The onset of convection in a porous layer induced by viscous dissipation: A linear stability analysis


Barletta, A., Celli, M. and Rees, D. A. S., 2009. The onset of convection in a porous layer induced by viscous dissipation: A linear stability analysis. International Journal of Heat and Mass Transfer, 52 (1-2), pp. 337-344.

Related documents:

This repository does not currently have the full-text of this item.
You may be able to access a copy if URLs are provided below. (Contact Author)

Official URL:


The effect of viscous dissipation oil parallel Darcy flow in a horizontal porous layer with an adiabatic lower boundary and an isothermal upper boundary is discussed. The presence of viscous dissipation serves to cause a nonlinear temperature profile within the layer. The linear stability of this nonisothermal base flow is then investigated with respect to the onset of convective rolls. The solution of the linear equations for the perturbation waves is determined analytically by a power series method, and the results are confirmed using a direct numerical approach Using a fourth order Runge Kutta method. The neutral stability curve and the critical value of the governing parameter R = GePe(2) are obtained, where Ge is the Gebhart number and Pe is the Peclet number. The effect of an imperfect isothermal boundary condition at the upper boundary is investigated by considering finite values of the Biot number.


Item Type Articles
CreatorsBarletta, A., Celli, M. and Rees, D. A. S.
Uncontrolled Keywordsviscous dissipation,linear,laminar flow,darcy model,mixed convection,stability,porous medium
DepartmentsFaculty of Engineering & Design > Mechanical Engineering
Research CentresAerospace Engineering Research Centre
ID Code12521


Actions (login required)

View Item