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Using iron amendments to reduce mercury methylation in engineered wetland sediments.

机译:使用铁改良剂减少工程湿地沉积物中的汞甲基化。

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摘要

One potential drawback of wetland construction and restoration is the formation of monomethylmercury (MHg).; The research described in this dissertation was designed to test the hypothesis that addition of iron to wetland sediments decreases the extent of net mercury methylation by decreasing the activity of sulfide, and therefore the concentration of neutral, bioavailable mercury-sulfide complexes. This hypothesis was tested with a series of laboratory microcosm experiments.; Batch microcosm experiments employing pure cultures of the sulfate-reducing bacterium Desulfobulbus propionicus (1pr3) (Chapter 2) indicated that net mercury methylation decreased with increasing [Fe(II)]. The decrease in net mercury methylation was not attributable to the effect of iron on sulfate reduction rates. Instead, filterable mercury measurements and chemical equilibrium speciation model results suggest that the lower net MHg production in the high-iron treatments was due to a decrease in sulfide activity and a concomitant decrease in the concentration of dissolved, bioavailable inorganic mercury.; Sediment slurry experiments conducted using sediment and surface water from five estuarine wetlands (Chapter 3) were qualitatively consistent with the results of the pure culture experiments. Addition of 25 to 30 mM (or 0.07 mmol g-1 w.w.) Fe(II) to wetland sediments significantly decreased net mercury methylation relative to unamended controls.; Flow-through microcosm experiments designed to simulate conditions found in freshwater treatment wetlands and tidal salt marshes (Chapter 4) showed that significantly less methylmercury was present in the effluent of the iron-amended treatments, compared with the unamended controls. Significantly lower sulfide concentrations were measured in the effluent of the iron-amended treatments relative to the unamended controls for both the freshwater (after 8 days) and seawater (during the entire experiment) microcosms. (Abstract shortened by UMI.)
机译:湿地建设和恢复的一个潜在弊端是单甲基汞(MHg)的形成。本论文描述的研究旨在验证以下假设:在湿地沉积物中添加铁可通过降低硫化物的活性,从而降低中性的,可生物利用的汞-硫化物复合物的浓度来降低净汞甲基化的程度。该假设通过一系列实验室微观实验进行了检验。使用硫酸盐还原细菌丙酸脱硫球菌(1pr3)的纯培养物进行的批量缩影实验表明,净汞甲基化随[Fe(II)]的增加而降低。净汞甲基化的减少不是由于铁对硫酸盐还原速率的影响。取而代之的是,可过滤的汞测量值和化学平衡形态模型结果表明,高铁处理中较低的净MHg产生是由于硫化物活性降低以及溶解的可生物利用的无机汞浓度随之降低。使用来自五个河口湿地的沉积物和地表水进行的泥浆实验(第3章)在质量上与纯培养实验的结果一致。与未修改的对照相比,向湿地沉积物中添加25至30 mM(或0.07 mmol g-1 w.w.)Fe(II)显着降低了净汞甲基化。设计用来模拟在淡水处理湿地和潮汐盐沼中发现的条件的流通微观实验(第4章)显示,与未经修正的对照相比,经铁修正的处理废水中存在的甲基汞明显更少。相对于未经修正的对照,在淡水(8天后)和海水(整个实验期间)的微观世界中,铁修正处理后的废水中测得的硫化物浓度显着降低。 (摘要由UMI缩短。)

著录项

  • 作者

    Mehrotra, Anna Steding.;

  • 作者单位

    University of California, Berkeley.;

  • 授予单位 University of California, Berkeley.;
  • 学科 Engineering Environmental.; Environmental Sciences.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 209 p.
  • 总页数 209
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境污染及其防治;环境科学基础理论;
  • 关键词

  • 入库时间 2022-08-17 11:45:19

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