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Role of Organic Acids in Promoting Colloidal Transport of Mercury from Mine Tailings

机译:有机酸在促进尾矿中汞胶体运输中的作用

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摘要

A number of factors affect the transport of dissolved and paniculate mercury (Hg) from inoperative Hg mines,including the presence of organic acids in the rooting zone of vegetated mine waste.We examined the role of the two most common organic acids in soils (oxalic and citric acid) on Hg transport from such waste by pumping a mixed organic acid solution (pH 5.7) at 1 mL/min through Hg mine tailings columns.For the two total organic acid concentrations investigated (20 muM and 1 mM),particle-associated Hg was mobilized,with the onset of paniculate Hg transport occurring later for the lower organic acid concentration.Chemical analyses of column effluent indicate that 98 wt % of Hg mobilized from the column was paniculate.Hg speciation was determined using extended X-ray absorption fine structure spectroscopy and transmission electron microscopy,showing that HgS minerals are dominant in the mobilized particles.Hg adsorbed to colloids is another likely mode of transport due to the abundance of Fe-(oxyhydr)oxides,Fe-sulfides,alunite,and jarosite in the tailings to which Hg(ll) adsorbs.Organic acids produced by plants are likely to enhance the transport of colloid-associated Hg from vegetated Hg mine tailings by dissolving cements to enable colloid release.
机译:有许多因素影响着不运转的汞矿的溶解和颗粒状汞(Hg)的运输,包括植被矿山废料生根区中存在有机酸。我们研究了土壤中两种最常见的有机酸(草酸)的作用通过将混合有机酸溶液(pH 5.7)以1 mL / min的速度通过Hg矿尾矿柱泵送来从此类废物中迁移Hg和柠檬酸。对于所研究的两个总有机酸浓度(20μM和1 mM),颗粒-降低了有机酸的浓度,使相关的汞被迁移,随后发生了颗粒状的汞迁移。色谱柱流出物的化学分析表明,从色谱柱中迁移出的汞98%(重量)是颗粒状的。精细结构光谱学和透射电镜观察表明,HgS矿物在动员的颗粒中占主导地位。由于胶体中的丰度高,吸附到胶体上的Hg是另一种可能的运输方式汞(II)吸附的尾矿中有铁氧化物,铁硫化物,褐铁矿和黄钾铁矾。植物产生的有机酸可能会通过以下方式增强植物性汞矿尾矿中胶体相关汞的运输:溶解水泥以使胶体释放。

著录项

  • 来源
    《Environmental Science & Technology》 |2005年第20期|p.7869-7874|共6页
  • 作者单位

    Surface & Aqueous Geochemistry Group,Department of Geological & Environmental Sciences,Stanford University,Stanford,California 94305-2115,U.S.Geological Survey,345 Middlefield Road,MS 901,Menlo Park,California 94025,and Stanford Synchrotron Radiation;

    Surface & Aqueous Geochemistry Group,Department of Geological & Environmental Sciences,Stanford University,Stanford,California 94305-2115,U.S.Geological Survey,345 Middlefield Road,MS 901,Menlo Park,California 94025,and Stanford Synchrotron Radiation;

    Surface & Aqueous Geochemistry Group,Department of Geological & Environmental Sciences,Stanford University,Stanford,California 94305-2115,U.S.Geological Survey,345 Middlefield Road,MS 901,Menlo Park,California 94025,and Stanford Synchrotron Radiation;

    Surface & Aqueous Geochemistry Group,Department of Geological & Environmental Sciences,Stanford University,Stanford,California 94305-2115,U.S.Geological Survey,345 Middlefield Road,MS 901,Menlo Park,California 94025,and Stanford Synchrotron Radiation;

  • 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

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