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首页> 外文期刊>International Journal of Solids and Structures >Effective thermal conductivity of transversely isotropic media with arbitrary oriented ellipsoidal inhomogeneities
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Effective thermal conductivity of transversely isotropic media with arbitrary oriented ellipsoidal inhomogeneities

机译:具有任意取向的椭圆不均匀性的横观各向同性介质的有效导热系数

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摘要

The objective of this work is to investigate the thermal conduction phenomena in transversely isotropic geomaterials or rock-like composites with arbitrary oriented ellipsoidal inhomogeneities of low aspect ratio. Based on the evaluation of the Green function, we provide here new expressions for the interaction tensor whose knowledge permits to obtain the concentration tensor of the polarization field used itself to evaluate the effective thermal conductivity tensor by homogenization. Some particular cases of the obtained general solution are equally presented, in order to validate the developed formalism. The obtained results are next used to study the effect of matrix anisotropy, pores systems and microstructure-related parameters on the overall effective thermal conductivity in transversely isotropic rocks. A two-step homogenization scheme is developed for the prediction of the initial anisotropy effects and to test the ability of the proposed model in the evaluation of effective thermal conductivity. With the help of an Orientation Distribution Function (ODF) the anisotropy due to the pore systems is also accounted. Numerical applications and comparisons with available experimental data are finally carried out for a partially saturated Opalinus clay and an argillite which are both composed of an argillaceous matrix and multiple solid minerals constituents. (c) 2006 Elsevier Ltd. All rights reserved.
机译:这项工作的目的是研究具有低长宽比的任意取向的椭圆不均匀性的横向各向同性的土工材料或类岩石复合材料中的热传导现象。基于格林函数的评估,我们在这里为相互作用张量提供了新的表达式,其知识允许获得偏振场的浓度张量,该浓度张量本身用于通过均质化来评估有效导热率张量。为了验证所开发的形式主义,将平均地介绍所获得的一般解决方案的一些特殊情况。接下来,将获得的结果用于研究基质各向同性,孔隙系统和微结构相关参数对横观各向同性岩石整体有效导热率的影响。开发了两步均化方案,用于预测初始各向异性效应,并测试提出的模型在评估有效导热率方面的能力。借助于取向分布函数(ODF),还可以考虑由于孔隙系统引起的各向异性。最后,对部分饱和的蛋白石粘土和泥锌矿进行了数值应用,并将其与可用的实验数据进行了比较,二者均由泥质基质和多种固体矿物成分组成。 (c)2006 Elsevier Ltd.保留所有权利。

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