Study of lithium ion exchange by two synthetic zeolites: Kinetics and equilibrium
Metadatos
Mostrar el registro completo del ítemAutor
Navarrete Casas, Ricardo; Navarrete Guijosa, Antonio; Valenzuela Calahorro, Cristóbal; López-González, Juan de Dios; García Rodríguez, AntonioEditorial
Elsevier
Fecha
2006Referencia bibliográfica
Published version: R. Navarrete-Casas et al., Study of lithium ion exchange by two synthetic zeolites:Kinetics and equilibrium, Journal of Colloid and Interface Science (2006), doi:10.1016/j.jcis.2006.10.002
Resumen
We examined the exchange of univalent cations (Na+ and H+) retained on two commercially available synthetic zeolites with Li+ ions present in aqueous solutions in contact with the solids with a view to preparing effective controlled–release pharmaceutical forms. The studied zeolites were manufactured by Merck and featured channel diameters of 0.5 (Zeolite 5A, Ref. 1.05705.250, designated Z-05 in this work) and 1.0 nm (Zeolite 13X, Ref. 1.05703.250, designated Z-10 here). The XRD technique revealed that Z-05 possesses an LTA structure derived from that of sodalite and Z-10 a faujasite-type structure. Their exchange capacities were found to be 2.72 and 3.54 meq/g. The Z-Na + Li+/ZLi+ Na+ and Z-H+Li+/Z-Li+H+ ion-exchange processes were found to be reversible and their kinetic laws to obey the equation (−dC/dt) = ka ·Cn · (1−θ)−(kd · θ), with n = 1 for Z-10 and n = 2 for Z-05. Based on the equilibrium results, the overall processes involve one (with Z-05) or two single ion-exchange processes (with Z-10). In both cases, the equations that govern equilibrium are direct results of the kinetic laws. Thus, the first process—the one with only Z-05—involves the retention of Li+ cations at anionic sites on the outer surface of the solid and their access to the larger pores; the second process—which occurs with Z-10 only—involves the retention of lithium(I) cations within the zeolite channels. In both systems, the exchange with Li+ (from the aqueous solution) is easier than that with H+; this is consistent with our kinetic, equilibrium, and thermodynamic results.