L. Gorb et al., The interaction of nitrobenzene with the hydrate basal surface of montmorillonite: an ab initio study, PHYS CHEM P, 2(21), 2000, pp. 5007-5012
The results of an ab initio Hartree-Fock study of the cluster molecular mod
el mimicking the ditrigonal cavity of montmorillonite are reported. Full op
timization of the geometry has been applied for the Si6Al6O30H18 cluster us
ing the HF/6-31G(d) basis set. In order to obtain a model of the isomorphic
substitution in the alumino oxygen layer of clay minerals, a magnesium ato
m has replaced one of the aluminium atoms of the alumino-oxygen layer in th
e cluster. To compensate for the negative charge which inevitably appears i
n this type of substitution, the Na+ exchangeable cation has been placed in
the area with the most negative electrostatic potential in the basal plane
of the cluster model. Finally, we have calculated the geometry and interac
tion energy for the adsorption complex which is formed by the interaction o
f nitrobenzene (the simplest nitroaromatic compound, having the chemical fo
rmula C6H5NO2) with the hydrated surface of clay minerals. The predicted BS
SE corrected energy of the interaction is of the same order (11.8 kcal mol(
-1) at the B3LYP/6-31G(d)//HF/6-31G(d) level) as has been estimated for the
adsorption of nitro-compounds interacting with full molecular contacts. We
have concluded that this type of adsorption of nitro-compounds should be a
t least as effective as the adsorbtion which includes the donor-acceptor ty
pe of interactions with a nonhydrated silicon-oxygen surface.