@article{
author = "Radojević, Zagorka and Kostić-Gvozdenović, L. and Tecilazic-Stevanović, M",
year = "1999",
abstract = "The aim of this paper is to contribute to the knowledge of the quantitative formulation of the ion exchange reaction in clays. The equilibrium was studied at 11 degrees C in a system of solutions of NaCl and MgCl2, the concentrations of which never exceeded 0.1 mol/dm(3), and the "Jelenkovac" montmorillonite, the particle size of which was below 2 mu m. The standard reaction Gibbs energy of the Mg-Na exchange determined by applying the Gapon equation (Delta(r)G(Mg)(0Na) = 11.9 kJ/mol) and that obtained according to Levy-Shainberg (Delta(r)G(Mg)(0Na) = 10.5 kJ/mol) showed a large degree of concordance. The latter method also includes the exchangeable ion activity coefficient obtained from ion-clay interaction data which includes data on the thickness of the intel layer space in the montmorillonite structure, as well as the thickness of the basis montmorillonite layer itself.",
publisher = "Srpsko hemijsko društvo, Beograd",
journal = "Journal of the Serbian Chemical Society",
title = "The standard reaction Gibbs energy of the cation exchange reaction of the biionic (Mg,Na)-form of montmorillonite",
pages = "213-207",
number = "3",
volume = "64",
url = "https://hdl.handle.net/21.15107/rcub_rims_14"
}