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Mechanisms of Adhesion to Clays, with Reference to Soil Systems

  • Chapter
Bacterial Adhesion

Abstract

Soil is undoubtedly the most complex of all microbial habitats. Primarily because of this complexity, there is insufficient information on how and where most microbial events—including adhesion—occur in soil in situ and which microbes are numerically and physiologically the most important participants in these events. The abiotic components of soil have been relatively well defined, both qualitatively and quantitatively. However, the micro-geographic distribution and the geometric relations of abiotic components to each other, and to the microbiotic component, and the interactions among and between the abiotic and microbiotic components are not clearly defined. Most of what is known about the composition of the abiotic components has been obtained by dispersing soil (either chemically or physically, including sonically) and, after careful fractionation, conducting detailed chemical (both inorganic and organic) and physical analyses on the individual fractions (see Marshall, 1964; Rich and Kunze, 1964; Black, 1965; Schnitzer and Kahn, 1972; Gieseking, 1975; Dixon and Weed, 1977; Greenland and Hayes, 1978; Stevenson, 1982).

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  1. Laboratory of Microbial Ecology, Department of Biology, New York University, New York, New York, 10003, USA

    G. Stotzky

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  1. University of Illinois, Urbana, Illinois, USA

    Dwayne C. Savage

  2. University of Warwick, Coventry, England

    Madilyn Fletcher

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Stotzky, G. (1985). Mechanisms of Adhesion to Clays, with Reference to Soil Systems. In: Savage, D.C., Fletcher, M. (eds) Bacterial Adhesion. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-6514-7_8

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  • Print ISBN: 978-1-4615-6516-1

  • Online ISBN: 978-1-4615-6514-7

  • eBook Packages: Springer Book Archive

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