EXPERIMENTAL TRANSFORMATION OF KAOLINITE TO HALLOYSITE

Citation
B. Singh et Idr. Mackinnon, EXPERIMENTAL TRANSFORMATION OF KAOLINITE TO HALLOYSITE, Clays and clay minerals, 44(6), 1996, pp. 825-834
Citations number
20
Categorie Soggetti
Mineralogy
Journal title
ISSN journal
00098604
Volume
44
Issue
6
Year of publication
1996
Pages
825 - 834
Database
ISI
SICI code
0009-8604(1996)44:6<825:ETOKTH>2.0.ZU;2-D
Abstract
A well-characterized kaolinite has been hydrated in order to test the hypothesis that platey kaolinite will roll upon hydration. Kaolinite h ydrates are prepared by repeated intercalation of kaolinite with potas sium acetate and subsequent washing with water. On hydration, kaolinit e plates roll along the major crystallographic directions to form tube s identical to proper tubular halloysite. Most tubes are elongated alo ng the b crystallographic axis, while some are elongated along the a a xis. Overall, the tubes exhibit a range of crystallinity. Well-ordered examples show a 2-layer structure, while poorly ordered tubes show li ttle or no 3-dimensional order. Cross-sectional views of the formed tu bes show both smoothly curved layers and planar faces. These character istics of the experimentally formed tubes are shared by natural halloy sites. Therefore, it is proposed that planar kaolinite can transform t o tubular halloysite.