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.
引用
收藏
页码:9398 / 9405
页数:8
相关论文
共 41 条
  • [11] Jackson M. L., 1986, Methods of soil analysis. Part 1. Physical and mineralogical methods, P101
  • [12] Remobilization of arsenic from buried wastes at an industrial site: mineralogical and geochemical control
    Juillot, F
    Ildefonse, P
    Morin, G
    Calas, G
    de Kersabiec, AM
    Benedetti, M
    [J]. APPLIED GEOCHEMISTRY, 1999, 14 (08) : 1031 - 1048
  • [13] Validation of an arsenic sequential extraction method for evaluating mobility in sediments
    Keon, NE
    Swartz, CH
    Brabander, DJ
    Harvey, CF
    Hemond, HF
    [J]. ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2001, 35 (13) : 2778 - 2784
  • [14] REFINEMENT OF CRYSTAL-STRUCTURE OF SCORODITE
    KITAHAMA, K
    KIRIYAMA, R
    BABA, Y
    [J]. ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1975, 31 (JAN15): : 322 - 324
  • [15] Mechanism of anion retention from EXAFS and density functional calculations: Arsenic (V) adsorbed on gibbsite
    Ladeira, ACQ
    Ciminelli, VST
    Duarte, HA
    Alves, MCM
    Ramos, AY
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 2001, 65 (08) : 1211 - 1217
  • [16] LAPERCHE V, 200111 CNRSSP, P1
  • [17] Stability of lead(II) arsenates
    Magalhaes, MCF
    Silva, MCM
    [J]. MONATSHEFTE FUR CHEMIE, 2003, 134 (05): : 735 - 743
  • [18] THE MECHANISM OF ANION ADSORPTION ON IRON-OXIDES - EVIDENCE FOR THE BONDING OF ARSENATE TETRAHEDRA ON FREE FE(O,OH)(6) EDGES
    MANCEAU, A
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (17) : 3647 - 3653
  • [19] *MIN AM TERR ENV, 1996, REC SIT SOLS POLL
  • [20] Morin G, 1999, AM MINERAL, V84, P420