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首页> 外文期刊>International journal of geomechanics >Precise Solution to 3D Coupled Thermohydromechanical Problems of Layered Transversely Isotropic Saturated Porous Media
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Precise Solution to 3D Coupled Thermohydromechanical Problems of Layered Transversely Isotropic Saturated Porous Media

机译:层状横观各向同性饱和多孔介质的3D耦合热流体力学问题的精确解

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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.
机译:本文提出了一种精确的解决方案,借助积分变换技术可以解决带有热源或温度升高的层状,横向各向同性的饱和多孔介质的耦合热流体力学问题。基于饱和多孔介质三维(3D)耦合热流体力学问题的控制方程,利用拉普拉斯-傅里叶变换推导了标准微分矩阵方程。在本文中,介绍了具有内部或表面载荷的分层系统的扩展精确积分方法。它被用来求解变换域中以前的标准微分方程。通过使用Laplace-Fourier变换的数值反演获得物理域中的实际解。通过两个例子证实了所提出理论的精度,并描述了各向异性渗透率和横向各向同性特性对层状饱和介质热-机械耦合行为的影响。

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