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Mineralogical Composition of Structural Clay Products

  • Wayne Ernest Brownell
Part of the Applied Mineralogy book series (MINERALOGY, volume 9)

Abstract

When clay materials are tempered with water to produce the plasticity necessary for proper workability, it is the clay minerals that are responsible for these properties. To understand the interaction between clay minerals and water, it is necessary to know the crystal structures of the various clay minerals. In addition, many of the disilicate minerals other than those of clays are often found in, or added to, the raw materials for structural clay products. These other disilicate minerals are of more concern in the firing operation than in the development of plasticity, but the crystal structures of these minerals, as well as the clays, is important in following the progress of the high-temperature reactions. The structural clay products engineer and scientist cannot solve the technical problems that arise without a good foundation in the crystal structures of the disilicate minerals.

Keywords

Clay Mineral Mineralogical Composition Octahedral Sheet Interlayer Cation Wall Tile 
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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References

  1. 1.
    Pauling, L.: The structure of micas and related minerals. Proc. Nat. Acad. Sci., U.S. 16, 123 (1930).CrossRefGoogle Scholar
  2. 2.
    Brindley, G. W., and K. Robinson: Randomness in the structures of kaolinitic clay minerals. Trans. Faraday Soc. 42B, 198–204 (1946).CrossRefGoogle Scholar
  3. 3.
    Weir, A. H., and R. Greene-Kelly: Beidellite. Am. Min. 47, 137–45 (1962).Google Scholar
  4. 4.
    Phillips, G. C., Jr.: Behavior of Illite on Heating. M.S. Thesis, N.Y. State College of Ceramics, June, 1964.Google Scholar
  5. 5.
    Yoder, H. S., Jr.: Experimental Studies on Micas: a Synthesis, in Clays and Clay Minerals, E. Ingerson, ed., pp. 42–60. New York: Pergamon Press. 1959.Google Scholar
  6. 6.
    Brindley, G. W., ed., X-ray Identification and Crystal Structures of Clay Minerals, pp. 199–212. London: The Mineralogical Soc. 1951.Google Scholar
  7. 7.
    Gruner, J. W.: The structures of vermiculite and their collapse by dehydration. Am. Min. 19, 557–75 (1934).Google Scholar
  8. 8.
    Brown, B. E., and S. W. Bailey: Chlorite polytypism, I, regular and semirandom one-layer structures. Am. Min. 47, 819–50 (1962).Google Scholar
  9. 9.
    Nelson, B. W., and R. Roy: Synthesis of the chlorites and their structural and chemical constitution. Am. Min. 43, 707–25 (1958).Google Scholar
  10. 10.
    Mackenzie, R. C.: Classification and nomenclature of clay minerals. Clay Min. Bull. 4, 52–66 (1959).Google Scholar
  11. 11.
    Lazarenko, E. K.: Nomenclature and classification of clay minerals. Clay Min. Bull. 4, 67–68 (1959).Google Scholar
  12. 12.
    Emrich, E. W.: History and development of ceramic wall tile bodies in the United States. Am. Ceram. Soc. Bull. 52, 687–88 (1973).Google Scholar

Copyright information

© Springer-Verlag/Wien 1976

Authors and Affiliations

  • Wayne Ernest Brownell
    • 1
  1. 1.New York State College of Ceramics at Alfred UniversityAlfredUSA

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