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Structure of single sheet iron oxides produced from surfactant interlayered green rusts

机译:表面活性剂夹层生锈产生的单片氧化铁的结构

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摘要

Ultrathin iron oxide particles are of high interest due to their large surface areas and unusual physical and chemical properties. Previous works have shown that single sheet.iron oxides (SSI) can be formed via delamination of oxidized layered iron (hydr)oxides (green rusts, GR) interlayered by dodecanoate. However, there is considerable uncertainty on the true structure of both starting material and final products, and the reaction pathway. In this work, we describe a robust method for SSI synthesis and provide detailed structural characterization of the initial, intermediate and final phases to decipher the reaction mechanism. The SSI product has the formula FeO0.82(OH)(1.38)center dot 0.7H(2)O, and consists of platelets with a height of 1 nm and lateral dimensions of 20 to 100 nm as observed by Atomic Force Microscopy and Transmission Electron Microscopy. Mossbauer spectroscopy from 300 to 9 K shows that SSI is distinct from goethite, ferrihydrite and feroxyhite. Pair distribution function (PDF) analysis of high energy X-ray scattering data reveals that SSI has two distinct nearest neighbor Fe-Fe distances in contrast to the single distance in the parent Fe-II-Fe-III (hydr)oxide composed of entirely edgesharing octahedra. Modeling of the SSI PDF data indicates that oxidation of Fe-II to Fe-III of dodecanoate-intercalated green rust results in displacements of Fe atoms perpendicular from the parent iron (hydr)oxide layer, forming a material that consists of iron polyhedra linked by both corner- and edge-sharing. This model which is different from the previously published model, matches the measured SSI thickness and electron diffraction pattern. This elucidated reaction pathway confirms that the dodecanoate interlayers in GR hinders Fe polymerization across interlayers and thus restrict chemical transformations to largely two-dimensional space. The increase of single- and double- coordinated O/OH groups in the SSI compared with the parent GRs is expected to give a high reactivity of SSI as surface complexation sorbents.
机译:超薄氧化铁颗粒由于其较大的表面积和不寻常的物理和化学性质而备受关注。以前的工作表明,单层氧化铁(SSI)可以通过分层分层形成十二烷酸酯的氧化层状氧化铁(氢)氧化物(生铁锈,GR)而形成。但是,起始原料和最终产物的真实结构以及反应途径都存在很大的不确定性。在这项工作中,我们描述了一种SSI合成的可靠方法,并提供了初始,中间和最终阶段的详细结构表征,以破译反应机理。 SSI产品的分子式为FeO0.82(OH)(1.38)中心点0.7H(2)O,由高度为1 nm,横向尺寸为20至100 nm的血小板组成(通过原子力显微镜和透射观察)电子显微镜。从300到9 K的Mossbauer光谱表明,SSI与针铁矿,水铁矿和亚铁矿不同。对高能X射线散射数据的成对分布函数(PDF)分析显示,与完全由母体Fe-II-Fe-III(氢)氧化物组成的单个距离相比,SSI具有两个不同的最接近的Fe-Fe距离边缘共享八面体。 SSI PDF数据的建模表明,十二酸根插入的生铁锈中的Fe-II氧化为Fe-III导致垂直于母体(水合)氧化物层垂直的Fe原子位移,形成了一种由多面体铁连接的材料边角共享。该模型与以前发布的模型不同,它与测得的SSI厚度和电子衍射图相匹配。这种阐明的反应路径证实了GR中的十二烷酸酯中间层阻碍了Fe跨中间层的聚合,从而将化学转化限制在很大程度上是二维空间。与母体GRs相比,SSI中单配位和双配位O / OH基团的增加有望使SSI作为表面络合吸附剂具有较高的反应活性。

著录项

  • 来源
    《Applied clay science》 |2019年第3期|86-96|共11页
  • 作者单位

    Univ Copenhagen, Dept Plant & Environm Sci, Thorvaldsenvej 40, DK-1871 Frederiksberg, Denmark;

    Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark|Univ Copenhagen, Dept Chem, Univ Pk 5, DK-2100 Copenhagen O, Denmark;

    Univ Lorraine, CNRS, LCPME, UMR 7564, Metz, France;

    Univ Lorraine, CNRS, LCPME, UMR 7564, Metz, France;

    Virginia Tech, Dept Geosci, Blacksburg, VA 24061 USA;

    Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark|Univ Copenhagen, Dept Chem, Univ Pk 5, DK-2100 Copenhagen O, Denmark;

    Univ Copenhagen, Dept Plant & Environm Sci, Thorvaldsenvej 40, DK-1871 Frederiksberg, Denmark;

  • 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

    Layered double hydroxides; Two-dimensional material; Delamination; Single sheet iron oxides;

    机译:层状双氢氧化物;二维材料;分层;单片氧化铁;

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