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EXAFS Analysis of Arsenite Adsorption onto Two-Line Ferrihydrite,Hematite,Goethite,and Lepidocrocite

机译:两线水铁矿,赤铁矿,针铁矿和纤铁矿上砷吸附的EXAFS分析

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摘要

The modes of As(III)sorption onto two-line ferrihydrite(Fh),hematite(Hm),goethite(Gt),and lepidocrocite(Lp)have been investigated under anoxic condition using X-ray absorption spectroscopy(XAS).X-ray absorption near-edge structure spectroscopy(XANES)indicates that the absence of oxygen minimized As(III)oxidation due to Fenton reactions.Extended X-ray absorption fine structure spectroscopy(EXAFS)indicates that As(III)formssimilarinner-sphere surface complexes on two-line ferrihydrite and hematite that differ from those formed on goethite and lepidocrocite.At high surface coverage,the dominant complex types on Fh and Hm are bidentate mononuclear edge-sharing(~2E)and bidentate binuclear corner-sharing(~2C),with As-Fe distances of 2.90 +-0.05 and 3.35 +-0.05 A,respectively.The same surface complexes are observed for ferrihydrite at low surface coverage.In contrast,As(III)forms dominantly bidentate binuclear corner sharing(~2C)sorption complexes on Gt and Lp [d(As-Fe)=3.3-3.4 A],with a minor amount of monodentate mononuclear corner-sharing(~1V)complexes [d(As-Fe)=3.5-3.6 A].Bidentate mononuclear edge-sharing(~2E)complexes are virtually absent in Gt and Lp at the high surface coverages that were investigated in the present study.These results are compared with available literature data and discussed in terms of the reactivity of iron(III)(oxyhydr)oxide surface sites.
机译:利用X射线吸收光谱法(XAS)研究了缺氧条件下As(III)在两线水铁矿(Fh),赤铁矿(Hm),针铁矿(Gt)和纤铁矿(Lp)上的吸附方式。射线吸收近缘结构光谱法(XANES)表示由于Fenton反应而使氧的存在最小化了As(III)的氧化作用。两线水铁矿和赤铁矿与针铁矿和纤铁矿上形成的不同。在高表面覆盖率下,Fh和Hm上的主要复杂类型是二齿单核边角共享(〜2E)和双齿双核角边共享(〜2C), As-Fe距离分别为2.90 + -0.05和3.35 + -0.05 A.在低表面覆盖率下,亚铁酸盐观察到相同的表面配合物。相反,As(III)形成主要的双齿双核角共享(〜2C)吸附具有氨基的Gt和Lp [d(As-Fe)= 3.3-3.4 A]上的络合物r数量的单齿单核角共享(〜1V)复合物[d(As-Fe)= 3.5-3.6 A]。在高表面覆盖率下,Gt和Lp实际上不存在双齿单核角共享(〜2E)复合物将这些结果与现有的文献数据进行比较,并就铁(III)(羟基氧化物)氧化物表面位点的反应性进行了讨论。

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  • 来源
    《Environmental Science & Technology》 |2005年第23期|p.9147-9155|共9页
  • 作者单位

    Institut de Mineralogie et de Physique des Milieux Condenses (IMPMC),UMR 7590,CNRS,Universite Paris 6 & 7,IPGP,140,rue de Lourmel,75015 Paris,France,Surface & Aqueous Geochemistry Group,Department of Geological and Environmental Sciences,Stanford Uni;

    Institut de Mineralogie et de Physique des Milieux Condenses (IMPMC),UMR 7590,CNRS,Universite Paris 6 & 7,IPGP,140,rue de Lourmel,75015 Paris,France,Surface & Aqueous Geochemistry Group,Department of Geological and Environmental Sciences,Stanford Uni;

    Institut de Mineralogie et de Physique des Milieux Condenses (IMPMC),UMR 7590,CNRS,Universite Paris 6 & 7,IPGP,140,rue de Lourmel,75015 Paris,France,Surface & Aqueous Geochemistry Group,Department of Geological and Environmental Sciences,Stanford Uni;

    Institut de Mineralogie et de Physique des Milieux Condenses (IMPMC),UMR 7590,CNRS,Universite Paris 6 & 7,IPGP,140,rue de Lourmel,75015 Paris,France,Surface & Aqueous Geochemistry Group,Department of Geological and Environmental Sciences,Stanford Uni;

    Institut de Mineralogie et de Physique des Milieux Condenses (IMPMC),UMR 7590,CNRS,Universite Paris 6 & 7,IPGP,140,rue de Lourmel,75015 Paris,France,Surface & Aqueous Geochemistry Group,Department of Geological and Environmental Sciences,Stanford Uni;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境化学;
  • 关键词

  • 入库时间 2022-08-17 14:08:10

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