화학공학소재연구정보센터
Transport in Porous Media, Vol.80, No.2, 399-400, 2009
Further Comments on "Combined Forced and Free Convective Flow in a Vertical Porous Channel: The Effects of Viscous Dissipation and Pressure Work"
This note is concerned with the assertion of Barletta and Nield (2009a) that "a fluid with a thermal expansion coefficient greater than that of a perfect gas (beta > beta (perfect gas)) is of marginal or no interest in the framework of convection in porous media", and that for a remark of Magyari (Transp. Porous Media, 2009) about the forced convection eigenflow solutions, the circumstance beta > beta (perfect gas) does not represent "a sound physical basis". Here, it is shown, however, that these assertions are in contradiction with the experimentally measured values of beta for important technical fluids as e.g., air, nitrogen, carbon dioxide, and ammonia where, in the temperature range between -20 and +100A degrees C, just the inequality beta > beta (perfect gas) holds.