MOLECULAR SIMULATIONS OF MONTMORILLONITE INTERCALATED WITH ALUMINUM COMPLEX CATIONS - PART II - INTERCALATION WITH AL(OH)(3)-FRAGMENT POLYMERS

Citation
P. Capkova et al., MOLECULAR SIMULATIONS OF MONTMORILLONITE INTERCALATED WITH ALUMINUM COMPLEX CATIONS - PART II - INTERCALATION WITH AL(OH)(3)-FRAGMENT POLYMERS, Clays and clay minerals, 46(3), 1998, pp. 240-244
Citations number
13
Categorie Soggetti
Agriculture Soil Science","Water Resources",Mineralogy
Journal title
ISSN journal
00098604
Volume
46
Issue
3
Year of publication
1998
Pages
240 - 244
Database
ISI
SICI code
0009-8604(1998)46:3<240:MSOMIW>2.0.ZU;2-5
Abstract
The Crystal Packer module in the Cerius(2) modeling environment has be en used to study the structure of montmorillonite intercalated with Al (OH)(3)-fragment (gibbsite-like) polymers. Basal spacings in gibbsite- like polymers arranged in 2 layers in the interlayer of montmorillonit e varied in the range 19.54-20.13 Angstrom, depending on the type and arrangement of Al(OH), fragments. The inhomogeneous distribution of in tercalating species in the interlayer and, consequently, the turbostra tic stacking of layers has been found for gibbsite-like polymers as we ll as in the case of Keggin cations (Capkova et al. 1998). The dominat ing contribution to the total sublimation energy comes from electrosta tic interactions for both intercalating species, gibbsite-like polymer s and Keggin cations.