Cancès B, Juillot F, Morin G, Laperche V, Alvarez L, Proux O, Hazemann J L, Brown G E, Calas G
Institut de Minéralogie et de Physique des Milieux Condenses, UMR CNRS 7590, 140 rue de Lourmel, 75015 Paris, France.
Environ Sci Technol. 2005 Dec 15;39(24):9398-405. doi: 10.1021/es050920n.
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.
通过将传统技术(X射线衍射、选择性化学萃取)与X射线吸收光谱法(XAS)相结合,已确定了法国奥宗附近中央地块一个受砷基农药影响的土壤剖面中砷的分子水平形态。顶部的砷浓度非常高(>7000 mg kg⁻¹),并迅速向下降低至每千克几百毫克。在10厘米深处发现了一层薄薄的水砷铅矿(PbHAsO₄),这是一种直到20世纪中叶还常用作杀虫剂的砷酸铅。尽管存在这种含砷矿物,但草酸盐萃取表明,超过65%的砷在无定形铁氧化物溶解时被释放出来,这表明在土壤剖面中砷主要与这些相缔合。由于草酸盐萃取不能明确区分砷的各种化学形态,这些结果通过使用XAS分析直接原位测定砷形态得到了证实。XANES数据表明,除了表层土壤样品中检测到少量(7%)的As(III)外,沿土壤剖面砷主要以As(V)形式存在。土壤样品的EXAFS光谱通过模型化合物光谱的线性组合和逐壳法进行拟合。这些程序清楚地证实,在土壤剖面中,As(V)主要(至少80 wt%)与无定形Fe(III)氧化物以共沉淀形式缔合。通过X射线衍射在一个单独的白色薄层中证实的水砷铅矿,如果有的话,在土壤样品中所占砷的比例不超过10 wt%。这项研究强调了铁氧化物在限制因用作农药并释放到土壤中的主要含砷固体溶解后砷在土壤中扩散方面的重要性。