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Effects of the Structure of Silica-Alumina Gel on the Hydrothermal Synthesis of Kaolinite

Published online by Cambridge University Press:  28 February 2024

Shigeo Satokawa*
Affiliation:
Engineering Research Association for Artificial Clay, National Industrial Research Institute of Nagoya, Kita, Nagoya 462, Japan
Yasushi Osaki
Affiliation:
Chemical Research Laboratory, Tosoh Corporation, Shin-nanyo, Yamaguchi 746, Japan
Soichiro Samejima
Affiliation:
Chemical Research Laboratory, Tosoh Corporation, Shin-nanyo, Yamaguchi 746, Japan
Ritsuro Miyawaki
Affiliation:
Ceramic Technology Department, National Industrial Research Institute of Nagoya, Kita, Nagoya 462, Japan
Shinji Tomura
Affiliation:
Ceramic Technology Department, National Industrial Research Institute of Nagoya, Kita, Nagoya 462, Japan
Yasuo Shibasaki
Affiliation:
Ceramic Technology Department, National Industrial Research Institute of Nagoya, Kita, Nagoya 462, Japan
Yoshiyuki Sugahara
Affiliation:
Department of Applied Chemistry, Waseda University, Ohkubo, Shinjuku, Tokyo 169, Japan
*
*Present address: Fundamental Technology Research Laboratory, Tokyo Gas Co., Ltd., Shibaura, Minato, Tokyo 105, Japan.
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Abstract

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Kaolinite was hydrothermally synthesized from two kinds of silica-alumina gels to examine the effect of the structure of the starting material. Two kinds of gels were prepared by precipitation at different pH conditions (pH = 9.6 and 4.2) from solutions containing water glass and aluminum sulfate. Na ions in the gels were removed with a resin before the hydrothermal treatment, but a slight amount of sulfate ions was still present in the gels. The nuclear magnetic resonance spectra of the starting gels suggested that the gel prepared at pH 9.6 consists of networks with alternating SiO4- and A1O4-tetrahedra (partially AlO6-octahedra), whereas the gel prepared at pH 4.2 consists of a sheet structure related to allophane. After the hydrothermal treatment at 220°C for 9 days, kaolinite particles with spherical shape were obtained from the former gel, and platy kaolinite was crystallized from the latter one. The difference in morphology of synthetic kaolinite was attributable to the structures of the starting gels, and the pH values in the hydrothermal reactions were not very significant to the morphology.

Type
Research Article
Copyright
Copyright © 1994, Clay Minerals Society

References

Barron, P. F., Wilson, M. A., Campbell, A. S., and Frost, R. L., (1982) Detection of imogolite in soils using solid state 29Si NMR: Nature 299, 616618.CrossRefGoogle Scholar
Barron, P. F., Frost, R. L., Skjemstad, J. O., and Koppi, A. J., (1983) Detection of two silicon environments in kaolins by solid-state 29Si NMR: Nature 302, 4950.CrossRefGoogle Scholar
Cloos, P., Léonard, A. J., Moreau, J. P., Herbillon, A., and Fripiat, J. J., (1969) Structural organization in amorphous silico-aluminas: Clays & Clay Minerals 17, 279287.CrossRefGoogle Scholar
De Kimpe, C., Gastuche, M. C., and Brindley, G. W., (1961) Ionic coordination in alumino-silicic gels in relation to clay mineral formation: Amer. Mineral. 46, 13701381.Google Scholar
De Kimpe, C., and Gastuche, M. C., (1964) Low-temperature syntheses of kaolin minerals: Amer. Mineral. 49, 116.Google Scholar
Ewell, R. H., and Insley, H., (1935) Hydrothermal synthesis of kaolinite, dickite, beidellite, and nontronite: J. Res. Nat. Bur. Stand. 15, 173186.CrossRefGoogle Scholar
Fripiat, J. J., Léonard, A., and Uytterhoeven, J. B., (1965) Structure and properties of amorphous silicoaluminas. II. Lewis and brønsted acid sites: J. Phys. Chem. 69, 32743279.CrossRefGoogle Scholar
Holdridge, D. A., and Vaughan, F., (1957) The kaolin minerals (Kandites): in The Differential Thermal Investigation of Clays, Mackenzie, R. C., ed., Mineralogical Society, London, 98139.Google Scholar
Léonard, A., Suzuki, Sho., Fripiat, J. J., and De Kimpe, C., (1964) Structure and properties of amorphous silicoaluminas. I. Structure from X-ray fluorescence spectroscopy and infrared spectroscopy: J. Phys. Chem. 68, 26082617.CrossRefGoogle Scholar
Lippmaa, E., Mägi, M., Samoson, A., Engelhardt, G., and Grimmer, A.-R., (1980) Structural studies of silicates by solid-state high-resolution 29Si NMR: J. Am. Chem. Soc. 102, 48894893.CrossRefGoogle Scholar
Lippmaa, E., Mägi, M., Samoson, A., Tarmak, M., and Engelhardt, G., (1981) Investigation of the structure of zeolites by solid-state high-resolution 29Si NMR spectroscopy: J. Am. Chem. Soc. 103, 49924996.CrossRefGoogle Scholar
MacKenzie, K. J. D., Bowden, M. E., and Meinhold, R. H., (1991) The structure and thermal transformations of allophanes studied by 29Si and 27Al high resolution solid-state NMR: Clays & Clay Minerals 39, 337346.CrossRefGoogle Scholar
Miyawaki, R., Tomura, S., Shibasaki, Y., and Samejima, S., (1989) Appropriate pH for hydrothermal synthesis of kaolinite from amorphous mixture of alumina and silica: Reports of the Government Industrial Research Institute, Nagoya 38, 330335 (in Japanese with English abstract).Google Scholar
Miyawaki, R., Tomura, S., Samejima, S., Okazaki, M., Mizuta, H., Maruyama, S., and Shibasaki, Y., (1991) Effects of solution chemistry on the hydrothermal synthesis of kaolinite: Clays & Clay Minerals, 39, 498508.CrossRefGoogle Scholar
Pourbaix, M., 1991 ed. () Atlas of Electrochemical in Aqueous Solutions: Pergamon Press, New York, 168–176, 458463 pp.Google Scholar
Roy, R., and Osborn, E. F., (1954) The system Al2O3-SiO2-H2O: Amer. Mineral. 39, 853885.Google Scholar
Thompson, J. G., Philippa, J. R. U., Whittaker, A. K., and Mackinnon, I. D. R., (1992) Structural characterization of kaolinite: NaCl intercalate and its derivatives: Clays & Clay Minerals, 40, 369380.CrossRefGoogle Scholar
Tomura, S., Shibasaki, Y., Mizuta, H., and Kitamura, M., (1983) Spherical kaolinite: Synthesis and mineralogical properties: Clays & Clay Minerals 31, 413421.CrossRefGoogle Scholar
Tomura, S., Shibasaki, Y., Mizuta, H., and Kitamura, M., (1985) Growth conditions and genesis of spherical and platy kaolinite: Clays & Clay Minerals 33, 200206.CrossRefGoogle Scholar
Tsuzuki, Y., (1976) Solubility diagrams for explaining zone sequences in bauxite, kaolin and pyrophyllite-diaspore deposits: Clays & Clay Minerals 24, 297302.CrossRefGoogle Scholar
Van der Marel, H. W., and Beutelspacher, H., 1976 eds. () Atlas of Infrared Spectroscopy of Clay Minerals and Their Admixtures: Elsevier, New York, 6593.Google Scholar
Watanabe, T., and Shimizu, H., (1986) High resolution solid state NMR and its application to clay minerals: J. Mineral Soc. Jpn. 17, 123136 (special issue, in Japanese with English abstract).Google Scholar
Wilson, M. A., McCarthy, S. A., and Fredericks, P. M., (1986) Structure of poorly-ordered aluminosilicates: Clay Miner. 21, 879897.CrossRefGoogle Scholar
Wilson, M. A., Wada, K., Wada, S. I., and Kakuto, Y., (1988) Thermal transformations of synthetic allophane and imogolite as revealed by nuclear magnetic resonance: Clay Miner. 23, 175190.CrossRefGoogle Scholar