4. METHOD OF SOLUTION
The model consists of a set of coupled
partial differential equations for heat and mass transfer in
porous media and an equation of state relating fluid density to
temperature. Simultaneous solution of the flow and energy
equations is accomplished by interlacing the solutions in time,
first assuming temperatures and fluid densities constant over an
interval and solving for new fluid pressure and velocity
distributions, then using the new pressure and velocity
distributions to compute new temperature and fluid density
distributions and so on. These equations are solved numerically
using an integrated finite difference method which treats
arbitrary nodal configurations in up to three dimensions. The
concepts of fluid and thermal time constants as indicators of
nodal response times and numerical stability limits is an inherent
part of the numerical scheme.