Oberbeck convection through vertical porous stratum

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Rudraiah, N. and Venkatachalappa, M. and Malashetty, M.S. (1982) Oberbeck convection through vertical porous stratum. Proceedings of the Indian Academy of Sciences - Mathematical Sciences, 91 (1). pp. 17-37. ISSN 0973-7685

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Official URL: https://doi.org/10.1007/BF02837258

Abstract

Natural convection through a vertical porous stratum is investigated both analytically and numerically. Analytical solutions are obtained using a perturbation method valid for small values of buoyancy parameter N and the numerical solutions are obtained using Runge-Kutta-Gill method. It is shown that analytical solutions are valid for N < 1 and several features of the effect of large values of N are reported. The combined effects of increase in the values of temperature difference between the plates and the permeability parameter on velocity, temperature, mass flow rate and the rate of heat transfer are reported. It is shown that higher temperature difference is required to achieve the mass flow rate in a porous medium equivalent to that of viscous flow. © 1982 Indian Academy of Sciences.

Item Type: Article
Additional Information: cited By 9
Subjects: Faculty of Science > Pure Sciences > Mathematics
Divisions: Jnana Bharathi / Central College Campus > Department of Mathematics
Depositing User: Mr. Kirana Kumar D
Date Deposited: 25 Jan 2016 10:31
Last Modified: 25 Feb 2016 10:43
URI: http://eprints-bangaloreuniversity.in/id/eprint/162

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