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Sepiolite-palygorskite: Textural study and genetic considerations

机译:海泡石-坡缕石:质地研究和遗传因素

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摘要

The fibrous morphology, the small particle size, and the presence of tunnels and channels in their structure give sepiolite (Sep) and palygorskite (Pal) a large specific surface area (SSA). The surface properties vary greatly among different Sep or Pal deposits because they are strongly conditioned by their textural and microtextural features (size, morphology, and arrangement of fibres). In this work, a detailed study is presented based on the scanning electron microscopy (SEM), field emission scanning electron microscopy (FEG) and transmission electron microscopy (TEM) observations of the microtextural features of a wide range of deposits of extremely pure Sep and Pal from all over the world. It has been confirmed that although all Sep and Pal have 'the same characteristic' fibrous morphology, the samples from different deposits have their own characteristic signatures that vary greatly from one locality to another, explaining why each deposits has different physical and chemical properties. Sep and Pal can consist of fibres with different sizes, curls, or types of aggregation. Several morphological fibre classifications have been made according to length, the width-length ratio (W/L), or curliness. In addition, local heterogeneities have been found as a consequence of particular genetic conditions. Aside from local heterogeneities, each Sep or Pal deposit has its own characteristic signature. As the minor width of fibres observed depends on the resolution of the study technique, we use three terms: lath (the smallest units that can be observed, the true unit crystal), rod (several laths in a crystallographical arrangement), and bundle (several rods parallel to the c-axis). Laths are approximately 10-30 nm wide and are the primary stable particles of Sep and Pal. Small crystals will not be stable and will have dissolved. After lath formation (nucleation), they should grow by oriented aggregation, forming rods and bundles after which they grow by adding ions to the ends of the fibres.
机译:纤维形态,小粒径以及在其结构中存在隧道和通道,使海泡石(Sep)和坡缕石(Pal)具有较大的比表面积(SSA)。不同的Sep或Pal沉积物的表面性质差异很大,因为它们的构造和微观构造特征(尺寸,形态和纤维排列)受到强烈的调节。在这项工作中,基于扫描电子显微镜(SEM),场发射扫描电子显微镜(FEG)和透射电子显微镜(TEM)观察,对大量极纯净Sep和Pb沉积物的微观结构特征进行了详细研究。来自世界各地的朋友。已经证实,尽管所有Sep和Pal都具有“相同的特征”纤维形态,但来自不同沉积物的样品具有其自身的特征特征,每个地方的特征特征差异很大,这解释了每个沉积物为何具有不同的物理和化学性质。 Sep和Pal可以由具有不同大小,卷曲或聚集类型的纤维组成。根据长度,宽长比(W / L)或卷曲度,已进行了几种形态纤维分类。此外,由于特定的遗传条件,还发现了局部异质性。除了局部异质性之外,每个Sep或Pal矿床都有其自己的特征标记。由于观察到的纤维的细小宽度取决于研究技术的分辨率,因此我们使用三个术语:板条(可以观察到的最小单位,真正的单位晶体),棒(晶体学排列的多个板条)和束(平行于c轴的几根杆)。板条约10-30 nm宽,是Sep和Pal的主要稳定颗粒。小晶体将不稳定并会溶解。板条形成(成核)后,它们应通过定向聚集生长,形成杆和束,然后通过向纤维末端添加离子来生长。

著录项

  • 来源
    《Applied clay science》 |2013年第12期|129-144|共16页
  • 作者

    E. Garia-Romero; M. Suarez;

  • 作者单位

    Departamento de Cristalografia y Mineralogia, Facultad de Geobgia, Universidad Complutense de Madrid, Avd. Jose Antonio Novais s, E-28040 Madrid, Spain ,Instituto de Geociencias (IGEO), Universidad Complutense de Madrid and Consejo Superior de Investigaciones Cientificas, Avd. Jose Antonio Novais s, E-28040 Madrid, Spain;

    Area de Cristalografia y Mineralogia, Departamento de Geobgia, Universidad de Salamanca, Plaza de la Merced s, 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

    Sepiolite; Palygorskite; Texture; Specific surface area; Crystal growth; Oriented aggregation;

    机译:海泡石;坡缕石;质地;比表面积;晶体生长;定向聚集;

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