peoples R China
[2] Zhejiang Univ, Minist Educ, Key Lab Soft Soils & Geoenviron Engn, Inst Geotech Engn, Hangzhou 310058, Zhejiang, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Thermohydromechanical coupling; Transverse isotropy; Layered porous media; Precise-integration method; Integral transform; DECAYING HEAT-SOURCE; POROELASTIC HALF-SPACE; COMPRESSIBLE CONSTITUENTS; 3-DIMENSIONAL CONSOLIDATION; INTEGRATION METHOD; NUMERICAL-METHOD; SURFACE LOADS; BEHAVIOR; MODEL; ROCK;
D O I
10.1061/(ASCE)GM.1943-5622.0001027
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
This paper presents a precise solution to coupled thermohydromechanical problems of layered, transversely isotropic, saturated, porous media with a heat source or a temperature increment with the aid of integral transform techniques. On the basis of governing equations of three-dimensional (3D) coupled thermohydromechanical problems of saturated porous media, a standard differential matrix equation was deduced by using the Laplace-Fourier transform. In this paper, an extended precise-integration method for a layered system with an internal or surface load is introduced. It was used to solve the previous standard differential equation in the transformed domain. Real solutions in the physical domain were obtained by using the numerical inversion of the Laplace-Fourier transform. The precision of the presented theory was confirmed by two examples, and the effects of the anisotropic permeability and the transverse isotropic characteristics on the thermohydromechanical coupling behavior of layered saturated media are described.
引用
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页数:11
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