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TEM studies of augite (100) deformation twinning boundaries, quartz sand coatings, and manganese valence state.

机译:钛铁矿(100)变形孪晶边界,石英砂涂层和锰价态的TEM研究。

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摘要

This thesis mainly addresses characterization of earth and environmental materials using a wide range of electron microscopy methods, among which high-resolution transmission electron microscopy (HRTEM), electron energy-loss spectroscopy (EELS), and EELS-based energy-filtered transmission electron microscopy (EFTEM) are highlighted.;HRTEM and EFTEM reveal that not only atomic structures change but also chemical variations occur at augite (100) deformation twinning boundaries. These results also suggest that other proposed structure models of twin boundaries in complex inorganic solids are oversimplified. Real twin boundaries may be complicated, involving structural and chemical variations compared to those of the host.;Quartz grains are commonly armored with micro-scale thickness coatings in aquifer environment. Rigorous characterization of these coatings using TEM needs a suitable sample preparation protocol. Focused Ion Beam (FIB) technique makes this type of work not only possible, but routine. Mineral phases in the coating, their textural relationship, and the interface structure between quartz and its associated coating is examined in detail.;Determination of Mn valence state ranging from Mn2+ to Mn4+ using Mn L2,3 electron energy-loss near-edge spectra is studied systematically. Different methods, including I(L3 )/I(L2) intensity ratio vs. Mn valence state, Gaussian peak fitting of Mn L3 peak, and multiple linear squares fitting of both Mn L3 and L2 peaks, are tried to get the best result. In addition, oxygen K edges for Mn oxides are discussed in terms of their dependence on crystal structures.
机译:本文主要通过多种电子显微镜方法研究地球和环境材料的特性,其中包括高分辨率透射电子显微镜(HRTEM),电子能量损失谱(EELS)和基于EELS的能量过滤透射电子显微镜(EFTEM)突出显示。HRTEM和EFTEM揭示,不仅原子结构发生变化,而且在闪石(100)变形孪晶边界上也会发生化学变化。这些结果还表明,其他提议的复杂无机固体中双晶界的结构模型被简化了。真正的孪晶边界可能很复杂,与主体相比,结构和化学变化都很大。石英颗粒通常在含水层环境中被微米级厚度的涂层所铠装。使用TEM对这些涂层进行严格的表征需要合适的样品制备方案。聚焦离子束(FIB)技术不仅使这种工作成为可能,而且使例行工作成为可能。详细研究了涂层中的矿物相,它们的织构关系以及石英及其相关涂层之间的界面结构。使用Mn L2,3电子能量损失近边缘光谱测定了Mn价态,范围从Mn2 +到Mn4 +。有系统地研究。尝试使用不同的方法(包括I(L3)/ I(L2)强度比与Mn价态,Mn L3峰的高斯峰拟合以及Mn L3和L2峰的多重线性平方拟合)来获得最佳结果。此外,根据锰氧化物对晶体结构的依赖性来讨论其氧K边缘。

著录项

  • 作者

    Zhang, Shouliang.;

  • 作者单位

    The Johns Hopkins University.;

  • 授予单位 The Johns Hopkins University.;
  • 学科 Geology.;Geochemistry.
  • 学位 Ph.D.
  • 年度 2009
  • 页码 135 p.
  • 总页数 135
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;地质学;
  • 关键词

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