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The thermal stability of kaolinite and the microstructure of its thermal products strongly depend on random defects ( R 2 ) rather than crystalline defects (HI). Kaolinite with a lower random defect density is more stable than that with higher defect density during dehydroxylation and the derived metakaolinite can be directly transformed into orthorhombic mullite (3/2‐mullite). However, for kaolinite with higher random defect density, there is a cubic phase occurring in the transformation from metakaolinite to primary mullite. Primary mullite will be transformed into orthorhombic mullite as temperature increases. Al V is universally present in the metakaolinite and the relative amounts of Al VI , Al V , and Al IV vary with the random defect density of the parent kaolinite.
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He et al. (2005) studied this question.
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