作者: Christopher J. Gabelich , Fredrick W. Gerringer , Connie C. Lee , William R. Knocke
DOI: 10.1002/J.1551-8833.2006.TB07665.X
关键词: Nuclear chemistry 、 Desorption 、 Alum 、 Chloride 、 Mineralogy 、 Chlorine 、 Ferric 、 Manganese 、 Aluminium sulfate 、 Sand filter 、 Chemistry 、 General chemistry 、 Water Science and Technology
摘要: The Metropolitan Water District of Southern California carried out a study to evaluate manganese (Mn) desorption from filter media during biological filtration startup. Mn contamination the was by-product prior use ferric chloride (FeC13), which contains Mn, for coagulation and free chlorine exposure. During pilot- full-scale testing at pH 6.5, FeCl 3 (without chlorine) released soluble nearly four times level by aluminum sulfate (alum; 105 μg/L 27 alum). Pilot-scale experiments demonstrated that present in column three valence states [Mn(ll), Mn(lll), Mn(IV)]. Mn(ll) influent . on anthracite hypothesized be Mn(II)/Mn(IV) first physically displaced iron, aluminum, hydrogen, then catalytically oxidized Mn(IV) silica sand.