Effect of anisotropy in permeability on thermal convection of viscoelastic fluids in rotating porous layer heated from below

dc.contributor.authorYOVOGAN, JULIEN
dc.contributor.authorMIWADINOU, Clément
dc.contributor.authorVODOUNNOU, Edmond
dc.date.accessioned2026-06-02T16:06:57Z
dc.date.available2026-06-02T16:06:57Z
dc.date.issued2018
dc.description.abstractIn this work, we studied the linear stability analyses of thermal convection, in a viscoelastic fluid saturated rotating anisotropic porous layer heated from below. The influence of hydrodynamic anisotropy and of rotation on the convective phenomenon are considered and investigated by extending the modified Darcy-Maxwell-Jeffrey model to include the Coriolis force term. It is shown that the anisotropic permeability ratio K, the inclination angle of the principal axes (φ) of the porous medium, the relaxation time (ε), the retardation time (ζ) and the Taylor Darcy number (TD) have a strong influence on the convective flow.
dc.identifier.doi10.1080/14484846.2018.1523294
dc.identifier.otherBECDB-14463
dc.identifier.urihttps://dspace.uac.bj/handle/123456789/12339
dc.language.isofr
dc.relation.ispartofAUSTRALIAN JOURNAL OF MECHANICAL ENGINEERING
dc.subjectConvection heat transfer
dc.subjectanisotropy
dc.subjectrotating
dc.subjectanisotropic porous layer
dc.subjectviscoelastic fluid
dc.titleEffect of anisotropy in permeability on thermal convection of viscoelastic fluids in rotating porous layer heated from below
dc.typeArticle

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