The dehydration of kaolinite to metakaolinite can be completely reversed; particles of rehydrated metakaolinite grow perpendicular to the c* axis and their edges are parallel to those of parent metakaolinite and kaolinite, showing that the rehydration is a topotactic solid-state process.
J. Rocha and J. Klinowski, J. Chem. Soc., Chem. Commun., 1991, 582 DOI: 10.1039/C39910000582
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