Chemical Speciation of Arsenic-Accumulating Mineral in a Sedimentary Iron Deposit by Synchrotron Radiation Multiple X-ray Analytical Techniques

The comprehensive characterization of As(V)-bearing iron minerals from the Gunma iron deposit, which were probably formed by biomineralization, was carried out by utilizing multiple synchrotron radiation (SR)-based analytical techniques at BL37XU at SPring-8. SR microbeam X-ray fluorescence (SR-μ-XR...

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Published inEnvironmental science & technology Vol. 42; no. 19; pp. 7152 - 7158
Main Authors Endo, Satoshi, Terada, Yasuko, Kato, Yasuhiro, Nakai, Izumi
Format Journal Article
LanguageEnglish
Published Washington, DC American Chemical Society 01.10.2008
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Summary:The comprehensive characterization of As(V)-bearing iron minerals from the Gunma iron deposit, which were probably formed by biomineralization, was carried out by utilizing multiple synchrotron radiation (SR)-based analytical techniques at BL37XU at SPring-8. SR microbeam X-ray fluorescence (SR-μ-XRF) imaging showed a high level of arsenic accumulation in the iron ore as dots of ca. 20 μm. Based on SEM observations and SR X-ray powder diffraction (SR-XRD) analysis, it was found that arsenic is selectively accumulated in strengite (FePO4·2H2O) with a concentric morphology, which may be produced by a biologically induced process. Furthermore, the X-ray absorption fine structure (XAFS) analysis showed that arsenic in strengite exists in the arsenate (AsO4 3−) form and is coordinated by four oxygen atoms at 1.68 Å. The results suggest that strengite accumulates arsenic by isomorphous substitution of AsO4 3− for PO4 3− to form a partial solid-solution of strengite and scorodite (FeAsO4·2H2O). The specific correlation between the distribution of As and biominerals indicates that microorganisms seems to play an important role in the mineralization of strengite in combination with an arsenic-accumulating process.
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ISSN:0013-936X
1520-5851
DOI:10.1021/es8006518