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Thermodynamics of the Various High Temperature Transformations of Kaolinite

Published online by Cambridge University Press:  01 January 2024

N. C. Schieltz
Affiliation:
Colorado School of Mines, Golden, Colorado, USA
M. R. Soliman
Affiliation:
Geological Survey and Mineral Research Department, Ministry of Industry, Cairo, Egypt

Abstract

Thermodynamic calculations of ΔG for all possible transformations of metakaolin at the temperature of the first DTA exothermic peak indicates that the most stable transformation is the one that yields mullite rather than γ-alumina.

The energy of crystallization of γ-alumina is quite small—36,513 cal per mol, compared with the energy of crystallization of mullite—336,180 cal per mol. Furthermore, the crystallization of γ-alumina is very slow, and the crystal growth never produces crystallite sizes much larger than the lower end of the colloidal region. Hence, the gradual release of the small amounts of energy liberated during the crystallization of γ-alumina would be extremely difficult to detect by DTA methods.

Type
General Session
Copyright
Copyright © Clay Minerals Society 1964

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References

Brindley, G. W., and Hunter, K. (1955) Thermal reactions of nacrite and the formation of metakaolin, alumina and mullite, Mineral. Mag., 30, 574–84.Google Scholar
Brindley, G. W., and Nakahira, M. (1958) A new concept of transformation sequence of kaolinite to mullite, Nature, 181, 1333–4.Google Scholar
Budnikov, P. P., and Mchedlov-Petrosyan, O. P. (1960) Thermodynamics of changes undergone by kaolinite when heated, Trans. Brit. Ceram. Soc., 59, 479–82.Google Scholar
Comeforo, J. E., Fisher, R. V., and Bradley, W. F. (1948) Multization of kaolinite, J. Am. Ceram. Soc. 31, 254–9.CrossRefGoogle Scholar
Coughlin, J. V. (1954) Contribution to the data on theoretical metallurgy, XII. Heats and free energies of formation of inorganic oxides, U.S. Bur. Mines Bull. 542.Google Scholar
Glassner, A. (1959) Thermodynamic properties of the oxides, chlorides and fluorides to 2500°K, Atomic Energy Commission, Argon National Laboratory, ANL 5750, Univ. Chicago.Google Scholar
Hodgman, C. D., and others (1960) Handbook of Chemistry and Physics, 41st. ed. Chemical Rubber Publishing Company, Cleveland, Ohio.Google Scholar
Hyslof, J. F. (1944) Decomposition of clays by heat, Trans. Brit. Ceram. Soc. 43, 4951.Google Scholar
Insley, H., and Ewell, R. H. (1935) Thermal behavior of kaolin minerals, J. Res. Nat. Bur. Std. 14, 615–27.CrossRefGoogle Scholar
Jay, A. H, (1939) Alumino-silicate refractories, Trans. Brit. Ceram. Soc., 38, 455–60.Google Scholar
Johns, W. D. (1953) High temperature phase changes in kaolinite, Mineral. Mag. 30, 186–98.Google Scholar
Kelly, K. K. (1960) Contributions to the data on theoretical metallurgy XIII. High temperature heat content, heat capacity and entropy data for elements and inorganic compounds, U.S. Bur. Mines Bull. 584.Google Scholar
Kubachewski, O., and Evans, E. L. (1951) Metallurgical Thermodynamics, Academic Press, New York.Google Scholar
Richardson, H. M., and Wild, F. G. (1952) An X-ray study of crystalline phases that occur in fired clays, Trans. Brit. Ceram. Soc. 51, 387400.Google Scholar
Vaughan, F. (1955) Energy changes when kaolin minerals are heated, Clay Minerals Bull. 2, 265–74.CrossRefGoogle Scholar