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Mechanistic investigations of Se(VI) treatment in anoxic groundwater using granular iron and organic carbon: An EXAFS study

机译:用颗粒铁和有机碳处理缺氧地下水中的Se(VI)的机理研究:EXAFS研究

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摘要

The removal of aqueous Se(VI) from a simulated groundwater by granular iron (GI), organic carbon (OC), and a mixture of these reactive materials (GI-OC) was evaluated in laboratory batch experiments. The experiments were performed under anoxic conditions to simulate subsurface treatment. A total reaction time of 120 h (5 d) was chosen to investigate the rapid changes in speciation occurring over reaction times that are reasonable for permeable reactive barrier (PRB) systems. After 120 h, concentrations of Se decreased by >90% in the Gl system, 15% in the OC system and 35% in the GI-OC mixture. Analysis of the materials after contact with Se using synchrotron-radiation based X-ray absorption spectroscopy (XAS) indicated the presence of Se(IV) and Se(0) on the margins of Gl grains after 6 h with evidence of Se-0 and Se-Se bonding, whereas Se(VI) was not observed. After 72 h, Se(0) was the only form of Se present in the Gl experiments. In the OC batches, the XAS analysis indicated binding consistent with sorption of aqueous Se(VI) onto the OC with only minor reduction to Se(IV) and Se(0) after 120 h. Selenium XAS spectra collected for the GI-OC mixture were consistent with spectra for Se(IV) and Se(0) on both the margins of Gl grains and OC particles, suggesting that the presence of dissolved Fe may have mediated the reduction of sorbed Se(Vl). The results suggest that the application of granular Fe is effective at inducing aqueous Se removal in anoxic conditions through reductive precipitation processes.
机译:在实验室批量实验中,评估了通过颗粒状铁(GI),有机碳(OC)和这些反应性材料的混合物(GI-OC)从模拟地下水中去除Se(VI)水溶液的方法。在缺氧条件下进行实验以模拟地下处理。选择总反应时间为120 h(5 d),以研究在整个反应时间内发生的形态快速变化,这对于渗透性反应性屏障(PRB)系统是合理的。 120小时后,硒的浓度在Gl系统中降低了> 90%,在OC系统中降低了15%,在GI-OC混合物中降低了35%。使用基于同步辐射的X射线吸收光谱法(XAS)对与Se接触后的材料进行分析,结果表明6 h后在Gl晶粒的边缘存在Se(IV)和Se(0),并显示出Se-0和Se-Se键合,而未观察到Se(VI)。 72小时后,Se(0)是Se实验中Se的唯一形式。在OC批次中,XAS分析表明结合与Se(VI)水溶液在OC上的吸附一致,而在120 h后仅少量还原为Se(IV)和Se(0)。 GI-OC混合物收集的硒XAS光谱与Gl颗粒和OC颗粒边缘的Se(IV)和Se(0)光谱一致,表明溶解的Fe的存在可能介导了Se的减少(Vl)。结果表明,粒状铁的应用可有效地通过还原性沉淀过程在缺氧条件下诱导去除水中的硒。

著录项

  • 来源
    《Journal of Hazardous Materials》 |2012年第30期|92-100|共9页
  • 作者单位

    Department of Earth and Environmental Sciences, University of Waterloo. 200 University Ave. W.. Waterloo, ON N2L 3G1, Canada;

    Department of Earth and Environmental Sciences, University of Waterloo. 200 University Ave. W.. Waterloo, ON N2L 3G1, Canada;

    Department of Earth and Environmental Sciences, University of Waterloo. 200 University Ave. W.. Waterloo, ON N2L 3G1, Canada;

    Department of Earth and Environmental Sciences, University of Waterloo. 200 University Ave. W.. Waterloo, ON N2L 3G1, Canada;

  • 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
  • 关键词

    se(VI) reduction; anoxic groundwater; micro XRF mapping; micro XANES/EXAFS;

    机译:se(VI)还原;缺氧地下水微型XRF映射;微型XANES / EXAFS;

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