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Adsorption and redox transformation of arsenite (As(III)) and arsenate (As(V)) at water-mineral interfaces.

机译:在水-矿物界面处吸附和氧化还原砷(As(III))和砷酸盐(As(V))。

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摘要

Adsorption and redox transformation are the two main processes controlling the mobility and bioavailability of arsenic in soil and water. In this research both wet chemistry and spectroscopic techniques were applied to study the adsorption and redox transformation of As(III) and As(V) on model minerals as well as in sod and sediment.; The present research is therefore summarized as follows: (1) For the first time, by using FTIR combined with a deuteration method, the singly (A-type), doubly (C-type) and triply (B-type) coordinated OH groups on goethite surfaces have been identified. By using this technique, it is found that major fractions of adsorbed arsenate and arsenite replaced singly coordinated hydroxyls (A-type) and may have formed inner-sphere binuclear complexes on the (110) faces of goethite. (2) Mn and Fe are closely related in chemical properties and often occur together in soils and sediments. Mn can isomorphously substitute Fe in the goethite structure. In this study Mn-substituted goethite was synthesized. The interaction between arsenite As(III) and Mn-substituted goethite was investigated by both wet chemistry and XANES spectroscopy. The results indicated that the oxidation of As(III) could be catalyzed by Mn-substituted goethite. This reaction was more sensitive to temperature than to pH. (3) The aging and chemical extraction experiments indicated that the solvents used did not provide good selectivity for defined “chemical forms” of arsenic in model sod minerals. The results from three typical schemes indicated that even qualitative interpretation of data from these selective sequential extraction methods was difficult. It is suggested that the fractions should be divided according to their affinity to the minerals rather than the “chemical forms”.; The adsorption and redox transformation of arsenic oxyanions on different components of soils and sediments are the major processes for controlling the mobility and bioavailability of arsenic in the terrestrial ecosystem. The results from this study provides important information for understanding these processes and potentially, possible techniques for arsenic contamination control. (Abstract shortened by UMI.)
机译:吸附和氧化还原转化是控制砷在土壤和水中的迁移率和生物利用度的两个主要过程。在这项研究中,采用湿化学和光谱技术研究了As(III)和As(V)在模型矿物以及草皮和沉积物中的吸附和氧化还原转化。因此,本研究总结如下:(1)首次通过FTIR结合氘化方法,单(A型),双(C型)和三(B型)配位OH基团在针铁矿表面上已被发现。通过使用该技术,发现吸附的砷酸盐和亚砷酸盐的主要部分取代了单配位羟基(A型),并且可能在针铁矿的(110)面上形成了内球双核络合物。 (2)锰和铁在化学性质上密切相关,经常一起存在于土壤和沉积物中。 Mn可以在针铁矿结构中同构地替代Fe。在这项研究中,合成了锰取代的针铁矿。通过湿化学和XANES光谱研究了亚砷酸盐As(III)和Mn取代的针铁矿之间的相互作用。结果表明,Mn取代的针铁矿可以催化As(III)的氧化。该反应对温度比对pH更敏感。 (3)老化和化学提取实验表明,所使用的溶剂对模型草皮矿物质中定义的砷的“化学形式”没有很好的选择性。三种典型方案的结果表明,即使对这些选择性顺序提取方法的数据进行定性解释也很困难。建议根据其对矿物质的亲和力而不是“化学形式”来划分馏分。砷氧阴离子在土壤和沉积物不同组分上的吸附和氧化还原转化是控制砷在陆地生态系统中迁移和生物利用度的主要过程。这项研究的结果为了解这些过程以及潜在的砷污染控制技术提供了重要信息。 (摘要由UMI缩短。)

著录项

  • 作者

    Sun, Xiaohua.;

  • 作者单位

    University of California, Berkeley.;

  • 授予单位 University of California, Berkeley.;
  • 学科 Engineering Environmental.; Agriculture Soil Science.; Chemistry Inorganic.
  • 学位 Ph.D.
  • 年度 1998
  • 页码 194 p.
  • 总页数 194
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境污染及其防治;土壤学;无机化学;
  • 关键词

  • 入库时间 2022-08-17 11:48:46

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