Non-Newtonian Natural Convection Along a Vertical Plate with Uniform Surface Heat Fluxes

Molla, M.M. and Yao, L.S. (2009) Non-Newtonian Natural Convection Along a Vertical Plate with Uniform Surface Heat Fluxes. Journal of Thermophysics and Heat Transfer, 23(1), pp. 176-185. (doi: 10.2514/1.37566)

Full text not currently available from Enlighten.

Publisher's URL: http://dx.doi.org/10.2514/1.37566

Abstract

Natural convection of non-Newtonian fluids along a vertical flat plate with the heating condition of uniform surface heat flux was investigated using a modified power-law viscosity model. In this model, there are no physically unrealistic limits in the boundary-layer formulation for power-law non-Newtonian fluids. The governing equations are transformed into parabolic coordinates and the singularity of the leading edge is removed; hence, the boundary-layer equations can be solved straightforwardly by marching from the leading edge downstream. Numerical results are presented for the case of shear-thinning as well as shear-thickening fluids for two limits. The numerical results demonstrate that a similarity solution for natural convection exists near the leading edge, where the shear rate is not large enough to trigger non-Newtonian effects. After the shear rate increases beyond a threshold value, non-Newtonian effects start to develop and a similarity solution no longer exists. This indicates that the length scale is introduced into the boundary-layer formulation by the classical power-law correlation.

Item Type:Articles
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Molla, Mr M D Mamun
Authors: Molla, M.M., and Yao, L.S.
College/School:College of Science and Engineering > School of Engineering > Systems Power and Energy
Journal Name:Journal of Thermophysics and Heat Transfer
ISSN:0887-8722
Published Online:01 January 2009

University Staff: Request a correction | Enlighten Editors: Update this record