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1 National Technical University of Athens, Laboratory of Metallurgy, 15780 Zografos, Greece
2 Technical University of Crete, Department of Mineral Resources Engineering, 73100 Chania, Greece
E-mail address of corresponding author: moirou{at}metal.ntua.gr
This paper examines the ion-exchange properties of synthetic zeolite Na-Pc, which was produced from perlite-waste fines and has a SiO2:Al2O3 ratio of 4.45:1 and a cation-exchange capacity (CEC) of 3.95 meq g1. Although equilibrium is attained rapidly for all three metals, exchange is incomplete, with Ac(max) (maximum equilibrium fraction of the metal in the zeolite) being 0.95 for Pb, 0.76 for Zn, and 0.27 for Ni. In both Na
Pb and Na
Zn exchange, the normalized selectivity coefficient is virtually constant for NAc (normalized equilibrium fraction of the metal in the zeolite) values of
0.6, suggesting a pronounced homogeneity of the available exchange sites. The Gibbs standard free energy,
G°, of the Na
Pb exchange calculated from the normalized selectivity coefficient is 3.11 kJ eq1 and, for the Na
Zn exchange, it is 2.75 kJ eq1.
Examination of the solid exchange products with X-ray diffraction (XRD) revealed a possible decrease in crystallinity of zeolite Pb-Pc as suggested by the significant broadening and disappearance of diffraction lines. This decrease is associated with a reduction of pore opening, as indicated from Fourier-transform infrared analysis (FTIR), which in turn results in a decrease of the amount of zeolitic water. Thermogravimetric-differential thermogravimetric (TG-DTG) analysis showed that water loss occurs in three steps, the relative significance of which depends on the type of exchangeable cation and subsequently on the type of complex formed with the cation and/or the zeolite channels. Zeolite Na-Pc might be utilized in environmental applications, such as the treatment of acid-mine drainage and electroplating effluents.
Key Words: Heavy Metals Ion Exchange Perlite Selectivity Selectivity Coefficient Zeolite Pc Zeolitization
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