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The formation and fate of intermediates during the oxidation of pyrite.

机译:黄铁矿氧化过程中中间体的形成和结局。

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摘要

The goal of this study is to enhance the understanding of the mechanism, or mechanisms, involved in the oxidation of pyrite and to characterize the species that influence those mechanisms at the molecular scale. To develop this enhanced understanding, the formation and fate of intermediate species during the oxidation of pyrite have been investigated using a variety of geochemical and surface science techniques. The critical issues that have been evaluated throughout the presented study are the effect of reactive intermediate species, the influence of different oxidants, and the result of different photo-environments on the pyrite oxidation system.; Batch aqueous experiments measured micromolar aqueous concentrations of hydrogen peroxide and hydroxyl radical and show hydrogen peroxide concentrations persisting throughout the course of an oxidation experiment. Fourier transform infrared spectroscopy, utilizing a flow-through attenuated total reflectance reaction cell, observed multiple sulfoxyanion species (sulfate and thiosulfate) at the pyrite surface during oxidation, verifying the step-wise oxidation of disulfide.; Two novel experimental techniques were developed for this study and make up a significant component of this report. The first technique is an ultra-high vacuum mass spectrometry method for the analysis of low concentrations of hydrogen peroxide that independently verified the presence of hydrogen peroxide in the pyrite system. The second technique is a modified photochemical flow-through attenuated total reflectance reaction cell that allowed for the characterization of surface sulfoxyanions during pyrite oxidation under illumination showing the effect light has on the surface speciation of sulfoxyanions.; The experimental analysis of reactive intermediates in the pyrite system has revealed a capacity for the pyrite surface to perform and undergo reactions that were previously overlooked and represents an advance in the knowledge of the surface reactivity of pyrite. The spectroscopic characterization of sulfur oxidation products offers insight into the fundamental mechanisms that govern the oxidation of pyrite.; Overall, this study presents an increased understanding of the formation, stability, and fate of intermediate species in the pyrite system. From this, it is now conceivable to explore the implications of this reactivity in both early earth and present-day environments.
机译:这项研究的目的是增进对黄铁矿氧化过程涉及的一种或多种机理的了解,并在分子规模上表征影响这些机理的物种。为了增强这种理解,已使用多种地球化学和表面科学技术研究了黄铁矿氧化过程中中间物种的形成和命运。在整个研究过程中已评估的关键问题是反应性中间物种的影响,不同氧化剂的影响以及不同的光环境对黄铁矿氧化系统的影响。分批的含水实验测量了过氧化氢和羟​​基自由基的微摩尔水溶液浓度,并表明过氧化氢浓度在整个氧化实验过程中持续存在。傅立叶变换红外光谱法,利用流通的衰减全反射反应池,在氧化过程中在黄铁矿表面观察到多种亚砜基阴离子种类(硫酸根和硫代硫酸根),验证了二硫化物的逐步氧化。为这项研究开发了两种新颖的实验技术,它们构成了本报告的重要组成部分。第一项技术是用于分析低浓度过氧化氢的超高真空质谱法,该方法独立地验证了黄铁矿系统中过氧化氢的存在。第二种技术是改进的光化学流通衰减全反射反应池,该池可在光照下黄铁矿氧化过程中表征表面亚砜基,表明光对亚砜基的表面形态有影响。黄铁矿体系中反应性中间体的实验分析表明,黄铁矿表面具有执行和进行先前被忽略的反应的能力,代表着对黄铁矿表面反应性的认识的进步。硫氧化产物的光谱表征提供了对控制黄铁矿氧化的基本机理的认识。总体而言,这项研究对黄铁矿系统中中间物种的形成,稳定性和命运有了更深入的了解。由此,现在可以想象在地球早期和当今环境中这种反应的意义。

著录项

  • 作者

    Borda, Michael James.;

  • 作者单位

    State University of New York at Stony Brook.;

  • 授予单位 State University of New York at Stony Brook.;
  • 学科 Geochemistry.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 117 p.
  • 总页数 117
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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