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In relation to this article, we declare that there is no conflict of interest.
Publication history
Received July 18, 2009
Accepted October 24, 2009
articles This is an Open-Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/bync/3.0) which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.
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Onset of buoyancy-driven convection in isotropic porous media heated from below

Department of Chemical Engineering, Jeju National University, Jeju 690-756, Korea
mckim@cheju.ac.kr
Korean Journal of Chemical Engineering, March 2010, 27(3), 741-747(7), 10.1007/s11814-010-0149-z
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Abstract

A theoretical analysis of buoyancy-driven instability under transient basic fields is conducted in an initially quiescent, fluid-saturated, horizontal, isotropic porous layer. Darcy’s law is employed to explain characteristics of fluid motion, and Boussinesq approximation is used to consider the density variation. Under the principle of exchange of stabilities, a stability analysis is conducted based on the linear stability analysis and energy method and their modifications. The critical condition of onset of buoyancy-driven convection is obtained as a function of the Darcy-Rayleigh_x000D_ number. The propagation theory and the modified energy method under the self-similar coordinate suggest reasonable stability criteria and support each other. The former one based on the linear stability theory predicts more stable results than the latter based on the energy method. The growth period for disturbances to grow seems to be required until the instabilities are detected experimentally.

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