XAS evidence of As(V) association with iron oxyhydroxides in a contaminated soil at a former arsenical pesticide processing plant

被引:120
作者
Cancès, B
Juillot, F
Morin, G
Laperche, V
Alvarez, L
Proux, O
Hazemann, JL
Brown, GE
Calas, G
机构
[1] CNRS, UMR 7590, Inst Mineral & Phys Milieux Condenses, F-75015 Paris, France
[2] Ctr Natl Rech Sites & Sols Pollues, F-59505 Douai, France
[3] Bur Rech Geol & Minieres, EPI ENV, F-45050 Orleans, France
[4] European Synchrotron Radiat Facil, F-38000 Grenoble, France
[5] Univ Grenoble 1, UMR CNRS, Lab Geophys Interne & Tectonophys, F-38400 St Martin Dheres, France
[6] CNRS, Lab Cristallog, F-38042 Grenoble 09, France
[7] Stanford Univ, Dept Geol & Environm Sci, Surface & Aqueous Geochem Grp, Stanford, CA 94305 USA
[8] SLAC, Stanford Synchrotron Radiat Lab, Menlo Pk, CA 94025 USA
关键词
D O I
10.1021/es050920n
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The molecular-level speciation of arsenic has been determined in a soil profile in the Massif Central near Auzon, France that was impacted by As-based pesticides by combining conventional techniques (XRD, selective chemical extractions) with X-ray absorption spectroscopy (XAS). The arsenic concentration is very high at the top (>7000 mg kg(-1)) and decreases rapidly downward to a few hundreds of milligrams per kilogram. A thin layer of schultenite (PbHAsO4), a lead arsenate commonly used as an insecticide until the middle of the 20th century, was found at 10 cm depth. Despite the occurrence of this As-bearing mineral, oxalate extraction indicated that more than 65% of the arsenic was released upon dissolution of amorphous iron oxides, suggesting a major association of arsenic with these phases within the soil profile. Since oxalate extraction cannot unambiguously distinguish among the various chemical forms of arsenic, these results were confirmed by a direct in situ determination of arsenic speciation using XAS analysis. XANES data indicate that arsenic occurs mainly as As(V) along the soil profile except for the topsoil sample where a minor amount (7%) of As(III) was detected. EXAFS spectra of soil samples were fit by linear combinations of model compounds spectra and by a shell-by-shell method. These procedures clearly confirmed that As(V) is mainly(at least 80 wt%) associated with amorphous Fe(III) oxides as coprecipitates within the soil profile. If any, the proportion of schultenite, which was evidenced by XRD in a separate thin white layer, does not account for more than 10 wt % of arsenic in soil samples. This study emphasizes the importance of iron oxides in restricting arsenic dispersal within soils following dissolution of primary As-bearing solids manufactured for use as pesticides and released into the soils.
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页码:9398 / 9405
页数:8
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