Revealing the Pressure-Induced Phase Transformation of Xenotime TbPO4 via In Situ Photoluminescence SpectroscopyClick to copy article linkArticle link copied!
- Jai SharmaJai SharmaDepartment of Metallurgical and Materials Engineering, Colorado School of Mines, Golden, Colorado 80401, United StatesMore by Jai Sharma
- Brandon ReynoldsBrandon ReynoldsDepartment of Chemical and Biological Engineering, Colorado School of Mines, Golden, Colorado 80401, United StatesMore by Brandon Reynolds
- Matthew J. CraneMatthew J. CraneDepartment of Chemical and Biological Engineering, Colorado School of Mines, Golden, Colorado 80401, United StatesMore by Matthew J. Crane
- Corinne E. Packard*Corinne E. Packard*[email protected]Department of Metallurgical and Materials Engineering, Colorado School of Mines, Golden, Colorado 80401, United StatesMore by Corinne E. Packard
Abstract

The pressure-induced phase transformations of certain rare earth (RE) orthophosphates have attracted broad interest from geoscience to structural ceramics. Studying these transformations has required in situ Raman spectroscopy or synchrotron X-ray diffraction (XRD), each of which suffers from poor signal or limited accessibility, respectively. This study exploits the photoluminescence (PL) of Tb3+ ions and the unique sensitivity of PL to the local bonding environment to interrogate the symmetry-reducing xenotime–monazite phase transformation of TbPO4. At pressures consistent with the XRD-based phase transformation onset pressure of 8.7(6) GPa, PL spectra show new peaks emerging as well as trend changes in the centroids and intensity ratios of certain PL bands. Furthermore, PL spectra of recovered samples show transformation is irreversible. Hysteresis in certain PL band intensity ratios also reveals the stress history in TbPO4. This in situ PL approach can be applied to probe pressure-induced transformations and crystal field distortions in other RE-based oxide compounds.
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