Natural convection from a Plane Vertical Porous Surface in Non Isothermal
Articles
S. C. Saha
IBAIS University, Bangladesh
Published 2004-04-25
https://doi.org/10.15388/NA.2004.9.2.15164
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Keywords

porous surface
non-isothermal surroundings
body force

How to Cite

Saha, S.C. (2004) “Natural convection from a Plane Vertical Porous Surface in Non Isothermal”, Nonlinear Analysis: Modelling and Control, 9(2), pp. 151–170. doi:10.15388/NA.2004.9.2.15164.

Abstract

In this paper, laminar natural convection flow from a permeable and isothermal vertical surface placed in non-isothermal surroundings is considered. Introducing appropriate transformations into the boundary layer equations governing the flow derives non-similar boundary layer equations. Results of both the analytical and numerical solutions are then presented in the form of skin-friction and Nusselt number. Numerical solutions of the transformed non-similar boundary layer equations are obtained by three distinct solution methods, (i) the perturbation solutions for small ξ (ii) the asymptotic solution for large ξ (iii) the implicit finite difference method for all ξ where ξ is the transpiration parameter. Perturbation solutions for small and large values of ξ are compared with the finite difference solutions for different values of pertinent parameters, namely, the Prandtl number Pr, and the ambient temperature gradient n.

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