A simple one-dimensional model of fluid migration through a disordered
medium is presented. The model is based on invasion percolation and i
s motivated by two-phase flow experiments in porous media. A uniform p
ressure gradient g drives fluid clusters through a random medium. The
clusters may both coalesce and fragment during migration. The leading
fragment advances stepwise. The pressure gradient g is increased conti
nuously. The evolution of the system is characterized by stagnation pe
riods. Simulation results are described and analyzed using probability
theory. The fragment length distribution is characterized by a crosso
ver length s(g) similar to g(-1/2) and the length of the leading frag
ment scales as s(p)(g) similar to g(-1). The mean fragment length is f
ound to scale with the initial cluster length s(o) and g as [s] = s(o)
(1/2)f(gs(o)(3/4)).