2007
DOI: 10.1016/j.ijsolstr.2006.08.011
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Effective thermal conductivity of transversely isotropic media with arbitrary oriented ellipsoïdal inhomogeneities

Abstract: The objective of this work is to investigate the thermal conduction phenomena in transversely isotropic geomaterials or rock-like composites with arbitrary oriented ellipsoïdal 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 … Show more

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Cited by 84 publications
(43 citation statements)
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“…The solid phase being composed by several minerals with different thermal conductivities, the equivalent grain thermal conductivity is unknown. It can be computed from classical mixing law or homogenization (see Gruescu et al, 2007;Giraud et al, 2007). In the present work, we choose to optimize directly λ S to limit the uncertainties due to additional computations.…”
Section: Application To a Clay-rockmentioning
confidence: 99%
“…The solid phase being composed by several minerals with different thermal conductivities, the equivalent grain thermal conductivity is unknown. It can be computed from classical mixing law or homogenization (see Gruescu et al, 2007;Giraud et al, 2007). In the present work, we choose to optimize directly λ S to limit the uncertainties due to additional computations.…”
Section: Application To a Clay-rockmentioning
confidence: 99%
“…The pore space is assumed to be made of a set of pores that can be described as inclusions of similar ellipsoidal shape (see Sayers, 1994), so there is only one class of pores, approximated by randomly oriented flat oblate spheroidal inclusions with low aspect ratio e % 0.05. The analogous problem for effective thermal conductivity has been presented in Gruescu et al (2007) and Giraud et al (2007a). It may be noticed that, in most cases, sedimentary rocks such as shales and argillites are transversely isotropic (see Giraud et al, 2007b for corresponding estimates of poroelastic coefficients).…”
Section: Porous Rock-like Composites Such As Deep Argillites and Shalesmentioning
confidence: 91%
“…The homogenization theory using RVE is usually carried out to numerically determine the effective properties of composites (Kanit et al 2003;Muliana 2009;Zohdi and Wriggers 2008). Based on the imposed boundary conditions, either the macroscopic flux or the macroscopic gradient field is calculated by averaging or homogenizing the microscopic counterparts, and then the effective property is calculated by using the macroscopic constitutive relationships (Kushch and Chernobai 2014;Giraud et al 2007;Lutz and Zimmerman 2005):q…”
Section: Governing Equations and Boundary Conditionsmentioning
confidence: 99%