Infrared Study of Attapulgite* and HCl Treated Attapulgite

Efraim Mendelovici
Instituto de Investigación Química, Facultad de Farmacia, Universidad de los Andes, Mérida, Venezuela
* Part of this work has been done at the Soil Sciences Department, Michigan State University, East Lansing, U.S.A.

Abstract: Infrared absorption spectra show important changes in the positions and form of the absorption bands of a film of attapulgite after it has been pumped out. An attempt to differentiate among some of the multiple frequencies due to OH groups is based on the information obtained from dehydration and deuteration experiments. The 1198 cm−1 shoulder, characteristic of attapulgite, is assigned to a Si-O vibration. When attapulgite is refluxed with 5N HCl for 5 hr the octahedral layer is dissolved. The acid attack causes the disappearance of the Si-O-Si absorption bands from attapulgite giving rise to a characteristic vibration at 1090 cm −1, as well as another absorption at 960 cm −1. The latter indicates the presence of silanol groups.

Clays and Clay Minerals; April 1973 v. 21; no. 2; p. 115-119; DOI: 10.1346/CCMN.1973.0210207
© 1973, The Clay Minerals Society
Clay Minerals Society (www.clays.org)