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Three-dimensional study by synchrotron radiation computed tomography of melt distribution in samples doped to enhance contrast

机译:通过同步辐射的三维研究在掺杂的样品中的熔体分布计算断层扫描,以增强对比度

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摘要

The three-dimensional distribution of melt in partially molten synthetic samples compositionally corresponding to diopside (90 wt.%)-anorthite (10 wt.%) and doped with PbO, WO3, MoO3, or Cs2O to enhance contrast was studied by X-ray computed tomography (CT) with synchrotron radiation. The heavy elements were strongly concentrated in the melt and contributed to an increase of the X-ray linear attenuation coefficient (LAC) of it. PbO was found to be compatible with silicate melt (>20 wt.% in solution) and incompatible with diopside crystals. Other oxides WO3 (~10 wt.%), MoO3 (~5 wt.%) and Cs2O (< 5 wt.%) are also soluble only in the melt. Such doping is useful not only for LAC control in X-ray CT measurements, but also for systematic control of the structure (wetting properties, distribution and connectivity) of partial melt. This technique gives basic information for discussion of the 3D distribution of partial melt having different wetting properties. As PbO was most effective in visualization of the diopside- anorthite partially molten system, CT images of the PbO-bearing sample were used for further 3D investigation of distribution. A distribution of dihedral angles at solid-melt-solid triple junctions ranging from 22 to 55° was observed with the 3D data. This range in angle distribution was probably caused by anisotropy of crystals and the result supports the argument that there is some limitation in a theoretical framework of stereology which estimates the 3D structure based on 2D observations. Investigators have begun to apply X-ray CT to the study of the 3D distribution of partial melts in rocks using synchrotron radiation. Our study on the effect of doping is one approach for developing a technique to investigate 3D melt distribution.
机译:通过X射线研究了与偶氮合成样品(90重量%) - 钙质(10重量%)和掺杂有PBO,WO3,MOO 3或CS2O以增强对比度的部分熔融合成样品的三维分布。计算机断层扫描(CT)具有同步辐射。重量的元素在熔体中强烈浓缩,有助于其X射线线性衰减系数(LAC)的增加。发现PBO与硅酸盐熔体(> 20重量%)与溶液中的硅酸盐(> 20重量%)相容,与硫代旁晶体不相容。其他氧化物WO3(〜10重量%),MOO3(〜5重量%)和CS2O(<5重量%)也仅可溶于熔体中。这种掺杂不仅是用于X射线CT测量中的LAC控制,而且用于系统控制部分熔体的结构(润湿性,分布和连接)。该技术提供了用于讨论具有不同润湿性质的部分熔体的3D分布的基本信息。由于PBO最有效地在偶极旁边熔化系统的可视化中,PBO轴承样品的CT图像用于进一步的分布3D调查。用3D数据观察到范围为22至55°的固式熔体固体三相角的二偏角角的分布。角度分布的该范围可能是由晶体的各向异性引起的,结果支持了基于2D观察估计3D结构的立体内容的理论框架存在一些限制的论点。研究人员已经开始将X射线CT应用于使用同步辐射的岩石中部分熔体的3D分布的研究。我们对掺杂效果的研究是开发一种研究3D熔体分布的技术的一种方法。

著录项

  • 来源
    《Mineralogical Magazine》 |2017年第5期|共20页
  • 作者单位

    1WPI-Advanced Institute for Materials Research (WPI-AIMR) Tohoku University Sendai980-8577 Japan;

    3Geological Survey of Japan National Institute of Advanced Industrial Science and Technology (AIST) Tsukuba Ibaraki305-8567 Japan;

    4Division of Earth and Planetary Sciences Graduate School of Science Kyoto University Kitashirakawa Oiwakecho Kyoto606–8502 Japan;

    5Japan Synchrotron Radiation Research Institute (JASRI/SPring-8) Mikazuki Hyogo 679-5198 Japan;

    3Geological Survey of Japan National Institute of Advanced Industrial Science and Technology (AIST) Tsukuba Ibaraki305-8567 Japan;

    6Geological Survey of Japan National Institute of Advanced Industrial Science and Technology (AIST) Tsukuba Ibaraki 305-8567 Japan;

    7Department of Earth and Planetary Science Graduate School of Science The University of Tokyo Bunkyo-ku Tokyo 113-0033 Japan;

    5Japan Synchrotron Radiation Research Institute (JASRI/SPring-8) Mikazuki Hyogo 679-5198 Japan;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

    partial melting; X-ray computed tomography; synchrotron radiation; doping; contrast enhancement; 3D observations; dihedral angles;

    机译:部分熔化;X射线计算断层扫描;同步辐射;掺杂;对比度增强;3D观察;二对面角;

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