Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
202536 | Fluid Phase Equilibria | 2014 | 9 Pages |
In this work, ion exchange equilibrium in NaY-packed columns was examined and equilibrium data was generated for Na+ ↔ Fe2+ in zeolite. In this context, different mathematical models were evaluated to describe the equilibrium: the through adsorption approach (Langmuir type model, Jain & Snoeyink model and Langmuir–Freundlich model), the ion exchange approach (the ideal and non-ideal mass action law) and the thermodynamic approach (IAST—ideal adsorbed solution theory and RAST—real adsorbed solution theory). Experiments were carried out at 30 °C using solutions of 1, 2 and 3 meq L−1 at pH 4.5 and a column flow rate of 8 mL min−1. Fe(II) was retained through ion exchange followed by adsorption. The non-ideal mass action law best fit the experimental data as it predicted the exchange process of electrolytes and detected the adsorption multilayer.