The adsorption of argon and nitrogen in silicalite-1 zeolite: A grand canonical Monte-Carlo study

Grand Ensemble Monte-Carlo simulations of adsorption of argon and nitrogen in silicalite have been performed using a new adsorbate/zeolite potential function. In both cases, a good agreement with zero coverage data (Henry law constant and isosteric heat of adsorption) has been obtained. For argon, the simulated isotherm at 77 K exhibits the experimentally observed step. This is attributed to an in site/off-site phase transition of the adsorbed phase. The calculated neutron diffraction spectra are in reasonable agreement with those obtained experimentally. Furthermore, we suggest, in light of recent Ar-40 diffraction experiments of Tosi-Pellenq and Coulomb [18,44], that the shift in pressure between the simulated and the experimental isotherms corresponds to changes in the zeolite structure accompanied with the adsorbate phase transition itself. For nitrogen, only the first of the two experimentally observed steps is reproduced in the simulation. This step corresponds to an ordering of the adsorbed phase. The fact that the second step is missing in the simulated isotherm supports the hypothesis of a distortion of the zeolite framework under the stress of the adsorbed fluid at high loading.