Prior to equilibrium experiments, a clinoptilolite-type Korean natural zeol
ite was pretreated with HCl, NaOH, and NaCl to improve the ion-exchange cap
acity for heavy metals. Single- and multi-species equilibrium data of heavy
metals such as copper, cadmium, cesium, and lead on treated and untreated
natural zeolites were measured experimentally. For single-species equilibri
um data, one of the conventional adsorption isotherms, the Sips equation, w
as used to fit them and then multi-species equilibrium data were predicted
by using the loading ratio correlation (LRC), the ideal adsorbed solution (
IAS) theory, and the real adsorbed solution (RAS) theory based on the Sips
equation. In applying the RAS theory, we used the Wilson equation for fitti
ng activity coefficients of metal ions in the ion-exchanger phase. It was p
roven that basic adsorption models except the LRC model could describe mult
i-species ion-exchange equilibrium for heavy metals/natural zeolite systems
well.