Grand canonical Monte Carlo (GCMC) simulations of binary
Lennard-Jones mixtures in the zeolite
silicalite have been used to predict the adsorption of CH4
and CF4 mixtures as a function of gas phase
composition, total pressure, and temperature. For single
components and mixtures, predictions of adsorption
isotherms and isosteric heats are in good agreement with experiment at
room temperature. Within the
experimental pressure range of 0 to 17 bar, the mixtures are well
described by the ideal adsorbed solution
(IAS) theory. For very high loading, deviations from IAS theory
appear. The configurations generated
in the simulation were used to calculate sorbate−zeolite interaction
energy distributions for different
types of siting locations within the zeolite pores. These
distributions display a pore shape related energetic
heterogeneity in different regions of silicalite. Near saturation
at a total loading of 12 molecules per unit
cell, the shape of the observed energy distribution is relatively
independent of the composition in the pore.
Nevertheless, the energetic heterogeneity is responsible for a
mild segregation in the adsorbed mixtures,
with methane adsorbed preferentially in the silicalite zigzag channels
and CF4 preferentially in the straight
channels.