Hydromagnetic Radiative Convection Flow in a Vertical Channel With Temperature Dependent Viscosity and Viscous Dissipation and Heat Generation/Absorption

Author:
1N. P. SINGH, 2V. UPADHYAY, 2A. K. AGRAWAL and 2KHILANAND GUPTA
Affiliation:

1Department of Mathematics, CL Jain (PG) College, Firozabad-283203 (INDIA)
2Department of Physical Sciences, MGCG, Vishwavidyalaya, Chitrakoot-485780 (INDIA)

Keyword:
Radiative convection, impermeable walls, vertical channel, viscous dissipation, heat generation/absorption
Issue Date:
August 2014
Abstract:

Fully developed radiative convection flow of an electrically conducting, incompressible viscous liquid in a long vertical channel consisting of two parallel impermeable plates is investigated. The flow exists under constant pressure gradient, temperature dependent viscosity, viscous dissipation and in the presence of transversely applied uniform magnetic field. To obtain the solutions of the coupled non-linear system of equations, the regular perturbation technique is used. The effects of different physical parameters on velocity field, temperature distribution, skin-friction and rate of heat transfer are numerically evaluated, presented graphically and discussed.

Pages:
ISSN:
2319-8052 (Online) - 2231-3478 (Print)
Source:
DOI:
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Copy the following to cite this article:

1N. P. SINGH, 2V. UPADHYAY, 2A. K. AGRAWAL and 2KHILANAND GUPTA, "Hydromagnetic Radiative Convection Flow in a Vertical Channel With Temperature Dependent Viscosity and Viscous Dissipation and Heat Generation/Absorption", Journal of Ultra Scientist of Physical Sciences, Volume 26, Issue 2, Page Number , 2016

Copy the following to cite this URL:

1N. P. SINGH, 2V. UPADHYAY, 2A. K. AGRAWAL and 2KHILANAND GUPTA, "Hydromagnetic Radiative Convection Flow in a Vertical Channel With Temperature Dependent Viscosity and Viscous Dissipation and Heat Generation/Absorption", Journal of Ultra Scientist of Physical Sciences, Volume 26, Issue 2, Page Number , 2016

Available from: http://ultraphysicalsciences.org/paper/385/

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