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Title: High-pressure powder x-ray diffraction study of EuVO{sub 4}

Abstract

The high-pressure structural behavior of europium orthovanadate has been studied using in-situ, synchrotron based, high-pressure x-ray powder diffraction technique. Angle-dispersive x-ray diffraction measurements were carried out at room temperature up to 34.7 GPa using a diamond-anvil cell, extending the pressure range reported in previous experiments. We confirmed the occurrence of zircon–scheelite phase transition at 6.8 GPa and the coexistence of low- and high-pressure phases up to 10.1 GPa. In addition, clear evidence of a scheelite–fregusonite transition is found at 23.4 GPa. The fergusonite structure remains stable up to 34.7 GPa, the highest pressure reached in the present measurements. A partial decomposition of EuVO{sub 4} was also observed from 8.1 to 12.8 GPa; however, this fact did not preclude the identification of the different crystal structures of EuVO{sub 4}. The crystal structures of the different phases have been Rietveld refined and their equations of state (EOS) have been determined. The results are compared with the previous experimental data and theoretical calculations. - Graphical abstract: The high-pressure structural sequence of EuVO{sub 4}. - Highlights: • EuVO{sub 4} is studied under pressure up to 35 GPa using synchrotron XRD. • The zircón–scheelite–fergusonite structural sequence is observed. • Crystal structures are refined and equationsmore » of state determined.« less

Authors:
 [1];  [2]
  1. High Pressure and Synchrotron Radiation Physics Division, Bhabha Atomic Research Centre, Mumbai 400085, Maharashtra (India)
  2. Departamento de Física Aplicada—ICMUV, MALTA Consolider Team, Universidad de Valencia, Edificio de Investigación, C/Dr. Moliner 50, Burjassot, 46100 Valencia (Spain)
Publication Date:
OSTI Identifier:
22475648
Resource Type:
Journal Article
Resource Relation:
Journal Name: Journal of Solid State Chemistry; Journal Volume: 226; Other Information: Copyright (c) 2015 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.; Country of input: International Atomic Energy Agency (IAEA)
Country of Publication:
United States
Language:
English
Subject:
37 INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY; COMPARATIVE EVALUATIONS; CRYSTAL STRUCTURE; DECOMPOSITION; DIAMONDS; EQUATIONS OF STATE; EUROPIUM COMPOUNDS; PHASE TRANSFORMATIONS; POWDERS; PRESSURE DEPENDENCE; PRESSURE RANGE GIGA PA; TEMPERATURE RANGE 0273-0400 K; VANADATES; X-RAY DIFFRACTION; ZIRCON

Citation Formats

Garg, Alka B., and Errandonea, D., E-mail: daniel.errandonea@uv.es. High-pressure powder x-ray diffraction study of EuVO{sub 4}. United States: N. p., 2015. Web. doi:10.1016/J.JSSC.2015.02.003.
Garg, Alka B., & Errandonea, D., E-mail: daniel.errandonea@uv.es. High-pressure powder x-ray diffraction study of EuVO{sub 4}. United States. doi:10.1016/J.JSSC.2015.02.003.
Garg, Alka B., and Errandonea, D., E-mail: daniel.errandonea@uv.es. Sun . "High-pressure powder x-ray diffraction study of EuVO{sub 4}". United States. doi:10.1016/J.JSSC.2015.02.003.
@article{osti_22475648,
title = {High-pressure powder x-ray diffraction study of EuVO{sub 4}},
author = {Garg, Alka B. and Errandonea, D., E-mail: daniel.errandonea@uv.es},
abstractNote = {The high-pressure structural behavior of europium orthovanadate has been studied using in-situ, synchrotron based, high-pressure x-ray powder diffraction technique. Angle-dispersive x-ray diffraction measurements were carried out at room temperature up to 34.7 GPa using a diamond-anvil cell, extending the pressure range reported in previous experiments. We confirmed the occurrence of zircon–scheelite phase transition at 6.8 GPa and the coexistence of low- and high-pressure phases up to 10.1 GPa. In addition, clear evidence of a scheelite–fregusonite transition is found at 23.4 GPa. The fergusonite structure remains stable up to 34.7 GPa, the highest pressure reached in the present measurements. A partial decomposition of EuVO{sub 4} was also observed from 8.1 to 12.8 GPa; however, this fact did not preclude the identification of the different crystal structures of EuVO{sub 4}. The crystal structures of the different phases have been Rietveld refined and their equations of state (EOS) have been determined. The results are compared with the previous experimental data and theoretical calculations. - Graphical abstract: The high-pressure structural sequence of EuVO{sub 4}. - Highlights: • EuVO{sub 4} is studied under pressure up to 35 GPa using synchrotron XRD. • The zircón–scheelite–fergusonite structural sequence is observed. • Crystal structures are refined and equations of state determined.},
doi = {10.1016/J.JSSC.2015.02.003},
journal = {Journal of Solid State Chemistry},
number = ,
volume = 226,
place = {United States},
year = {Sun Mar 15 00:00:00 EDT 2015},
month = {Sun Mar 15 00:00:00 EDT 2015}
}