首页> 外文期刊>American Mineralogist >Evolution of local electronic structure in alabandite and niningerite solid solutions [(Mn,Fe)S, (Mg,Mn)S, (Mg,Fe)S] using sulfur K- and L-edge XANES spectroscopy
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Evolution of local electronic structure in alabandite and niningerite solid solutions [(Mn,Fe)S, (Mg,Mn)S, (Mg,Fe)S] using sulfur K- and L-edge XANES spectroscopy

机译:用硫K边和X边XANES光谱分析石和镍矿固溶体[(Mn,Fe)S,(Mg,Mn)S,(Mg,Fe)S]中局部电子结构的演变

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摘要

Synchrotron radiation S K- and L-edge X-ray absorption near-edge structure (XANES) spectra are reported for the cubic, rocksalt (B1) structure sulfides niningerite (MgS), alabandite (MnS), and oldhamite (CaS), and for their solid solutions (Mn,Fe)S and (Mg,Mn)S, and S L-edge XANES spectra are reported also for (Mg,Fe)S solid solutions. Pre-edge features at the S K-edge are attributed to transition of S 1s electrons to the lowest available unoccupied S 3p * antibonding states hybridized with metal 3d(eg) states, and at the S L-edge to transition of S 2p electrons to unoccupied S 3s *, 4s *, and 3d antibonding states hybridized with metal 3d(eg) states, and to a lesser extent 3d(t2g) states.
机译:报告了立方,岩盐 (B1)结构硫化物镍矿(MgS)的同步辐射S K和L边缘X射线吸收近边缘 结构(XANES)光谱),石(MnS), 和硫铁矿(CaS)以及它们的固溶体(Mn,Fe)S 和(Mg,Mn)S和S L-还报告了 (Mg,Fe)S固溶体的XANES边缘光谱。 S K-edge 处的前边缘特征归因于S 1s电子跃迁到最低的 可用空位S 3p *与 金属3d(e g )状态,并且在S L边缘处,S 2p电子跃迁为未占据的S 3s *,4s *和3d反键 状态与金属3d(e g )状态混合,并与较小的 范围3d(t 2g )状态混合。 sup>

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  • 来源
    《American Mineralogist》 |2002年第10期|1321-1332|共12页
  • 作者单位

    Department of Earth Sciences,University of Western Ontario,London, Ontario N6A 5B7, Canada;

    Department of Earth Sciences,University of Western Ontario,London, Ontario N6A 5B7, Canada;

    Faculty of Physics, Rostov State University,344090, Rostov-on-Don, Russia;

    Faculty of Physics, Rostov State University,344090, Rostov-on-Don, Russia;

    Faculty of Physics, Rostov State University,344090, Rostov-on-Don, Russia;

    Department of Earth Sciences,University of Western Ontario,London, Ontario N6A 5B7, Canada;

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