Ion-exchange equilibria and exchange heats on clinoptilolite involving singly-charged cations

Isotherms and integral heats of exchange of alkali metal, ammonium, and silver cations on sodium clinoptilolite were measured. Exchange involving K₊, NH₄ ⁺, Cs⁺, and Ag⁺ displacing cations was found to be exothermic for all occupancies of the clinoptilolite exchange sites. Exchange was exothermic for Li₊ cations up to = 0.15. The dependence of the differential ion-exchange heats on was determined. Clinoptilolite was found to have two types of exchange sites with different heats of ion exchange. The experimental data were used to calculate the selectivity coefficients, thermodynamic constants, and ion-exchange entropy. These findings are discussed relative to the differences in the cation properties and structural features of clinoptilolite.A. V. Dumanskii Institute of Colloid Chemistry and the Chemistry of Water, National Academy of Sciences of Ukraine, 42 Prospekt Akademika Vernadskogo, 252680 Kiev-142, Ukraine. Translated from Teoreticheskaya i Éksperimental'naya Khimiya, Vol. 32, No. 5, pp. 315–319, September–October, 1996. Original article submitted February 12, 1996.