4.8 Article

Removal of dissolved metals by zero-valent iron (ZVI): Kinetics, equilibria, processes and implications for stormwater runoff treatment

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WATER RESEARCH
卷 39, 期 17, 页码 4153-4163

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.watres.2005.07.040

关键词

adsorption; cementation; heavy metals; iron corrosion; runoff pollutants; zero-valent iron (ZVI)

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Infiltration of stormwater runoff contaminated with metals is often questionable in several cases due to its long-term potential to cause deterioration of groundwater quality. To ensure the quality of filtrate, a pre-treatment of contaminated runoff is required. This study investigates the processes of copper and zinc ion removal from stormwater runoff using zero-valent iron (ZVI, Fe-0). Kinetic and equilibrium tests were performed with laboratory-prepared and in situ stormwater runoff samples collected from roof, street and highway catchments. Based on the results, a substantial portion of Cu2+ is reduced and transformed to insoluble forms of Cu-0 and Cu2O, Unlike copper, the adsorption and co-precipitation associated with freshly precipitated iron oxides play important roles for the removal of Zn2+. Investigations under various water quality conditions demonstrated a relatively minor impact on Cu2+ uptake rates. However, the different conditions apparently altered the removal stoichiometry and phases of the copper deposits. The removal rates of Zn2+ increase with higher dissolved oxygen (DO), ionic strength (IS), temperature (7) and pH. Dissolved organic carbon (DOC) in runoff samples forms complexes with metals and Fe, thereby kinetically decreasing the metal uptake rates. Furthermore, depending on its composition, a larger molecular weight organic fraction was found to preferentially compete for the adsorption sites. The study demonstrates that ZVI is a promising medium for achieving comparable capacity to a commercial adsorbent like granular ferric hydroxide (GFH). Longterm performance of ZVI, however, may be limited and governed by the formation of non-conductive layers of iron and cuprous oxides. (c) 2005 Elsevier Ltd. All rights reserved.

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