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University of Louvain, Soil Science Unit
IRFA/CIRAD, Place Croix du Sud 2, B-1348 Louvain-la-Neuve, Belgium
*Corresponding author.
ABSTRACT
Ion exchange equilibria involving K cannot be described by a constant selectivity coefficient for all surface compositions. The main reason is that the soil exchanger contains various types of sites with different affinities for K ions. This paper makes use of a multi-site model, the main assumption of which is that the exchange reaction is governed by single values of the Vanselow selectivity coefficient, Kv, for each type of site. The simplest model—i.e., the two-site model—is tested. Three parameters must be adjusted: the proportion of high and low selective sites, and the Kv's for these two classes of sites. Simulated K-Ca exchange isotherms are shown, with various combinations of the parameters. The model has been adjusted to experimental K-Ca exchange data, using a non-linear regression procedure. A fair agreement between the experimental and calculated curves is obtained. As a consequence, this simple model proves to be a powerful tool for a quantitative description of exchange data involving K ions.
Received for publication October 14, 1988.
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