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

Table 5

Region-specific lateral (2D) diffusivity () of interlayer cations and water through our model synthetic clays.

T (K)
293	0.39  0.02	1.68  0.14	0.50  0.01	1.86  0.03	0.27  0.01	2.32 0.13	0.15  0.07	1.92  0.02
300	0.71  0.08	1.75  0.27	0.73  0.12	1.80  0.10	0.42  0.10	2.83 0.11	0.17  0.12	2.28  0.26
323	1.03  0.05	2.72  0.06	1.01  0.28	2.49  0.09	0.42  0.18	3.49 0.29	0.15  0.02	2.28  0.26
350	0.31  0.03	4.46  0.10	0.64  0.33	4.30  0.26	1.01  0.12	3.68 0.16	1.34  0.10	3.88  0.33