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Energy changes in dehydration processes of clay minerals

Published online by Cambridge University Press:  09 July 2018

Toshio Sudo ,
Susumu Shimoda ,
Shigeru Nishigaki  and
Masaharu Aoki
Toshio Sudo
Affiliation:
Geological and Mineralogical Institute, Faculty of Science, Tokyo University of Education
Susumu Shimoda
Affiliation:
Geological and Mineralogical Institute, Faculty of Science, Tokyo University of Education
Shigeru Nishigaki
Affiliation:
Rigaku Denki Company, Tokyo, Japan
Masaharu Aoki
Affiliation:
Rigaku Denki Company, Tokyo, Japan
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Abstract

Using the adiabatic calorimeter which has been developed by Nagasaki & Takagi (1948) and manufactured by the Rigaku Denki Company, the energy changes associated with the dehydration and dehydroxylation processes of clay minerals were measured at room pressure. The samples studied were mont-morillonite, chlorite (trioctahedral type), and three kinds of interstratified minerals with component layers such as mica, dioctahedral chlorite, and montmorillonite. ΔH-values due to the dehydration of the interlayer region were 9·8 kcal/H2O mole for montmorillonite and 12·4–13·4 kcal/H2O mole for interstratified minerals mica-montmoriIlonite and dioctahedral chlorite-montmorillonite. The values due to dehydroxylation of the silicate layer were 17·7 kcal/H2O mole for montmorillonite, 16·8–17·5 kcal/H2O mole for the interstratified mica- montmorillonite, and 19·3 kcal/H2O mole for chlorite. The value for the dehydroxylation of the hydroxyl layer of chlorite was 19·3 kcal/H2O mole. For the sake of comparison, the heat of transition α↔β of quartz was found to be 140 cal/mole. The reproducibility of these values was in the range of ±5%.

Type
Research Article
Information
Clay Minerals , Volume 7 , Issue 1 , July 1967 , pp. 33 - 42
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1967

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References

Birch, F. (1942) Handbook of physical constants. Geol. Soc. Am., Special Paper. 36.Google Scholar
Frank-Kamenetsky, V.A., Logvinenko, N.V. & Drits, V.A. (1963) International Clay Conference, Stockholm, Vol. 2, pp. 181–186.Google Scholar
Grimshaw, R.W. & Roberts, A.L. (1957) The Differential Thermal Investigation of Clays (Mackenzie, R. C., editor), Chap. XI, pp. 275–298. Mineralogical Society, London.Google Scholar
Kelley, K.K. (1960) Contribution to the data on the theoretical metallurgy, XIII. High temperature heat content, heat capacity and entropy data on the elements and inorganic compounds. U.S. Govt Print. Off.Google Scholar
Nagasaki, S. & Takagi, U. (1948) Appl. Phy. 17, 104.Google Scholar
Nagasaki, S., Yonemitsu, K. & Maezono, A. (1961) Adv. Clay Sc. 3, 42.Google Scholar
Sakamoto, T. & Sudo, T. (1956) Mineralog. J., Sappor.1, 348.Google Scholar
Sudo, T. & Hayashi, H. (1956) Clays Clay Miner. NAS-NRC Publications 456, 398–412.Google Scholar
Sudo, T., Hayashi, H. & Shimoda, S. (1962) Clays Clay Mine. 8, 378.Google Scholar
Sudo, T. & Kodama, H (1957) Z. Kristallogr. Kristallgeo. 109, 406.Google Scholar
Sudo, T. & Sato, M. (1966) International Clay Conferehce, Jerusalem, Vol. 1, pp. 33–39.Google Scholar
Sudo, T., Takahashi, H. & Matsui, H. (1954) Nature, Lond. 173, 261.Google Scholar
Wagman, D. D. (1957) American Institute of Physics Handboo. Chap. 4, J, p. 155.Google Scholar