Effects of buoyancy assisting and opposing flows on mixed convection boundary layer flow over a permeable vertical surface
โ Scribed by S.V. Subhashini; Nancy Samuel; I. Pop
- Publisher
- Elsevier Science
- Year
- 2011
- Tongue
- English
- Weight
- 560 KB
- Volume
- 38
- Category
- Article
- ISSN
- 0735-1933
No coin nor oath required. For personal study only.
โฆ Synopsis
The present study deals with new similarity solution of steady mixed convection boundary layer flow over a permeable surface for convective boundary condition. It has been shown that a self similar solution is possible when the mass transfer velocity at the surface of the plate varies like x -1/2 , where x is the distance from the leading edge of the solid surface. Two point boundary value problem governed by non-linear coupled ordinary differential equations have been solved numerically using implicit finite difference scheme in combination with the quasi-linearization technique. It is interesting to note that dual solutions exist for buoyancy assisting flow, besides that usually reported in literature for buoyancy opposing flow. Further, the buoyancy assisting force causes considerable overshoot in the velocity profile and the Prandtl number strongly affects the thermal boundary layer thickness including the surface heat transfer rate.
๐ SIMILAR VOLUMES
This work studies the natural convection boundary layer flow of a micropolar fluid near a vertical permeable cone with variable wall temperature. The transformed boundary layer governing equations are solved by the cubic spline collocation method. The local Nusselt numbers are presented as functions
A similarity analysis of the steady free convection boundary layer over vertical and horizontal surfaces embedded in a fluidsaturated porous medium with mixed thermal boundary conditions is performed in this paper. New variables relating the similarity solutions of the Darcian velocity and temperatu
A mathematical model is analyzed in order to study the heat and mass transfer characteristics in mixed convection boundary layer flow about a linearly stretching vertical surface in a porous medium filled with a viscoelastic fluid, by taking into account the diffusionthermo (Dufour) and thermal-diff