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首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >Thermohydromechanics of partially saturated geological media: governing equations and formulation of four finite element models
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Thermohydromechanics of partially saturated geological media: governing equations and formulation of four finite element models

机译:部分饱和地质介质的热流体力学:控制方程和四个有限元模型的表示

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This paper presents the general governing equations for coupled thermohydromechanical (THM) processes in saturated and unsaturated geologic formations and reviews four finite element codes fur modeling of such system. Three of the codes are developed for the special purpose of analyzing coupled THM processes in unsaturated porous and fractured geological media, and the fourth is a commercial code that has been used in its standard version, with a few adaptations for this specialized problem. The basic assumptions and fundamental equations for coupled THM processes in unsaturated porous fractured rock are presented. and formulations of the four finite element models are compared. (C) 2001 Elsevier Science Ltd. All rights reserved. [References: 71]
机译:本文提出了在饱和和非饱和地质构造中耦合热流体力学(THM)过程的一般控制方程,并回顾了该系统的四个有限元编码。开发了其中三个代码,用于分析不饱和多孔和压裂地质介质中耦合THM过程的特殊目的,第四个代码是已在其标准版本中使用的商业代码,针对该特殊问题进行了一些修改。给出了非饱和多孔裂隙岩体中THM耦合过程的基本假设和基本方程。比较了四个有限元模型的公式。 (C)2001 Elsevier ScienceLtd。保留所有权利。 [参考:71]

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