In-situ high-pressure Raman scattering studies in PbWO4 up to 48 GPa

被引:7
|
作者
Errandonea, D. [1 ]
Lacomba-Perales, R. [1 ]
Mishra, K. K. [2 ]
Polian, A. [3 ,4 ]
机构
[1] Univ Valencia, Dept Fis Aplicada, Inst Univ Ciencia Dels Mat, C Doctor Moliner 50, E-46100 Valencia, Spain
[2] Indira Gandhi Ctr Atom Res, Condensed Matter Phys Div, Kalpakkam 603102, Tamil Nadu, India
[3] Univ Paris 06, Sorbonne Univ, IMPMC, 4 Pl Jussieu, F-75005 Paris, France
[4] CNRS, UMR 7590, F-75005 Paris, France
关键词
Raman spectroscopy; High pressure; Phase transitions; LEAD TUNGSTATE; X-RAY; POWDER DIFFRACTION; CAWO4; AMORPHIZATION; SPECTRA; RASPITE;
D O I
10.1016/j.jallcom.2016.01.082
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The effect of pressure on the Raman spectrum of PbWO4 has been investigated up to 48 GPa in a diamond-anvil cell using neon as pressure-transmitting medium. Changes are detected in the Raman spectrum at 6.8 GPa as a consequence of a structural phase transition from the tetragonal scheelite structure to the monoclinic PbWO4-III structure. Additional changes are detected in the Raman spectra at 15.5 and 21.2 GPa. They are proposed to be the consequence of two additional phase transitions to the previously unknown crystalline phases IV and V. Additionally, at 47.7 GPa all Raman modes disappear, which could be caused by a pressure-induced amorphization. All structural changes are reversible, being the scheelite phase recovered at ambient pressure. However, the two most intense modes of the PbWO4-III phase are still present after full decompression, indicating that this phase coexists as a minority metastable phase with the scheelite phase after pressure release. The wavenumber of the Raman modes and their pressure dependencies are reported for the four crystalline phases. The present reported results are compared with previous studies. (c) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:36 / 43
页数:8
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