Convection in a stratified flow in an inclined porous channel
The flow of a fluid of variable viscosity in an inclined channel bounded by two permeable layers is considered. The flow between the permeable layers is governed by Navier-Stokes equations. The flow in the porous medium is governed by Darcy law. The velocity field and the temperature distribution are obtained and the results are discussed.
scientific article; zbMATH DE number 4053256