Trace amounts of water are sufficient to produce cation redistribution in zeolites. Monte Carlo simulations of zeolite faujasite NaY reveal a spontaneous redistribution of site-I and site-I′ cations upon water adsorption. When aromatics are coadsorbed in the zeolite, cation redistribution takes place for a very small amount of water (full dots in the figure).
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Beauvais et al. (2004) studied this question.
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