Using grand-canonical-ensemble Monte Carlo and molecular dynamics simu
lations, adsorption equilibria and diffusion of finite-size molecules
in model pillared clays are studied. Our simulations show that, at mod
erate and high porosities, clustering of the pillars and their spatial
distribution do not have a significant effect on the adsorption isoth
erms. However, the dependence of the adsorption isotherms on the poros
ity is different at low and high pressures. At low pressures, the equi
librium loading increases as the porosity decreases, whereas at high p
ressures it increases with increasing porosity. The difference is due
to the competition between the adsorption surface and the accessible v
olume of the system, which are the two most important factors that con
trol the adsorption behavior of the system. At low enough temperatures
and at any porosity, a first-order phase transition (condensation) oc
curs. The self-diffusivity D is found to be a monotonically increasing
function of the temperature. Unlike adsorption isotherms, however, cl
ustering of the pillars does have a strong effect on the diffusivity o
f the molecules. Moreover, over the entire loading range studied, D in
creases monotonically as the porosity increases. Copyright (C) 1996 El
sevier Science Ltd.