A model based on invasion percolation was used to simulate the migrati
on of a non-wetting fluid through a porous medium filled with an immis
cible wetting fluid under the influence of a gradient such as that pro
vided by gravity. The migrating fluid clusters undergo both fragmentat
ion and coalescence. The fragment size distribution obtained from two-
dimensional simulations in which the gradient g is slowly increased fr
om 0 can be represented by the scaling form N(s)(g) approximately s-2f
(s/\g\-z) where z = 1 + (D - 1)nu/(nu + 1). Here D is the fractal dime
nsionality of invasion percolation, with trapping, and nu is the ordin
ary percolation correlation length exponent.