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Swelling clays and related complex layered oxides

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Chemical Physics of Intercalation

Part of the book series: NATO ASI Series ((NSSB,volume 172))

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Abstract

The geological term “clay” refers to any naturally occuring material with a particle size less than 2μ. However, the term “clay mineral” refers to a specific composition of matter and a discrete structure, but with a particle size less than 2μ. Clay minerals are usually layered oxides. Included in this family are the layered silicate clays.

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Author information

Authors and Affiliations

  1. Department of Chemistry and Center for Fundamental Materials Research, Michigan State University, East Lansing, MI, 48824, USA

    Thomas J. Pinnavaia

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  1. Thomas J. Pinnavaia
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Editor information

Editors and Affiliations

  1. ESPCI, Paris, France

    A. P. Legrand

  2. Domaine Universitaire, Talence, France

    S. Flandrois

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Pinnavaia, T.J. (1987). Swelling clays and related complex layered oxides. In: Legrand, A.P., Flandrois, S. (eds) Chemical Physics of Intercalation. NATO ASI Series, vol 172. Springer, Boston, MA. https://doi.org/10.1007/978-1-4757-9649-0_12

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  • DOI: https://doi.org/10.1007/978-1-4757-9649-0_12

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4757-9651-3

  • Online ISBN: 978-1-4757-9649-0

  • eBook Packages: Springer Book Archive

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