Abstract

A novel mechanism for the effect of ferrous iron (Fe2+) on low-pressure ultrafiltration membrane (LPM) flux is discovered in this study. In previous studies, the Fe2+ concentrations of removing excessive Fe2+ and manganese (Mn2+) by LPM are low (0.4−1.5 mg L−1), and the presence of Fe2+ would reduce the flux, thus not suitable for treating water with high Fe2+ concentrations. In this study, we systematically investigated the performance of down-flow LPM (D-LPM) and opposite-flow LPM (O-LPM) under different Fe2+ concentrations (0−5 mg L−1) with Mn2+ and ammonia (NH4+). The results demonstrate that the flux did decrease at low Fe2+ concentration, while significantly increasing by 95.9% with Fe concentration at 3−5 mg L−1. Furthermore, high Fe2+ enhanced Fe, Mn2+, and NH4+ removal by iron autocatalytic oxidation, enriching the relative abundance of manganese-oxidizing bacteria, and facilitating anammox activities, respectively. A series of characteristic analyses suggest that thin biofilm layer structures in D-LPM and O-LPM, along with the low soluble microbial products-polysaccharide concentrations, resulted in the high steady flux under high Fe2+ concentrations. These findings widen the applicability of LPM in practical applications and provide novel strategies to increase the flux of LPM systems.

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