Skip Navigation

The Quarterly Journal of Mechanics and Applied Mathematics 1985 38(2):277-295; doi:10.1093/qjmam/38.2.277
© 1985 by Oxford University Press
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to My Personal Archive
Right arrow Download to citation manager
Right arrowRequest Permissions
Google Scholar
Right arrow Articles by RILEY, D. S.
Right arrow Articles by REES, D. A. S.
Right arrow Search for Related Content
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

NON-DARCY NATURAL CONVECTION FROM ARBITRARILY INCLINED HEATED SURFACES IN SATURATED POROUS MEDIA

D. S. RILEY and D. A. S. REES

( 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 {alpha}. The flow is induced by the heated surface, which is at an angle {delta} to the gravity vector, where -1/{pi} <{delta}lequal1/2{pi} 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 {alpha} {delta} and G.


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?




Disclaimer:
Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.