Home Nondestructive three-dimensional element-concentration mapping of a Cs-doped partially molten granite by X-ray computed tomography using synchrotron radiation
Article
Licensed
Unlicensed Requires Authentication

Nondestructive three-dimensional element-concentration mapping of a Cs-doped partially molten granite by X-ray computed tomography using synchrotron radiation

  • Susumu Ikeda EMAIL logo , Tsukasa Nakano , Akira Tsuchiyama , Kentaro Uesugi , Yoshio Suzuki , Ko-Ichi Nakamura , Yoshito Nakashima and Hideto Yoshida
Published/Copyright: March 28, 2015
Become an author with De Gruyter Brill

Abstract

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.

Received: 2003-4-6
Accepted: 2004-4-12
Published Online: 2015-3-28
Published in Print: 2004-8-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Introductory overview: Hydrate knowledge development
  2. Scanning Electron Microscopy investigations of laboratory-grown gas clathrate hydrates formed from melting ice, and comparison to natural hydrates
  3. Dynamics of trimethylene oxide in a structure II clathrate hydrate
  4. The stability of methane hydrates in highly concentrated electrolyte solutions by differential scanning calorimetry and theoretical computation
  5. The effect of elevated methane pressure on methane hydrate dissociation
  6. Methane hydrate formation in partially water-saturated Ottawa sand
  7. Methanol—inhibitor or promoter of the formation of gas hydrates from deuterated ice?
  8. Investigating the performance of clathrate hydrate inhibitors using in situ Raman spectroscopy and differential scanning calorimetry
  9. Physical properties and rock physics models of sediment containing natural and laboratory-formed methane gas hydrate
  10. Experimental studies on the formation of porous gas hydrates
  11. Investigation of jet breakup and droplet size distribution of liquid CO2and water systems—implications for CO2hydrate formation for ocean carbon sequestration
  12. Measurement of clathrate hydrate precipitation from CO2solution by a nondestructive method
  13. Influence of water thermal history and overpressure on CO2-hydrate nucleation and morphology
  14. Growth-controlling processes of CO2gas hydrates
  15. Thermodynamic prediction of clathrate hydrate dissociation conditions in mesoporous media
  16. Modeling dynamic marine gas hydrate systems
  17. Late-stage, high-temperature processesing in the Allende meteorite: Record from Ca,Fe-rich silicate rims around dark inclusions
  18. Partitioning of Sr, Ba, Rb, Y, and LREE between alkali feldspar and peraluminous silicic magma
  19. Nondestructive three-dimensional element-concentration mapping of a Cs-doped partially molten granite by X-ray computed tomography using synchrotron radiation
  20. A theoretical study of structural factors correlated with 23Na NMR parameters
  21. Metamorphic formation of Sr-apatite and Sr-bearing monazite in a high-pressure rock from the Bohemian Massif
  22. Ultra-deep origin of garnet peridotite from the North Qaidam ultrahigh-pressure belt, Northern Tibetan Plateau, NW China
  23. Letter. Novel high-pressure behavior in chlorite: A synchrotron XRD study of clinochlore to 27 GPa
  24. Letter. Periodic precipitation pattern formation in hydrothermally treated metamict zircon
  25. A high pressure X-ray diffraction study of aragonite and the post-aragonite phase transition in CaCO3
Downloaded on 21.9.2025 from https://www.degruyterbrill.com/document/doi/10.2138/am-2004-8-919/html
Scroll to top button