Journal
JOURNAL OF PHYSICAL CHEMISTRY C
Volume 111, Issue 40, Pages 14707-14712Publisher
AMER CHEMICAL SOC
DOI: 10.1021/jp073857s
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Using classical molecular dynamics (MD) simulations, we have studied some structural and diffusive properties of water molecules adsorbed in chabazite. In particular, we have investigated the variation of the self-diffusion coefficient of the water molecules as a function of their concentration and the nature of the hydration shells of the extraframework Ca++ ions with varying concentrations of water. Our study indicates that the well-defined and stable hydration shells of this ion play an important role in the diffusion process. The diffusion anisotropy is computed at T = 600 K. It is compared with theoretical results based on jump, models and qualitatively compared with pulsed field gradient nuclear magnetic resonance (PFG NMR) experiments of a single chabazite crystal at 293 K and with tracer diffusion studies.
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