Potassium-exchange behaviour of an illite.

Authors

  • J.C.H. van Schouwenburg
  • A.C. Schuffelen

DOI:

https://doi.org/10.18174/njas.v11i1.17567

Abstract

The specificity of K adsorption on illite with respect to divalent cations can be explained by accepting the existence of three types of exchange sites, each of which shows a normal exchange process which may be described with the Gapon exchange equation. The K exchange on illite can be described mathematically as the sum of these three processes. Proof of the validity of the mathematical expression is presented. (Abstract retrieved from CAB Abstracts by CABI’s permission)

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Published

1963-02-01

Issue

Vol. 11 No. 1 (1963)

Section

Papers

License

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