© 1985 by Oxford University Press
NON-DARCY NATURAL CONVECTION FROM ARBITRARILY INCLINED HEATED SURFACES IN SATURATED POROUS MEDIA
( School of Mathematics, University Walk Bristol BS8 1TW )
An analysis is presented of steady free convection in a saturated porous medium bounded by a heated flat surface and a second thermally insulated (or cold) flat surface, which forms a wedge of angle
. The flow is induced by the heated surface, which is at an angle
to the gravity vector, where -1/
<
lequal1/2
The pressure gradient-velocity relation is taken to be nonlinear, with departure from the linear Darey situation measured by a parameter G. Matched asymptotic expansions are employed in analysing two distinct cases: the heated surface is (i) horizontal and (ii) at a finite angle above the horizontal. In the former case the flow is driven along by a buoyancy-induced pressure gradient, whilst in the latter it is the direct action of buoyancy forces that drives the flow. Extensive consideration is given to the effects of varying
and G.