Abstract
The effect of surface mass tranfer on the buoyancy-induced flow in a varibale-porosity medium adjacent to a horizontal heated plate is studied. Similary solutions are obtained for a power law variation in surface temperature, T w∝ χ λ , and surface blowing, v w∝χ (λ−2)/3 , for a wide range of parameters that define the ratio of solid to fluid thermal conductivity, b. It is shown for the case of uniform surface mass transfer (λ=2) that the variable porosity model in general predicts a higher surface heat flux compared to the uniform porosity model. This increased heat flux depends strongly on the quantity b.
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More From: International Communications in Heat and Mass Transfer
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