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• W2054799503 abstract "A study of breakthrough curves for cations usually found in acid mine drainage (Pb2+, Cu2+, Zn2+ and H+) and municipal wastewater (NH4+) have been conducted on some natural zeolitic tuffs. The zeolitic tuffs used in this study are: three zeolitic tuffs from Cayo Formation, Guayaquil (Ecuador), characterized by X-ray diffraction as clinoptilolite (sample CLI-1) and heulandite (samples HEU-1 and HEU-2)-rich tuffs, and two zeolitic tuffs from Parnaiba Basin, Belem do Pará (Brazil), characterized as stilbite-rich tuffs (samples STI-1 and STI-2). The clinoptilolite sample CLI-1 shows an exceedingly good exchange capacities for Pb2+ and NH4+ as received, and also a very high exchange capacity for Cu2+ and Zn2+ when conditioned with 2 M sodium chloride, with much higher values than those reported in the literature for other clinioptilolite ores. A general order of effective cation exchange capacity could be inferred from breakthrough curves on these zeolitic tuffs:CLI-1>HEU-2>HEU-1>STI-2 Since it is true for most of the cations studied." @default.
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• W2054799503 date "2009-07-30" @default.
• W2054799503 modified "2023-10-02" @default.
• W2054799503 title "Continuous elimination of Pb2+, Cu2+, Zn2+, H+ and NH4+ from acidic waters by ionic exchange on natural zeolites" @default.
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• W2054799503 doi "https://doi.org/10.1016/j.jhazmat.2008.11.087" @default.
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