TY - JOUR
T1 - Nondestructive three-dimensional element-concentration mapping of a Cs-doped partially molten granite by X-ray computed tomography using synchrotron radiation
AU - Ikeda, Susumu
AU - Nakano, Tsukasa
AU - Tsuchiyama, Akira
AU - Uesugi, Kentaro
AU - Suzuki, Yoshio
AU - Nakamura, Ko Ichi
AU - Nakashima, Yoshito
AU - Yoshida, Hideto
PY - 2004
Y1 - 2004
N2 - 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 omographic 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.
AB - 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 omographic 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.
UR - http://www.scopus.com/inward/record.url?scp=4444368452&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=4444368452&partnerID=8YFLogxK
U2 - 10.2138/am-2004-8-919
DO - 10.2138/am-2004-8-919
M3 - Article
AN - SCOPUS:4444368452
SN - 0003-004X
VL - 89
SP - 1304
EP - 1312
JO - American Mineralogist
JF - American Mineralogist
IS - 8-9
ER -