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Interstratified Clay Minerals

  • Chapter
Soil Components

Abstract

Interstratification is a phenomenon that was first observed on studying clay minerals by X-ray diffraction. It was noted that the majority of them had basal reflections (001), which did not form a regular series. It was verified that this irregularity was due to the interstratification of different types of crystalline layers.

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  1. D. M. C. MacEwan
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  1. University of Illinois, Urbana, Illinois, USA

    John E. Gieseking (Professor of Soil Chemistry) (Professor of Soil Chemistry)

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MacEwan, D.M.C., Ruiz-Amil, A. (1975). Interstratified Clay Minerals. In: Gieseking, J.E. (eds) Soil Components. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-65917-1_8

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