A linear stability analysis is performed to study the onset of convection i
n a horizontal saturated porous layer of finite aspect ratio and anisotropi
c in permeability. The critical Rayleigh number is established as a functio
n of the permeability ratio, the inclination angle of the principal axes an
d the enclosure aspect ratio. A linear stability analysis is conducted thro
ugh a numerical procedure. Also, for the weak finite amplitude convection,
results are obtained by solving numerically the full governing equations. (
C) 2000 Elsevier Science Ltd.