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Quantitative mineralogical analysis of ‘blue clay’ from vonšov, bohemia: a comparative study by nine laboratories

Published online by Cambridge University Press:  14 March 2018

J. Konta
J. Konta*
Affiliation:
Institute of Petrology, Charles University, Prague
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Abstract

Samples of ‘blue clay’ were distributed among nine laboratories in various countries to assess the possibility of quantitative mineralogical determination. The disordered form kaolinite commonly found in fireclays and illite, or mica, were found by all laboratories, as was a material variously described as montmorillonite, swelling material (vermiculite, beidellite or open illite), or intermediate or swelling illite. The next most abundant mineral was quartz. Opal, chlorite, felspar, anatase, and organic matter, all in small quantities, were not all found by any laboratory and traces of calcite and dolomite were observed in one only. The most effective procedure is discussed, and it is concluded that the results are of a semi-quantitative rather than a quantitative nature.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 5 , Issue 30 , December 1963 , pp. 255 - 264
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1963

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References

Brindley, G. W., 1961. The X-ray Identification and Crystal Structures of Clay Minerals (Brown, G., editor). Mineralogical Society, London. 2nd Edition, Chapter XIV, p. 489.Google Scholar
Brindley, G. W., and Kijrtossy, S. S., 1961. Amer. Mitt., 46, 1205.Google Scholar
Dyal, R. S., and Hendricks, S. B., 1950. Soil Sci., 69, 421.CrossRefGoogle Scholar
Hofmann, U., Ernst, TH., and Zwetsch, A., 1958. Vergleichende Priifung der Verfahren zur quantitativen Mineralanalyse bei Tonen und Kaolinen. Fachausschussbericht dtsch, keram. Ges., No. 12.Google Scholar
Hofmann, U., and Haacke, H., 1962. Ber. dtsch, keram. Ges., 39, 41.Google Scholar
Konta, J., 1957. Clay Minerals of Czechoslovakia. Naklad. CSAV, Prague.Google Scholar
Konta, J., 1961. Amer. Min., 46, 289.Google Scholar
Konta, J., 1962. Imbibometry—Study of Argillaceous rocks on Ground Flat Sections. Acta Univ. Carol. Geol., Monographia 1.Google Scholar
Konta, J., and Kužvart, M., 1956. Univ. Carol., Geol., 2, 171.Google Scholar
Mackenzie, R. C., 1961. Acta Univ. CaroL, Geol., Suppl 1, p. 11.Google Scholar
van der Marel, H. W., 1961. Acta Univ. Carol., Geol., Suppl. 1, p. 23.Google Scholar
Oki, Y., Oki, S., and Shibata, H., 1962. Bull. chem. Soc. Japan, 35, 273.Google Scholar
Wiegmann, J., and Kranz, G., 1961. Ber. dtsch, keram. Ges., 38, 294.Google Scholar