A model is set up which is believed to contain the essential physics o
f foam drainage. Mathematically, the model leads to a non-linear parti
al differential equation, which we were able to solve exactly by analy
tical methods for the physical boundary conditions relevant for recent
experiments in which a dry foam is wetted by a steady addition of liq
uid. The solution represents a density wave of constant profile (or so
litary wave) in qualitative accord with these experiments. The observe
d dependences of liquid fraction and wet/dry foam boundary velocity on
input flow are reproduced by the model.