NATURAL CONVECTION BELOW A DOWNWARD FACING HEATED HORIZONTAL SURFACE IN A FLUID-SATURATED POROUS MEDIUM

Abstract

The nature of natural convection under a downward facing horizontal surface in a vast fluid-saturated porous medium is numerically studied. The two-dimensional flow is considered to be symmetric about the mid-vertical plane under the surface, and numerical calculations are presented for one half of the domain. The flow and thermal fields demonstrate no boundary layer behavior, and hence similarity and integral analyses are not possible. A layer of thermally stratified fluid grows under the central region of the surface, which inhibits flow. Convection picks up toward the edges of the surface, where the heat transfer rates are consequently high. The average Nusselt number (based on the total length of the surface) is correlated as Nu = 1.142Ra^0-37 in the range 30  Ra  1000. The structure of the thermal and flow fields under the heated surface in a porous medium is explained.

Notes

Address correspondence to Prof. G. P. Peterson, Office of the Dean of Engineering, Texas A & M University, 301 Weisenbaker Engineering Research Center, College Station, TX 77843-3126, USA.