Convective instabilities in porous media
β
George M. Homsy; Albert E. Sherwood
π
Article
π
1976
π
American Institute of Chemical Engineers
π
English
β 722 KB
## Abstract The stability of a thermally stratified, saturated porous media through which mass is being ejected is considered theoretically. The stability parameter is a flow modified D'ArcyβRayleigh number and is a function of a single scalar variable, the dimensionless throughβflow strength. Resu