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Clay Minerals; June 2003; v. 38; no. 2; p. 233-242; DOI: 10.1180/0009855033820092
© 2003 Mineralogical Society of Great Britain and Ireland
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A new way of assessing clay cation adsorption using normalized salt concentration

J.-L. BERSILLON*, F. VILLIÉRAS, L. MICHOT and J.-M. CASES

Laboratoire Environnement et Minéralurgie, UMR 7569 CNRS - INPL, Centre de Recherche François Fiessinger, 15 avenue du Charmois, BP 40, F- 54501 Vandoeuvre cedex, France

* E-mail: jean-luc.bersillon{at}ensg.inpl-nancy.fr

(Received 16 November 2001; revised 6 December 2002)

Kaolinite cation adsorption data are processed using recent gas adsorption concepts such as the undersaturation {Delta}µ= ln (C/Cs) and the monolayer coverage {theta}. This process shows that using the proper reference phase through its solubility Cs, it is possible to characterize adsorption sites that have the same adsorption energy regardless of the nature of the cation. Under mildly acidic conditions, a single ‘Langmuirian’ site category fits cation adsorption data whereas another family of sites is revealed in mildly alkaline conditions. These results suggest that at mildly acidic pH, only silanol sites are available to ion exchange and adsorption whereas at higher pH, a wider range of sites is made available, some of them displaying the same average adsorption energy and the others constituting a different category of sites with a much lower adsorption energy. This latter category is attributed to the aluminol sites.

KEYWORDS: kaolinite, ion adsorption, soil science, environmental science







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