Abstract
We consider the combined effects of suction and transverse anisotropy on the instability of the uniform thickness boundary layer which is formed on an inclined heated surface in a porous medium. When the medium is isotropic, the stability characteristics are shown to be very similar to that of the inclined Darcy-Benard problem. In particular, longitudinal rolls are always preferred, and transverse rolls are always stable when the inclination of the surface is greater than approximately 31.9°. Transverse anisotropy has no effect on the identity of the preferred mode of convection whenever the anisotropy parameter, ξ, is less than unity. When ξ > 1, there always exists a range of surface inclinations where transverse rolls are preferred. A detailed set of numerical results are given showing how the critical Rayleigh number and wavenumber vary with both inclination and ξ. © 2002 Published by The Japan Society of Fluid Mechanics and Elsevier Science B.V. All rights reserved.
| Original language | English |
|---|---|
| Pages (from-to) | 155-168 |
| Number of pages | 14 |
| Journal | Fluid Dynamics Research |
| Volume | 30 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - 2002 |
Keywords
- Anisotropy
- Fluid dynamics
- Porous materials
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