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Quantitative electron microprobe analysis of Fe3+/{sum}Fe: Basic concepts and experimental protocol for glasses

机译:Fe3 + / {sum} Fe的定量电子微探针分析:玻璃的基本概念和实验方案

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摘要

The presence of an unfilled 3d electron shell in the transition metals of the first series is manifested in X-ray self-absorption effects that cause distortions in the L emission spectra. In particular, one observes peak shape changes and peak position shifts toward lower energies that are attributed to X-ray photon self-absorption in the specimen. Self-absorption corresponds to partial overlap of both L-emission and absorption transitions in the region of the Fermi level. Such an overlap is related to relaxation effects that follow the creation of the core hole in the studied ions. For Fe, the overlap between the FeL emission peak and the corresponding FeLIII absorption band is clearly higher for Fe2+ than for Fe3+, leading to an enhanced self-absorption induced shift of the FeL peak for Fe2+. The shift of the L peak between Fe2+ and Fe3+ can be measured with the electron microprobe and hence exploited to determine the Fe3+/Fe ratios in silicates and glasses. For that purpose, an empirical method has been established based on working curves constructed from reference materials. A complete set of working curves is presented for glasses as well as an original experimental protocol.
机译:在第一个系列的过渡金属中存在未填充的3d电子壳,这在X射线自吸收效应中表现出来,该效应导致L发射光谱畸变。在 中,人们观察到峰形变化和峰位置 向较低能量的移动,这归因于样品中X射线光子 的自吸收。自吸收与 对应于费米能级区域中L发射和吸收跃迁 的部分重叠。这种重叠与被研究离子中形成核孔 之后的弛豫效应有关。对于Fe,Fe 2 + III 吸收带之间的重叠明显 更高。与Fe 3 + 相比,导致Fe 2 + 的FeL峰的自吸收增强。 Fe 2 + 和Fe 3 + 之间的L峰 的位移可以用电子探针 和因此可用于确定硅酸盐 和玻璃中Fe 3 + / Fe的比率。为此,已根据参考材料构建的工作曲线建立了一种经验方法。 给出了 眼镜的完整工作曲线集以及原始的实验方案。

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  • 来源
    《American Mineralogist》 |2004年第4期|00000654-00000662|共9页
  • 作者单位

    Centre de Microanalyse Camparis, Université Paris 6, 4 place jussieu, 75252 Paris cedex 5, France|Laboratoire de Géosciences Marines, UMR 7097-CNRS, Université Paris 6 et 7, Institut de Physique de Globe, 4 place Jussieu, 75252 Paris cedex 5, France;

    Laboratoire de Géosciences Marines, UMR 7097-CNRS, Université Paris 6 et 7, Institut de Physique de Globe, 4 place Jussieu, 75252 Paris cedex 5, France;

    Laboratoire de Pétrologie, Modélisation des Matériaux et Processus, Université Paris 6, 4 place Jussieu, 75252 Paris cedex 5, France;

    IPGP, 4 place Jussieu, 75252 Paris cedex 5, France;

    Laboratoire de Géosciences Marines, UMR 7097-CNRS, Université Paris 6 et 7, Institut de Physique de Globe, 4 place Jussieu, 75252 Paris cedex 5, France;

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