Temperature dependence study of water dynamics in Fluorohectorite clays using Molecular dynamics simulations

In this work, we have carried out molecular dynamics (MD) simulation techniques to study the diffusion coefficient of interlayer molecules at different temperature. Within the wider context of water dynamics in soils, and with a particular emphasis on clays, we present here the translational dynamics of water in clays, in a bi-hydrated states. We focus on temperatures between 293 K and 350 K, i.e., the range relevant to the environmental waste packages. A natural hectorite clay of interest is modified as a synthetic clay, which allows us to understand the determinantal parameters from MD simulations through a comparison with the experimental values. The activation energy E a determined by our simulation is [8.50 - 16.62] KJ/mol. The calculated diffusive constants are in the order of 10^{-5} {cm^{2}}/s. The simulation results are in good agreement with experiments for the relevant set of conditions, and they give more insight into the origin of the observed dynamics.