The surface geometry of Vycor porous glass was examined by using the r
elative permeability (P-R) technique in a H2O/He system. At a water re
lative pressure of similar to 0.3, a maximum is observed on the P-R cu
rve. This maximum is explained in terms of geometrical changes taking
place due to the deposition of a water film on the internal Vycor surf
ace. When the sample is dry, diffusion in a fractal system is found to
be more appropriate in describing the process. When the sample is wet
, the diffusion process obeys classical Knudsen theory for smooth cyli
nders. (C) 1998 Academic Press.