Abstract

Copper adsorption by and desorption from clinoptilolite (natural zeolite) are reflected in this document. The Ca, Mg, and Na release from the substrate, Si, Al dissolution, and Cl −, NO 3 −, SO 4 2− movement were examined. Experimental variables were Cu concentration and electrolyte anion. Three different electrolytes of 0.01 N were used (KCl, KNO 3, K 2SO 4). Tested solutions had different pH values due to different Cu concentrations used. Thus, solution pH was also taken as a variable, and the effects of [H +] differentiation on Cu adsorption and on Si/Al dissolution were also examined. Copper adsorption was found to be higher when KNO 3 was used as electrolyte, compare to KCl and K 2SO 4, which gave almost equal Cu adsorption. Copper desorption follows the order: K 2SO 4>KNO 3>KCl. Large amounts of K + from bulk solution were also adsorbed by the substrate. The dissolution of Al from the zeolitic framework during Cu adsorption was enhanced in the presence of SO 4 2− ions, whereas the presence of Cl − limited the dissolution. The dissolution of Si from the zeolite framework was not found to be affected by the three anions. Cl − and NO 3 − ions were adsorbed by the substrate whereas, SO 4 2− ions were not. From the study of FTIR spectra significant changes for the bands assigned to Si–OH–Al bridges and to hydrogen bonds at the region between 3650 and 3400 cm −1 were observed. After Cu adsorption the monomeric H-bonds for samples in K 2SO 4, are not as extensively destroyed as those for samples in KCl and KNO 3. Such a destruction is a reflection of the extent of Cu 2+ adsorption and on the impact of Cl − and NO 3 −.

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