EVOLUTION OF BENZYLAMMONIUM-VERMICULITE AND ORNITHINE-VERMICULITE INTERCALATES

Citation
C. Delacalle et al., EVOLUTION OF BENZYLAMMONIUM-VERMICULITE AND ORNITHINE-VERMICULITE INTERCALATES, Clays and clay minerals, 44(1), 1996, pp. 68-76
Citations number
23
Categorie Soggetti
Mineralogy
Journal title
ISSN journal
00098604
Volume
44
Issue
1
Year of publication
1996
Pages
68 - 76
Database
ISI
SICI code
0009-8604(1996)44:1<68:EOBAOI>2.0.ZU;2-H
Abstract
This report consists of a study of 1-ornithine hydrochloride-vermiculi te and of benzylammonium hydrochloride-vermiculite complex. The evolut ion of these organo-vermiculite structures upon heating is studied by X-ray diffraction (XRD) as well as infrared spectroscopy. fter heating vermiculite saturated with 1-ornithine cations, it shows condensation of interlayer ornithine molecules (peptide complexes). The stacking m ode, opposing ditrigonal cavities, is not modified between aminoacid c omplex and peptide complex. For vermiculite saturated with benzylammon ium cations, the stacking sequence changes through heating by changing benzylammonium to NH4+. This transformation implies a sliding of the layers over each other. The ditrigonal surface cavities become face to face, as in the original mica. There are no random translations as in the starting complex.