Effects of anisotropy in permeability on the two-phase flow and heat transfer in a porous cavity |
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Authors: | X. L. Zhang T. Hung Nguyen R. Kahawita |
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Affiliation: | Départment de Génie Mécanique Ecole affilée á L’Université de Montréal 2500, Chemin de Polytechnique Montréal (Québec) H3T 107, Canada, CA Ecole Polytechnique de Montréal Montréal (Québec), H3C 3A7, Canada, CA
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Abstract: | This paper reports on the results of a numerical study of convection flow and heat transfer in a rectangular porous cavity filled with a phase change material under steady state conditions. The two vertical walls of the cavity are subject respectively to temperatures below and above the melting point of the PCM while adiabatic conditions are imposed on the horizontal walls. The porous medium is characterized by an anisotropic permeability tensor with the principal axes arbitrarily oriented with respect to the gravity vector. The problem is governed by the aspect ratioA, the Rayleigh numberRa, the anisotropy ratioR and the orientation angle θ of the permeability tensor. Attention is focused on these two latter parameters in order to investigate the effects of the anisotropic permeability on the fluid flow and heat transfer of the liquid/solid phase change process. The method of solution is based on the control volume approach in conjunction with the Landau-transformation to map the irregular flow domain into a rectangular one. The results are obtained for the flow field, temperature distribution, interface position and heat transfer rate forA=2.5,Ra=40, 0≤θ≤π, 0.25≤R≤4. It was found that the equilibrium state of the solid/liquid phase change process may be strongly influenced by the anisotropy ratioR as well as by the orientation angle θ of the permeability tensor. First, for a given set of parametersA,Ra andR, there exists an optimum orientation θmax for which the flow strength, the liquid volume and the heat transfer rate are maximum. There also exists an orientation θmin=θmax+π/2 for which these quantities are minimum. Second, when an anisotropic medium is oriented along the optimum direction θmax, an increase of the permeability component along that direction will increase the flow and heat transfer rate in a same order while an increase of the other permeability component only has a negligible effect. For the parameter ranges considered in the present study, it was found that the optimum direction is lying between the gravity vector and the dominant flow direction. |
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