Onset of convection in porous layers salted from above and below


For a porous layer heated from below and salted from above and below, the non existence of subcritical instabilities and conditions of global stability - for special values of the Prandtl numbers - are found.

DOI Code: 10.1285/i15900932v32n1p159

Keywords: Multi-component fluid mixtures; Porous media; Convection; Stability

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