Experimental transformation of kaolinite to halloysite


Autoria(s): Singh, Balbir; Mackinnon, Ian D.R.
Data(s)

1996

Resumo

A well-characterized kaolinite has been hydrated in order to test the hypothesis that platey kaolinite will roll upon hydration. Kaolinite hydrates are prepared by repeated intercalation of kaolinite with potassium acetate and subsequent washing with water. On hydration, kaolinite plates roll along the major crystallographic directions to form tubes identical to proper tubular halloysite. Most tubes are elongated along the b crystallographic axis, while some are elongated along the a axis. Overall, the tubes exhibit a range of crystallinity. Well-ordered examples show a 2-layer structure, while poorly ordered tubes show little or no 3-dimensional order. Cross-sectional views of the formed tubes show both smoothly curved layers and planar faces. These characteristics of the experimentally formed tubes are shared by natural halloysites. Therefore, it is proposed that planar kaolinite can transform to tubular halloysite.

Formato

application/pdf

Identificador

http://eprints.qut.edu.au/55706/

Publicador

The Clay Minerals Society

Relação

http://eprints.qut.edu.au/55706/3/55706.pdf

DOI:10.1346/CCMN.1996.0440614

Singh, Balbir & Mackinnon, Ian D.R. (1996) Experimental transformation of kaolinite to halloysite. Clays and Clay Minerals, 44(6), pp. 825-834.

Direitos

Copyright 1996 Clay Minerals Society

Reproduced with kind permission of The Clay Minerals Society, publisher of Clays and Clay Minerals

Fonte

Institute for Future Environments

Palavras-Chave #040306 Mineralogy and Crystallography #bonding #chemical properties #clay mineralogy #crystal chemistry #crystal growth #crystallography #electrons #experimental studies #geochemistry #halloysite #hydration #kaolinite #polyhedra #sheet silicates #TEM data #transformations #X-ray diffraction data
Tipo

Journal Article