The use of clays for the adsorption of contaminants from water has gained significant attention in recent decades. Clays and their modified forms have been extensively studied for their ability to adsorb both inorganic and organic pollutants. The purpose of this study is to investigate the use of montmorillonite (k10), local montmorillonite (MMT-Na), and their 1,10-phenanthroline modified forms (k10-phen and MMT-phen) for the adsorption of iron(II) ions. Adsorption of iron(II) on k10 and MMT-Na has been observed to be physical; however, adsorption on k10-phen is chemical. Nevertheless, iron (II) adsorption on MMT-phen combines physical and chemical adsorption. To characterize all these clays, X-ray diffraction (XRD), Infrared spectroscopy (IR), thermogravimetric analysis (TGA), and BET nitrogen adsorption–desorption isotherm were performed. In order to determine the specific surface area of the clays, the BET and methylene blue methods were used, and both ways were quite similar. A cation exchange capacity (CEC) of 39 meq/100 g for k10 and 85 meq/100 g for MMT-Na is calculated. To optimize the Fe(II) adsorption on clays, pH, clay mass, and contact time were studied. The adsorption isotherms were analyzed using linear and nonlinear Langmuir, Freundlich, Dubinin-Radushkevich, Sips, and Toth isotherms. A study of adsorption kinetics was conducted using linear, nonlinear, and differential pseudo first and second orders. An Elovich model has been applied to the obtained data about chemisorption character. Boyd and Weber& Morris's intraparticle diffusions have also been examined. Upon adsorption of Fe(II) on all clays, the standard free energies were negative, confirming the spontaneous nature of the adsorption process. As a result of the endothermic nature of the adsorption, the enthalpies are positive. In the presence of other cations, k10-phen and MMT-phen demonstrated the most excellent selectivity in uptaking Fe(II).
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