Natural convection in a vertical porous slot heated from below and with horizontal concentration gradients
β Scribed by A. Bahloul; L. Kalla; R. Bennacer; H. Beji; P. Vasseur
- Publisher
- Elsevier Science
- Year
- 2004
- Tongue
- French
- Weight
- 389 KB
- Volume
- 43
- Category
- Article
- ISSN
- 1290-0729
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β¦ Synopsis
Double-diffusive natural convection in a slender vertical porous enclosure is studied both analytically and numerically. The buoyancy forces that induce the fluid motion result from the imposition of both a vertical temperature gradient and a horizontal solutal gradient. The first part of the study contains an analytical solution valid for stratified flows in enclosures with relatively high aspect ratios. The second part of the study contains a numerical study of the full governing equations that validate the analytical model. Comparison between the numerical and analytical solutions covers the thermal Rayleigh number range -6 Γ 10 2 R T 10 4 , the buoyancy range 0 N 10 3 and the Lewis number range 10 -2 Le 10 2 . In the absence of a horizontal solutal gradient (N = 0), the solution takes the form of standard BΓ©nard bifurcation. The asymmetry resulting from the imposition of a small (N 1) horizontal solutal gradient is investigated. The existence of multiple solutions, for a given range of the governing parameters, is demonstrated.
π SIMILAR VOLUMES
The effect of nonun iform permeability and thermal d iffusivity on natural convection through a porous system heated from the side is investigated numerically. The first part of the study, in Section 2, focuses on systems composed of vert ical sublayers. It is shown that the heattransferrate is infl
This paper presents results for coupled heat and mass transport under laminar and turbulent flow regimes in porous cavities. Two driving mechanisms are considered to contribute to the overall momentum transport, namely temperature driven and concentration driven mass fluxes. Aiding and opposing flow