4.7 Article

Abiotic reduction of antimony(V) by green rust (Fe-4(II)Fe-2(III)(OH)(12)SO4 center dot 3H(2)O)

Journal

CHEMOSPHERE
Volume 70, Issue 5, Pages 942-947

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.chemosphere.2007.07.021

Keywords

antimony; green rust; XAFS; HPLC-ICP-MS

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Green rust (Fe-4(II)Fe-2(III)(OH)(12)SO4 center dot 3H(2)O) is an intermediate phase in the formation of iron (oxyhydr)oxides such as goethite, lep-idocrocite, and magnetite. It is widely considered that green rust occurs in many soil and sediment systems. Green rust has been shown to reduce sorbed Se(VI), Cr(VI), and U(VI). In addition, it is also reported that green rust does not reduce As(V) to As(III). In this study, we have investigated for the first time the interaction between Sb(V) and green rust using XAFS and HPLC-ICP-MS. Most of the added Sb(V) was adsorbed on green rust, and Sb(III), a reduced form, was observed in both solid and liquid phases. Thus, it was shown that green rust has high affinity for Sb(V), and that Sb(V) was reduced to more toxic Sb(III) by green rust despite the high stability of the Sb(V) species even under reducing condition as reported in previous studies. Therefore, green rust can be one of the most important reducing agents for Sb(V), which can influence the Sb mobility in suboxic environments where green rust is formed. (c) 2007 Elsevier Ltd. All rights reserved.

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