Joint experimental and theoretical study of bulk Y2O3 at high pressure

We report a joint experimental and theoretical study of the structural and vibrational properties of C-type bulk Y2O3 under hydrostatic compression. The combination of high-pressure X-ray diffraction and Raman scattering experimental measurements with ab initio theoretical calculations on bulk Y2O3 allows us to confirm the cubic (C -type) - monoclinic (B-type) - trigonal (A-type) phase transition sequence on the upstroke and the trigonal-monoclinic phase transition on the downstroke. This result reconciles with the results already found in related rare-earth sesquioxides of cations with similar ionic radii as Y, such as Ho2O3 and Dy2O3, and ends with the controversy regarding the existence of the intermediate monoclinic phase between the cubic and trigonal phases in pure bulk Y2O3 on the upstroke. As a byproduct, the good agreement between experimental and calculated results allows us to use extensive theoretical data to discuss the structural and vibrational behavior of the three phases of Y2O3 under compression, thus allowing a more detailed understanding of the effect of pressure on rare-earth sesquioxides than previous studies.

Automated summary

In this study, the structural and vibrational properties of C-type Y2O3 under hydrostatic compression were investigated through a combination of high-pressure X-ray diffraction, Raman scattering experimental measurements, and ab initio theoretical calculations. The results confirmed the phase transition sequence of C-type to B-type to A-type on the upstroke and A-type to B-type on the downstroke. This finding is consistent with other rare-earth sesquioxides with similar ionic radii as Y. The good agreement between experimental and calculated results allowed for a more detailed understanding of the effect of pressure on rare-earth sesquioxides.