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An insight in the structure of a palygorskite from Palygorskaja: Some questions on the standard model

机译:Palygorskaja对坡缕石结构的见解:关于标准模型的一些问题

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摘要

In this study we analyze in detail a palygorskite from Palygorskaja. This palygorskite is situated in the context of the existing studies using X-ray powder diffraction analysis. Moreover, a novel microdiffraction study on a small bunch of fibers shows highly structured 2D diffraction patterns that allow to decipher some information on the microstructure, thus overcoming the uncertainty usually originated by large samples containing mixtures and impurities. Structural data provided by Chisholm (1992) are used to simulate 1D and 2D powder and fiber diffraction patterns for palygorskite, which are compared with the experimental results. We performed simulations for powder and fiber diffraction and we centered our attention in the region of interest with d-spacings between 4.0 and 4.5 angstrom. This palygorskite is consistent with a purely orthorhombic palygorskite, based on good agreement of data with simulations. The experimental results present some reflections not found in the simulations. These reflections are interpreted as corresponding to other hk1 planes of palygorskite. They do not match any reflection from the monoclinic structural model nor from probable impurities, reinforcing the interpretation of them being intrinsic to the structure of the mineral. Our findings suggest a revisal of the commonly accepted structure of palygorskite. They correspond to hid planes of palygorskite, and they do not match any reflection neither from the monoclinic structural model nor from possible impurities, and thus reinforcing the idea of them being intrinsic to the structure of the mineral, suggesting the necessity of a revisal of the commonly accepted structure of palygorskite.
机译:在这项研究中,我们详细分析了Palygorskaja的坡缕石。该坡缕石位于使用X射线粉末衍射分析的现有研究的范围内。此外,对一小束纤维进行的新型微衍射研究显示了高度结构化的2D衍射图样,该图可以解密一些微结构信息,从而克服了通常由包含混合物和杂质的大样品引起的不确定性。 Chisholm(1992)提供的结构数据用于模拟坡缕石的1D和2D粉末和纤维衍射图,并与实验结果进行比较。我们进行了粉末和纤维衍射的模拟,并将注意力集中在d间距在4.0至4.5埃之间的关注区域。基于数据与模拟的良好一致性,该坡缕石与纯斜方坡缕石一致。实验结果提出了一些在仿真中未发现的思考。这些反射被解释为与坡缕石的其他hk1平面相对应。它们与单斜晶结构模型或可能的杂质都没有任何反射,从而增强了对它们是矿物结构固有的解释。我们的发现表明对坡缕石的公认结构进行了修订。它们对应于坡缕石的隐蔽平面,并且既不与单斜晶结构模型也不可能与可能的杂质反射不匹配,因此加强了它们是矿物结构所固有的思想,表明有必要对矿物进行修订。坡缕石的公认结构。

著录项

  • 来源
    《Applied clay science》 |2017年第11期|39-47|共9页
  • 作者单位

    Univ Salamanca, Dept Geol, Plaza Merced S-N, E-37008 Salamanca, Spain|Univ Complutense Madrid, CSIC, Inst Geociencias IGEO, Avd Jose Antonio Novais S-N, E-28040 Madrid, Spain;

    ESRF, European Synchrotron, 71 Ave Martyrs, F-38000 Grenoble, France;

    Univ Complutense Madrid, CSIC, Inst Geociencias IGEO, Avd Jose Antonio Novais S-N, E-28040 Madrid, Spain|Univ Complutense Madrid, Dept Crystallog & Mineral, Avd Jose Antonio Novais S-N, Madrid 28040, Spain;

    Univ Salamanca, Dept Geol, Plaza Merced S-N, E-37008 Salamanca, Spain;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Palygorskite; Palygorskaja; X-ray diffraction; Powder diffraction; Fiber diffraction;

    机译:坡缕石;Palygorskaja;X射线衍射;粉末衍射;纤维衍射;

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