DyVO<sub>4</sub>高压拉曼光谱研究

doi:10.13883/j.issn1004-5929.202102006

光散射学报 ›› 2021, Vol. 33 ›› Issue (2) : 149-155. DOI: 10.13883/j.issn1004-5929.202102006

材料中的应用

DyVO₄高压拉曼光谱研究

王宝云^1,2,3, 宋茂双^1,3

作者信息 +

High pressure Raman spectroscopic study of DyVO₄

WANG Baoyun^1,2,3, SONG Maoshuang^1,3

Author information +

History +

摘要

利用金刚石压腔和拉曼光谱研究了DyVO₄的压缩行为。结果表明:DyVO₄在0-35.4 GPa发生了两次相变。第一次相变在7.8±0.5 GPa开始,在13.3 GPa结束,DyVO₄从锆石相不可逆地转变成白钨矿相,这个相变伴随着锆石相拉曼峰的消失和白钨矿相拉曼峰的出现,光谱特征清晰。第二个相变发生在约21.9 GPa, DyVO₄从白钨矿相进一步可逆地转变成褐钇铌矿相。白钨矿相模133 cm^-1 (B_g)频率随压力的演化趋势在相变点发生变化,另外对应VO₄四面体伸缩振动区域的拉曼峰在褐钇铌矿相逐渐展宽。DyVO₄的褐钇铌矿相一直稳定到35.4 GPa,卸压到常压后,DyVO₄是白钨矿相。

Abstract

The compression behaviour of DyVO₄ has been studied using the combined diamond anvil cell and Raman spectra. The results show DyVO₄ experiences two phase transitions at pressure from ambient pressure to 35.4 GPa. The first phase transition takes place at 7.8±0.5 GPa and finishes at 13.3 GPa. DyVO₄ transforms from zircon phase to scheelite phase companied by distinct disappearance and appearance of Raman peaks in zircon phase and scheelite phase. The second phase transition takes place at 21.9 GPa, DyVO₄ transforms from scheelite phase to fergusonite phase. The evolution of 133 cm^-1 (B_g) mode of scheelite phase changes at transition point. The modes corresponding to stretching vibration of VO₄ of fergusonite phase gradually broaden. The fergusonite phase is stable up to 35.4 GPa. DyVO₄ is scheelite phase at ambient condition after decompression.

导出引用

王宝云, 宋茂双. DyVO₄高压拉曼光谱研究. 光散射学报. 2021, 33(2): 149-155 https://doi.org/10.13883/j.issn1004-5929.202102006

WANG Baoyun, SONG Maoshuang. High pressure Raman spectroscopic study of DyVO₄. Chinese Journal of Light Scattering. 2021, 33(2): 149-155 https://doi.org/10.13883/j.issn1004-5929.202102006

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国家自然科学基金项目(41874107、41574079)

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