TY - JOUR
T1 - X-ray-excited optical luminescence imaging for on-site identification of xenotime
AU - Imashuku, Susumu
AU - Wagatsuma, Kazuaki
N1 - Funding Information:
The present study was supported by Japan Oil, Gas and Metals National Corporation ( JOGMEC ) for Basic Research on Mining & Metallurgical Technology. The authors thank Mr. Issei Narita of Tohoku University for helping us perform the EPMA analysis.
Publisher Copyright:
© 2021 Elsevier B.V.
PY - 2021/6
Y1 - 2021/6
N2 - The on-site identification of rare-earth-element (REE) bearing minerals prior to off-site quantitative analysis helps to efficiently develop mines that reserve REEs. This study examines a method for rapidly identifying xenotime, which is one of the principal REE bearing minerals, leading to such on-site analysis. It is based on acquiring X-ray-excited optical luminescence (XEOL) images of mineral ores that primarily comprise xenotime. Intense green or greenish-yellow luminescence originating from Sm, Eu, Tb, and Dy was detected for xenotime with a uranium content of less than 1.1 wt%, which includes over half of the xenotime in the world. Other minerals emitted no luminescence (e.g., cheralite, chlorite, and potassium feldspar), different colored luminescence from xenotime (e.g., albite and potassium feldspar), or weak green luminescence (e.g., zircon). Therefore, xenotime can in most circumstances be distinguished from other minerals by detecting intense green or greenish-yellow luminescence in XEOL images. The XEOL measurement was performed in air within 60 s for an area with the diameter of 3 mm, and the setup primarily required an X-ray tube of the type used in portable analyzers (e.g., X-ray fluorescence analyzers) and a digital camera. The results suggest that the XEOL imaging method may have potential to be used for the on-site and/or field identification of REE bearing minerals.
AB - The on-site identification of rare-earth-element (REE) bearing minerals prior to off-site quantitative analysis helps to efficiently develop mines that reserve REEs. This study examines a method for rapidly identifying xenotime, which is one of the principal REE bearing minerals, leading to such on-site analysis. It is based on acquiring X-ray-excited optical luminescence (XEOL) images of mineral ores that primarily comprise xenotime. Intense green or greenish-yellow luminescence originating from Sm, Eu, Tb, and Dy was detected for xenotime with a uranium content of less than 1.1 wt%, which includes over half of the xenotime in the world. Other minerals emitted no luminescence (e.g., cheralite, chlorite, and potassium feldspar), different colored luminescence from xenotime (e.g., albite and potassium feldspar), or weak green luminescence (e.g., zircon). Therefore, xenotime can in most circumstances be distinguished from other minerals by detecting intense green or greenish-yellow luminescence in XEOL images. The XEOL measurement was performed in air within 60 s for an area with the diameter of 3 mm, and the setup primarily required an X-ray tube of the type used in portable analyzers (e.g., X-ray fluorescence analyzers) and a digital camera. The results suggest that the XEOL imaging method may have potential to be used for the on-site and/or field identification of REE bearing minerals.
KW - On-site analysis
KW - Rare earth elements
KW - X-ray-excited optical luminescence
KW - Xenotime
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U2 - 10.1016/j.gexplo.2021.106763
DO - 10.1016/j.gexplo.2021.106763
M3 - Article
AN - SCOPUS:85102650079
SN - 0375-6742
VL - 225
JO - Journal of Geochemical Exploration
JF - Journal of Geochemical Exploration
M1 - 106763
ER -