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Article Abstract
In situ Raman spectra of HoVO micro- and nanocrystals were obtained at high pressures up to 25.4 and 18.0 GPa at room temperature, respectively. The appearance of new peaks in the Raman spectra and the discontinuities of the Raman-mode shift provided powerful evidence for an irreversible zircon-to-scheelite structure transformation for HoVO microcrystals at 7.2 GPa and for HoVO nanocrystals at 8.7 GPa. The lattice contraction caused by the size effect was thought to be responsible for the different phase-transition pressures. Also, the higher stability of HoVO nanocrystals compared with the microcrystals was also confirmed using the Raman frequencies and pressure coefficients. The results of the phase transition of HoVO were compared with previously reported rare-earth orthovanadates, and the phase diagram of REVO with RE ionic radius at different pressures was presented.
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| http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6643725 | PMC |
| http://dx.doi.org/10.1021/acsomega.8b02519 | DOI Listing |
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