“…Therefore, the low-silicon calcium variety of clinoptilolite, to which Transcarpathian clinoptilolite belongs, after converting it into the sodium form, shows increased efficiency of cation exchange, in particular, increased selectivity to multi-charged cations. It is well known that Na-forms of clinoptilolite have markedly different sorptive characteristics than unmodified clinoptilolite, and they typically have a greater sorption capacity towards cations of d- and f-transition elements [ [30] , [31] , [32] , [33] , [34] , [35] , [36] ].…”