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The self-diffusion properties of pure CH 4 and its binary mixture with CO 2 within NaY zeolite have been investigated by combining an experimental quasi-elastic neutron scattering (QENS) technique and classical molecular dynamics simulations. The QENS measurements carried out at 200 K led to an unexpected self-diffusivity profile for pure CH 4 with the presence of a maximum for a loading of 32 CH 4 /unit cell, which was never observed before for the diffusion of apolar species in a zeolite system with large windows. Molecular dynamics simulations were performed using two distinct microscopic models for representing the CH 4 /NaY interactions. Depending on the model, we are able to fairly reproduce either the magnitude or the profile of the self-diffusivity. Further analysis allowed us to provide some molecular insight into the diffusion mechanism in play. The QENS measurements report only a slight decrease of the self-diffusivity of CH 4 in the presence of CO 2 when the CO 2 loading increases. Molecular dynamics simulations successfully capture this experimental trend and suggest a plausible microscopic diffusion mechanism in the case of this binary mixture.
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Déroche et al. (2010) studied this question.
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