文摘
Using classical molecular dynamics (MD) simulations, we have studied some structural and diffusive propertiesof water molecules adsorbed in chabazite. In particular, we have investigated the variation of the self-diffusioncoefficient of the water molecules as a function of their concentration and the nature of the hydration shellsof 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 diffusionanisotropy is computed at T = 600 K. It is compared with theoretical results based on jump models andqualitatively compared with pulsed field gradient nuclear magnetic resonance (PFG NMR) experiments of asingle chabazite crystal at 293 K and with tracer diffusion studies.