Combined Free and Forced Convection in Vertical Channels of Porous Media

In this paper we investigate the combined free and forced convection of a fully developed Newtonian fluid within a vertical channel composed of porous media when viscous dissipation effects are taken into consideration. The flow is analysed in the region of a first critical Rayleigh number in order to interpret the multiple-valued solutions and discuss their validity. The governing fourth-order, ordinary differential equation, which contains the Darcy and the viscous dissipation terms, is solved analytically using perturbation techniques and numerically using D02HBF NAG Library. A detailed investigation of the governing O.D.E. is performed on both clear fluid and porous medium for various values of the viscous dissipation parameter, ε, when the wall temperature decreases linearly with height, and the pressure gradient is both above and below its hydrostatic value. Although mathematically the results in all cases show that there are two solution branches, producing four possible solutions, the study of the velocity and buoyancy profiles together with the Darcy effect indicate that only one of the two solutions at any value of the Rayleigh number appears to be physically acceptable. It is shown that the effect of the Darcy number decreases as the critical Rayleigh numbers increase.

[1]  H. Brinkman,et al.  On the permeability of media consisting of closely packed porous particles , 1949 .

[2]  F. K. Moore,et al.  Theory of laminar flows , 1964 .

[3]  J. L. Lage,et al.  The effect of thermal stratification on natural convection in a vertical porous insulation layer , 1996 .

[4]  D. Kassoy,et al.  Convection fluid dynamics in a model of a fault zone in the earth's crust , 1978, Journal of Fluid Mechanics.

[5]  H. Brinkman A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles , 1949 .

[6]  P. Cheng,et al.  Natural convection heat transfer from a horizontal cylinder embedded in a porous medium , 1986 .

[7]  Derek B. Ingham,et al.  Combined free and forced convection in a porous medium between two vertical walls with viscous dissipation , 1990 .

[8]  D. Nield Resolution of a Paradox Involving Viscous Dissipation and Nonlinear Drag in a Porous Medium , 2000 .

[9]  P. M. Beckett,et al.  Combined natural- and forced-convection between parallel vertical walls , 1980 .

[10]  P. M. Beckett,et al.  Combined natural and forced convection between parallel walls: Developing flow at higher Rayleigh numbers , 1984 .

[11]  B. Morton,et al.  Laminar convection in uniformly heated vertical pipes , 1960, Journal of Fluid Mechanics.

[12]  Simon Ostrach,et al.  Combined natural- and forced-convection laminar flow and heat transfer of fluids with and without heat sources in channels with linearly varying wall temperatures , 1954 .