Lattice dynamics of YVO4 at high pressures

被引:57
|
作者
Manjon, F. J. [1 ]
Rodriguez-Hernandez, P. [2 ]
Munoz, A. [2 ]
Romero, A. H. [3 ]
Errandonea, D. [4 ]
Syassen, K. [5 ]
机构
[1] Univ Politecn Valencia, Inst Diseno Fabricac & Prod Automatizada, MALTA Consolider Team, Valencia 46022, Spain
[2] Univ La Laguna, MALTA Consolider Team, Dept Fis Fundamental 2, Tenerife, Spain
[3] CINVESTAV, Unidad Queretaro, Queretaro 76230, Mexico
[4] Univ Valencia, MALTA Consolider Team, Fdn Gen, E-46100 Valencia, Spain
[5] Max Planck Inst Festkorperforsch, D-70569 Stuttgart, Germany
关键词
INDUCED PHASE-TRANSITIONS; SCHEELITE STRUCTURE; OPTICAL-PROPERTIES; RAMAN-SCATTERING; INDUCED ZIRCON; MECHANISM; EU; CAWO4;
D O I
10.1103/PhysRevB.81.075202
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We report an experimental and theoretical lattice-dynamics study of yttrium orthovanadate (YVO4) up to 33 GPa together with a theoretical study of its structural stability under pressure. Raman-active modes of the zircon phase are observed up to 7.5 GPa, where the onset of an irreversible zircon-to-scheelite phase transition is detected, and Raman-active modes in the scheelite structure are observed up to 20 GPa, where a reversible second-order phase transition occurs. Our ab initio total-energy calculations support that the second-order phase transition in YVO4 is from the scheelite to the monoclinic M-fergusonite structure. The M-fergusonite structure remains up to 33 GPa and on pressure release the sample reverts back to the metastable scheelite phase. Raman-and IR-mode symmetries, frequencies, and pressure coefficients in the zircon, scheelite, and M-fergusonite phases are discussed.
引用
收藏
页数:11
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