Temperature Dependence Study of Water Dynamics in Fluorohectorite Clays Using Molecular Dynamics Simulations

Table 4

Region-specific 3D diffusivity () of interlayer cation and water through our model synthetic clays.

T (K)
293	0.26  0.01	1.12  0.09	0.34  0.01	1.06  0.02	0.19  0.01	1.55  0.08	0.11  0.05	1.28  0.01
300	0.48  0.06	1.17  0.18	0.49  0.07	1.20  0.06	0.29  0.06	1.88  0.07	0.13  0.09	1.52  0.18
323	0.69  0.03	1.82  0.04	0.68  0.18	1.67  0.06	0.29  0.15	2.33  0.19	0.11  0.01	2.42  0.09
350	0.91  0.07	2.59  0.22	0.68  0.08	2.45  0.10	0.43  0.23	2.87  0.17	0.22  0.01	2.97  0.08