Molecular structure in the interlayers of sodium Wyoming montmorilloni
te with one, two, or three water monolayers was investigated by Monte
Carlo and molecular dynamics simulation, based on tested water-water,
water-counterion, clay-water, and clay-counterion potential unctions.
Calculated layer spacings and thermodynamic properties, as well as int
erlayer water configurations and interlayer-species self-diffusion coe
fficients, were in good agreement with available experimental data. In
ner-sphere surface complexes of Na+ with tetrahedral charge sites pers
isted in all hydrates, whereas the outer-sphere surface complexes with
octahedral charge sites found in the one-layer hydrate dissociated pa
rtially into an incipient diffuse layer in the two- and three-layer hy
drates. Even in the three-layer hydrate, interlayer water molecules di
d not replicate their structure or mobility in bulk aqueous solution.
Improved diffraction and spectroscopic data on interlayer water are ne
eded to guide future simulation studies.