A model for the migration of gas through clay is described, in which gas pr
opagates as a set of independent paths. The paths are constructed stochasti
cally from sections of capillary-like tubes which inflate when the gas pres
sure exceeds a threshold value. The paths partially deflate when they break
through the clay, but their inflation is still sufficient to significantly
increase the resultant slow flow of gas. The model also includes gas flows
for path content and gas puss at breakthrough, and describes expelled wate
r in a simple manner. (C) 1999 Elsevier Science B.V. All rights reserved.