Kinetic study of the kaolinite-mullite reaction sequence. Part I: Kaolinite dehydroxylation

M. Bellotto, A. Gualtieri, G. Artioli*, S. M. Clark

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

201 Citations (Scopus)


The decomposition reaction of kaolinite has been investigated as a function of the defectivity of the starting material and the temperature of reaction. Time resolved energy-dispersive powder diffraction patterns have been measured using synchrotron radiation, both under a constant heating rate (heating rates from 10 to 100° C/min) and in isothermal conditions (in the temperature range 500 to 700° C). The apparent activation energy of the dehydroxylation process is different for kaolinites exhibiting a different degree of stacking fault density. The results of the analysis of the kinetic data indicate that the starting reaction mechanism is controlled by diffusion in the kaolinite particle. The diffusion process is dependent on the defective nature of both kaolinite and metakaolinite. At high temperatures, and at higher heating rates, the reaction mechanism changes and the resistance in the boundary layer outside the crystallites becomes the rate-limiting factor, and nucleation begins within the reacting particle. During the final stage of the dehydroxylation process the reaction is limited by heat or mass transfer, and this might be interpreted by the limited diffusion between the unreacted kaolinite domains and the metakaolinite matrix.

Original languageEnglish
Pages (from-to)207-217
Number of pages11
JournalPhysics and Chemistry of Minerals
Issue number4
Publication statusPublished - Jun 1995
Externally publishedYes


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