We study the flow of two immiscible fluids of different density and mobilit
y in a porous medium. If the heavier phase lies above the lighter one, the
interface is observed to be unstable. The two phases start to mix on a meso
scopic scale and the mixing zone grows in time-an example of evolution of m
icrostructure. A simple set of assumptions on the physics of this two-phase
flow in a porous medium leads to a mathematically ill-posed problem-when u
sed to establish a continuum free boundary problem, We propose and motivate
a relaxation of this "nonconvex" constraint of a phase distribution with a
sharp interface on a macroscopic scale. We prove that this approach leads
to a mathematically well-posed problem that predicts shape and evolution of
the mixing profile as a function of the density difference and mobility qu
otient. (C) 1999 John Wiley & Sons, Inc.