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首页> 外文期刊>American Mineralogist >Nondestructive three-dimensional element-concentration mapping of a Cs-doped partially molten granite by X-ray computed tomography using synchrotron radiation
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Nondestructive three-dimensional element-concentration mapping of a Cs-doped partially molten granite by X-ray computed tomography using synchrotron radiation

机译:使用同步辐射的X射线计算机断层摄影术对掺Cs的部分熔融花岗岩进行无损三维元素浓度映射

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摘要

Nondestructive, three-dimensional (3-D) element-concentration mapping was performed and high spatial resolution and quantitative applicability were demonstrated. X-ray computed tomography using synchrotron radiation developed at SPring-8 (SP-µCT) enabled us to acquire high-resolution tomographic images with X-ray energies just above and below the absorption edge of an element. Concentration of the element could be calculated from the difference of these images with a correction using standard material. A 3-D Cs concentration map of a partially molten granite was obtained by this technique and compared with a 2-D element map produced by an electron-probe X-ray microanalyzer (EPMA), with respect to spatial and compositional resolution. A spatial resolution of about 20 µm was achieved by SP-µCT. The compositional resolution of ±2.5 wt% was achieved using the following two calibration processes of linear attenuation coefficients (LAC): (1) calibration based on the empirical relationship between theoretical LACs and observed CT values, and (2) the calibration of spatial variation of observed mass attenuation coefficients (MAC) due to X-ray energy shift using a standard material (Cs-bearing solution). Using the Cs2O map obtained by SP-µCT, 3-D image analysis was demonstrated, for example, connectivity of melt was calculated and it was found that 88 vol% of melt was connected in three dimensions in the sample. Furthermore, the possibility of 3-D diffusion studies by SP-µCT was discussed based on the spatial and compositional resolutions. This "nondestructive" and "3-D" mapping technique can reveal the internal compositional distribution of precious samples such as extraterrestrial materials and cultural assets, and can solve many 3-D issues such as material transport in geological and industrial materials.
机译:进行了无损三维(3-D)元素浓度映射,证明了较高的空间分辨率和定量的适用性。使用在SPring-8开发的 同步辐射的X射线计算机断层扫描(SP-µCT)使 us能够获取具有X射线的高分辨率断层图像 元素的浓度可以根据这些图像的差异 进行计算,并使用标准材料进行校正。通过此技术获得了部分熔融花岗岩的 3-D Cs浓度图,并与通过 生成的二维元素图进行了比较。电子探针X射线显微分析仪(EPMA),相对于 的空间和组成分辨率。 SP-µCT的空间分辨率 约为20 µm。使用以下两个线性衰减系数 (LAC)校准过程,可实现±2.5 wt%的组成 分辨率:(1)基于校准 理论LAC与观测到的CT值之间的经验关系,以及(2)观测到的质量衰减系数 (MAC)的空间变化的校准 由于使用标准材料(含Cs的 解决方案)的X射线能量转移。使用通过SP-µCT获得的Cs 2 O图,演示了3-D 图像分析,例如,计算了 熔体的连通性并结果发现,在样品中的三个维度中, 的熔体体积百分比为88%。此外,基于空间和组成分辨率,讨论了通过SP-µCT进行3D扩散研究的 可能性。这种“非破坏性” 和“ 3-D”映射技术可以揭示珍贵样品(如地球外物质 和文化资产)的内部成分 分布。并可以解决许多3-D问题,例如地质和工业材料中的材料 运输。

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  • 来源
    《American Mineralogist》 |2004年第9期|00001304-00001313|共10页
  • 作者单位

    Department of Complexity Science and Engineering, Graduate School of Frontier Sciences, The University of Tokyo, Kashiwanoha 5-1-5, Kashiwa, Chiba 277-8561, Japan;

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

    Department of Earth and Space Science, Graduate School of Science, Osaka University, Toyonaka, Osaka 560-0043, Japan;

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

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

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

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

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

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