Physics and Chemistry of Minerals

, Volume 22, Issue 4, pp 207–217 | Cite as

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

  • M. Bellotto
  • A. Gualtieri
  • G. Artioli
  • S. M. Clark


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.


Boundary Layer Activation Energy Heating Rate Reaction Mechanism Kaolinite 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Copyright information

© Springer-Verlag 1995

Authors and Affiliations

  • M. Bellotto
    • 1
  • A. Gualtieri
    • 2
  • G. Artioli
    • 3
  • S. M. Clark
    • 4
  1. 1.CISE Tecnologie InnovativeSegrateItaly
  2. 2.Istituto di Mineralogia e Petrologia, Università di ModenaModenaItaly
  3. 3.Dipartimento di Scienze della TerraUniversità di MilanoMilanoItaly
  4. 4.SERC Daresbury LaboratoryDaresburyUK

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