The traditional hopping model of diffusion in zeolites predicts a conc
entration-independent diffusivity D-r whereas observations almost alwa
ys yield D(theta) increasing strongly with Increasing average occupanc
y theta of the adsorption sites. An explanation is attempted in terms
of a model allowing double occupancy of adsorption wells or ''cages.''
It is assumed that the repulsion between molecules adsorbed in one we
ll lifts its bottom, whereas the level of the ''windows'' between well
s remains unchanged. The potential barrier from well to window is ther
eby lowered so that jumps become more frequent at higher density, when
double occupancy is more probable. The resulting expression for D(the
ta) is compared with the main features of existing experimental curves
. Although it is possible to fit the observed low density behavior of
D[theta), the model is not able to reproduce the steep approach toward
saturation.