首页> 外文学位 >Comparison of the reactivity of various manganese oxides with trivalent aqueous chromium: Microscopic and spectroscopic observations of dissolution, chromium sorption and chromium and manganese redox interactions.
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Comparison of the reactivity of various manganese oxides with trivalent aqueous chromium: Microscopic and spectroscopic observations of dissolution, chromium sorption and chromium and manganese redox interactions.

机译:各种锰氧化物与三价铬水溶液反应性的比较:溶解,铬吸附以及铬和锰氧化还原相互作用的显微和光谱观察。

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摘要

The complex interaction between CrIIIaq and manganite (γ-MnOOH) was systematically studied at room temperature over a pH range of 3 to 6, and within a concentration range of 10−4 to 10−2 M CrOH2+aq. CrIII-hydroxy hydrate was shown to precipitate on the manganite surface while still undersaturated in bulk solution. Due to direct redox coupling with Mn reduction, Cr oxidation was most rapid in the lower pH range. Neither MnII nor CrVI were ever detected on manganite surfaces, even at the maximum rate of their generation. At the highest pH's of this study, CrIIIaq was effectively removed from solution to form CrIII-hydroxy hydrate on manganite surfaces and in the bulk solution, and manganite dissolution and CrVI aq generation were minimized. This heterogeneity is a direct result of the heterogeneous semiconducting nature of natural manganite crystals, and is also an expression of the proximity effect, whereby redox processes on semiconducting surfaces are not limited to next nearest neighbor sites.; The interaction between CrIIIaq and seven different Mn-oxides (6 monomineralic, 1 synthetic) has been observed in pH 4.4 HNO 3 and pH 4.4 ∼ 10−4 M Cr IIIaq solutions. For each mineral-solution interaction, the aqueous chemical concentrations (e.g. [Mn]aq, [Cr]aq, [CrVIaq]) were measured with time. Our surface sensitive FESEM and AFM observations tend to suggest that Cr-uptake is by isolated site binding, very small (30 nm) surface clusters or monolayer scale films. Cr-uptake was followed by slow Cr-release on several of the solids (particularly the layered solids) after a substantial portion of the total aqueous Cr had been converted to CrVIaq.; The oxidizing ability of the different Mn-oxides for CrIII aq is evaluated with regards to the energy level of the redox couple (i.e. the redox potential) as compared with the Fermi energy level of the Mn-oxide. The Mn-oxides that exhibited the greatest and longest lasting Cr III-oxidizing power were the Mn-oxides containing Mn3+, and in particular those containing Mn3+ and Mn2+. It is believed that the combined presence of a reducible Mn ion (e.g. Mn 3+) and a highly soluble Mn2+ ion facilitates a sustained CrIII-oxidation reaction because fresh surface is exposed during the reaction. (Abstract shortened by UMI.)
机译:在室温,pH范围为3至6,浓度范围为10的条件下,系统地研究了Cr III aq 与锰矿(γ-MnOOH)之间的复杂相互作用。 −4 至10 −2 M CrOH 2 + aq 。结果表明,Cr 羟基水合物沉淀在锰矿表面,但在本体溶液中仍不饱和。由于直接的氧化还原和Mn的还原,Cr的氧化在较低的pH范围内最快。即使在锰矿的最大生成速度下,也没有在锰表面检测到Mn II 和Cr VI 。在这项研究的最高pH值下,有效地从溶液中去除了Cr III aq ,从而在锰矿表面和锰表面形成了Cr III -羟基水合物。体溶液,锰的溶解和Cr VI aq 的生成最小化。这种异质性是天然锰矿晶体的异质半导体性质的直接结果,并且也是邻近效应的一种表达,由此在半导体表面上的氧化还原过程不限于下一个最近的相邻位点。在pH 4.4 HNO 3 和pH下观察到Cr III aq 与七种不同的锰氧化物(6种单矿物,1种合成的)之间的相互作用。 4.4〜10 −4 M Cr III aq 溶液。对于每种矿物质溶液相互作用,其含水化学浓度(例如[Mn] aq ,[Cr] aq ,[Cr VI aq ])随时间测量。我们对表面敏感的FESEM和AFM观察结果倾向于表明,Cr的吸收是通过孤立的位点结合,非常小的(<30 nm)表面簇或单层水垢膜实现的。在大部分总的Cr水溶液已转化为Cr VI aq .;根据氧化还原对的能级(即氧化还原电势),与费米比较,评估了不同的锰氧化物对Cr III aq 的氧化能力。锰氧化物的能级。表现出最大和最长持续Cr III 氧化能力的Mn-氧化物是含有Mn 3 + 的Mn-氧化物,特别是含有Mn 3的Mn-氧化物+ 和Mn 2 + 。据认为,可还原的Mn离子(例如Mn 3 + )和高溶解性的Mn 2 + 离子的共同存在促进了Cr III的持续

著录项

  • 作者

    Weaver, Robert Michael.;

  • 作者单位

    Virginia Polytechnic Institute and State University.;

  • 授予单位 Virginia Polytechnic Institute and State University.;
  • 学科 Geochemistry.; Mineralogy.
  • 学位 Ph.D.
  • 年度 2001
  • 页码 107 p.
  • 总页数 107
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;矿物学;
  • 关键词

  • 入库时间 2022-08-17 11:47:06

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