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Rates of Cr(VI) Generation from Cr_xFe_(1-x)(OH)_3 Solids upon Reaction with Manganese Oxide

机译:与氧化锰反应后从Cr_xFe_(1-x)(OH)_3固体生成Cr(VI)的速率

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摘要

The reaction of manganese oxides with Cr(III)-bearing solids in soils and sediments can lead to the natural production of Cr(Vl) in groundwater. Building on previous knowledge of MnO_2 as an oxidant for Cr(III)-containing solids, this study systematically evaluated the rates and mechanisms of the oxidation of Cr(III) in iron oxides by δ-MnO_2. The Fe/Cr ratio (x = 0.055-0.23 in Cr_xFe_(1-x)(OH)_3) and pH (5—9) greatly influenced the Cr(VI) production rates by controlling the solubility of Cr(III) in iron oxides. We established a quantitative relationship between Cr(VI) production rates and Cr(III) solubility of Cr_xFe_(1-x)(OH)_3, which can help predict Cr(VI) production rates at different conditions. The adsorption of Cr(VI) and Mn(II) on solids shows a typical pH dependence for anions and cations. A multichamber reactor was used to assess the role of solid—solid contact in Cr_xFe_(1-x)(OH)_3-MnO_2 interactions, which eliminates the contact of the two solids while still allowing aqueous species transport across a permeable membrane. Cr(VI) production rates were much lower in multichamber than in completely mixed batch experiments, indicating that the redox interaction is accelerated by mixing of the solids. Our results suggest that soluble Cr(III) released from Cr_xFe_(1-x)(OH)_3 solids to aqueous solution can migrate to MnO_2 surfaces where it is oxidized.
机译:锰氧化物与土壤和沉积物中含Cr(III)的固体的反应可导致地下水中Cr(Vl)的自然产生。基于先前对MnO_2作为含Cr(III)固体的氧化剂的认识,本研究系统地评估了δ-MnO_2氧化铁中Cr(III)的氧化速率和机理。 Fe / Cr比(Cr_xFe_(1-x)(OH)_3中的x = 0.055-0.23)和pH(5-9)通过控制Cr(III)在铁中的溶解度极大地影响了Cr(VI)的生产率。氧化物。我们建立了Cr(VI)生产率与Cr_xFe_(1-x)(OH)_3的Cr(III)溶解度之间的定量关系,这可以帮助预测不同条件下的Cr(VI)生产率。 Cr(VI)和Mn(II)在固体上的吸附显示出阴离子和阳离子的典型pH依赖性。多室反应器用于评估固-固接触在Cr_xFe_(1-x)(OH)_3-MnO_2相互作用中的作用,这消除了两种固体之间的接触,同时仍允许水性物质通过可渗透膜传输。多腔室中的Cr(VI)生成速率远低于完全混合批处理中的实验速率,这表明通过混合固体可以加速氧化还原相互作用。我们的结果表明,从Cr_xFe_(1-x)(OH)_3固体释放到水溶液中的可溶性Cr(III)可以迁移到MnO_2表面,并在其中被氧化。

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  • 来源
    《Environmental Science & Technology》 |2017年第21期|12416-12423|共8页
  • 作者单位

    Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, Missouri, 63130 United States;

    State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing, P.R. China;

    Department of Earth and Planetary Sciences, Washington University in St. Louis, St. Louis, Missouri, 63130 United States;

    State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, P. R. China;

    Department of Civil and Environmental Engineering, Louisiana State University, Baton Rouge, Louisiana 70803 United States;

    Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, Missouri, 63130 United States;

  • 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
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  • 入库时间 2022-08-17 13:58:01

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