The concept of structural stability is discussed and briefly reviewed withi
n the context of fluid flow in porous media. Then the equations for non-Bou
ssinesq (penetrative) convection in a porous medium with anisotropic permea
bility are analysed. It is shown, by deriving truly a priori estimates, tha
t the solution exists in the natural functional framework and depends conti
nuously on changes in the permeability. Since under appropriate circumstanc
es the onset of thermal convection may be via Hopf bifurcation rather than
stationary convection, such a priori continuous dependence estimates are of
much value. Copyright (C) 2001 John Wiley & Sons, Ltd.