Structures of di- and trioctahedral smectites intercalated with a Keggin li
ke cation [Al13O4(OH)(24)(H2O)(12)](7+) have been studied using molecular m
echanics simulations in the Cerius(2) modelling environment.
The present study is focused on the effect of substitutions and distortions
in the silicate layers on the crystal energy in these two types of interca
lated layer structures.
Detailed analysis of charge distribution has been carried out to explain th
e differences in behaviour of these two intercalated smectites. Tetrahedral
substitution in the smectite layer reduces locally the negative charge of
the smectite outside oxygen layer. This charge reduction favours the creati
on of preferential interlayer positions of the Keggin ion. The consequence
of these preferential interlayer positions is a more homogeneous distributi
on of the intercalating ion. (C) 2000 Elsevier Science B.V. All rights rese
rved.