Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
669916 | International Journal of Thermal Sciences | 2008 | 9 Pages |
The present paper is concerned with mixed convection in a vertical plane parallel channel filled with a porous medium. Steady parallel flow is examined, assuming that the effect of viscous dissipation is significant. Under these assumptions, the governing balance equations admit a first integral, so that the general solution can be given in an exact analytical form in terms of the Weierstrass' elliptic P-function. Based on this general solution and on a suitable parametrization of the problem, a unified approach which applies to all the thermal boundary conditions compatible with the steady parallel flow regime is reported. It is shown that the velocity field can either be unidirectional or bidirectional. Moreover, bidirectional flow configurations are possible also for vanishing average velocity, Um=0. A remarkable feature of the problem is that for Um