We present an account of the linear instability of Darcy-Boussinesq convection in a uniform, unstably stratified porous layer at arbitrary inclinations α from the horizontal. A full numerical solution of the linearized disturbance equations is given and the detailed graphical results used to motivate various asymptotic analyses. A careful study shows that at large Rayleigh numbers two-dimensional instability can only arise when α≤31.30°. However it is also demonstrated that the maximum inclination below which this instability may be possible is the slightly greater value of 31.49° which corresponds to a critical Rayleigh number of 104.30.
History
Publication title
Acta Mechanica
Volume
144
Issue
1-2
Pagination
103-118
ISSN
0001-5970
Department/School
School of Natural Sciences
Publisher
Springer-Verlag Wien
Place of publication
Sachsenplatz 4-6, Po Box 89, Vienna, Austria, A-1201