International Journal of Computer Applications
Foundation of Computer Science (FCS), NY, USA
|
Volume 121 - Issue 3 |
Published: July 2015 |
Authors: D. Iranian, P. Loganathan, P. Ganesan |
![]() |
D. Iranian, P. Loganathan, P. Ganesan . Unsteady MHD Natural Convective Flow over Vertical Plate in Thermally Stratified Media with Variable Viscosity and Thermal Conductivity. International Journal of Computer Applications. 121, 3 (July 2015), 18-24. DOI=10.5120/21520-4498
@article{ 10.5120/21520-4498, author = { D. Iranian,P. Loganathan,P. Ganesan }, title = { Unsteady MHD Natural Convective Flow over Vertical Plate in Thermally Stratified Media with Variable Viscosity and Thermal Conductivity }, journal = { International Journal of Computer Applications }, year = { 2015 }, volume = { 121 }, number = { 3 }, pages = { 18-24 }, doi = { 10.5120/21520-4498 }, publisher = { Foundation of Computer Science (FCS), NY, USA } }
%0 Journal Article %D 2015 %A D. Iranian %A P. Loganathan %A P. Ganesan %T Unsteady MHD Natural Convective Flow over Vertical Plate in Thermally Stratified Media with Variable Viscosity and Thermal Conductivity%T %J International Journal of Computer Applications %V 121 %N 3 %P 18-24 %R 10.5120/21520-4498 %I Foundation of Computer Science (FCS), NY, USA
The effects of exponentially varying viscosity and linearly varying thermal conductivity on unsteady MHD natural convective flow past a semi infinite vertical plate in a thermally stratified medium is studied. The variables of both viscosity and thermal conductivity are considered only a function of temperature. The governing boundary layer equations of continuity, momentum and energy have been transformed into dimensionless coupled and nonlinear equations and after that solved by implicit finite-difference method of Crank-Nicolson type. The effects of the varying viscosity, thermal conductivity and stratification parameter at various times are discussed with velocity and temperature profiles and additionally the skin-friction and the rate of heat transfer.