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Crystal-chemical changes of mixed-layer kaolinite-smectite with progressive kaolinization, as investigated by TEM-AEM and HRTEM

Published online by Cambridge University Press:  01 January 2024

Javier Cuadros ,
Fernando Nieto  and
Teresa Wing-Dudek
Javier Cuadros*
Affiliation:
Department of Mineralogy, Natural History Museum Cromwell Road SW7 5BD London UK
Fernando Nieto
Affiliation:
Departamento de Mineralogía y Petrología and IACT, Universidad de Granada-CSIC 18002 Granada Spain
Teresa Wing-Dudek
Affiliation:
Department of Mineralogy, Natural History Museum Cromwell Road SW7 5BD London UK
*
aj.cuadros@nhm.ac.uk
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Abstract

The mechanism for the kaolinization of smectite is extremely complex. The purpose of this study was to explore this mechanism by providing more microscopic information about kaolinite-smectite (K-S) intermediate phases. Crystal-chemical changes were investigated and integrated in a model of the transformation mechanism. Eight K-S samples from three localities, derived from volcanic ash beds, were studied using transmission and analytical electron microscopy (TEM, AEM) and high-resolution TEM (HRTEM). The study completes a previous investigation, using several analytical techniques. The samples cover the range of K-S composition available from the previously studied sample set. Analysis by TEM indicated the preservation of particle morphology throughout the process. Most K-S particles had anhedral, smectite-like morphology, and only the most kaolinitic specimen revealed the coexistence of anhedral and euhedral, hexagonal particles. Analytical electron microscopy showed large chemical variations within samples, corresponding to various degrees of smectite kaolinization. Comparison of chemical results (Si/Al) and d060 values (proxy for octahedral composition) with the extent of kaolinization from thermogravimetry (TG) indicates that chemical changes in the octahedral sheet occur mainly when the proportion of kaolinite is 40–70%. The results above are consistent with kaolinization occurring via layer-by-layer transformation through the progressive loss of individual tetrahedral sheets in smectite layers and subsequent chemical changes in the octahedral sheet. Such a mechanism would produce the results observed in this study: (1) most particles preserve their original morphology; (2) significant variation in terms of the extent of transformation of particles within samples, and (3) formation of crystal structures intermediate between those of smectite and kaolinite, with parts of the tetrahedral sheets missing (kaolinite-like patches). Such structures become least stable at kaolinite ∼50%, when the perimeter of the kaolinite-like patches is largest and chemical changes in the octahedral sheet can occur more easily. Kaolinite layers could not be resolved by HRTEM in most cases and showed lattice fringes corresponding to superstructures. A model was established to quantify kaolinite and smectite layers in the HRTEM images with results which matched TG-derived values.

Keywords

HRTEMKaolinite-smectiteSolid-state TransformationTEM-AEM

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Type
Article
Information
Clays and Clay Minerals , Volume 57 , Issue 6 , December 2009 , pp. 742 - 750
Copyright
© The Clay Minerals Society 2009

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