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Title: Monazite-type SrCr O 4 under compression

Abstract

We report a high-pressure study of monoclinic monazite-type SrCrO4 up to 26 GPa. Therein we combined x-ray diffraction, Raman, and optical-absorption measurements with ab initio calculations, to find a pressure-induced structural phase transition of SrCrO4 near 8-9 GPa. Evidence of a second phase transition was observed at 10-13 GPa. The crystal structures of the high-pressure phases were assigned to the tetragonal scheelite-type and monoclinic AgMnO4-type structures. Both transitions produce drastic changes in the electronic band gap and phonon spectrum of SrCrO4. We determined the pressure evolution of the band gap for the low- and high-pressure phases as well as the frequencies and pressure dependencies of the Raman-active modes. In all three phases most Raman modes harden under compression, however the presence of low-frequency modes which gradually soften is also detected. In monazite-type SrCrO4, the band gap blueshifts under compression, but the transition to the scheelite phase causes an abrupt decrease of the band gap in SrCrO4. Calculations showed good agreement with experiments and were used to better understand the experimental results. From x-ray-diffraction studies and calculations we determined the pressure dependence of the unit-cell parameters of the different phases and their ambient-temperature equations of state. The results are compared withmore » the high-pressure behavior of other monazites, in particular PbCrO4. A comparison of the high-pressure behavior of the electronic properties of SrCrO4 (SrWO4) and PbCrO4 (PbWO4) will also be made. Lastly, the possible occurrence of a third structural phase transition is discussed.« less

Authors:
 [1];  [2];  [2];  [2];  [3];  [3];  [4];  [5];  [6];  [6];  [7];  [8]
  1. Univ. de Valencia, Valencia (Spain); Imperial College London, London (United Kingdom)
  2. Univ. de Valencia, Valencia (Spain)
  3. Univ. of Salford, Manchester (United Kingdom)
  4. Florida Intl Univ., Miami, FL (United States)
  5. Univ. of Nevada, Las Vegas, NV (United States)
  6. Univ. de La Laguna, Tenerife (Spain)
  7. Univ. of Campeche, Campeche (Mexico)
  8. Univ. of Verona and INSTM, Verona (Italy)
Publication Date:
Research Org.:
Univ. of Nevada, Las Vegas, NV (United States)
Sponsoring Org.:
USDOE National Nuclear Security Administration (NNSA), Office of Defense Programs (DP)
OSTI Identifier:
1332350
Grant/Contract Number:  
NA0001982
Resource Type:
Accepted Manuscript
Journal Name:
Physical Review B
Additional Journal Information:
Journal Volume: 94; Journal Issue: 13; Journal ID: ISSN 2469-9950
Publisher:
American Physical Society (APS)
Country of Publication:
United States
Language:
English
Subject:
36 MATERIALS SCIENCE; 75 CONDENSED MATTER PHYSICS, SUPERCONDUCTIVITY AND SUPERFLUIDITY; high pressure; X-ray diffraction; phase transition

Citation Formats

Gleissner, J., Errandonea, Daniel, Segura, A., Pellicer-Porres, J., Hakeem, M. A., Proctor, J. E., Raju, S. V., Kumar, R. S., Rodríguez-Hernández, P., Munoz, A., Lopez-Moreno, S., and Bettinelli, M. Monazite-type SrCrO4 under compression. United States: N. p., 2016. Web. doi:10.1103/PhysRevB.94.134108.
Gleissner, J., Errandonea, Daniel, Segura, A., Pellicer-Porres, J., Hakeem, M. A., Proctor, J. E., Raju, S. V., Kumar, R. S., Rodríguez-Hernández, P., Munoz, A., Lopez-Moreno, S., & Bettinelli, M. Monazite-type SrCrO4 under compression. United States. https://doi.org/10.1103/PhysRevB.94.134108
Gleissner, J., Errandonea, Daniel, Segura, A., Pellicer-Porres, J., Hakeem, M. A., Proctor, J. E., Raju, S. V., Kumar, R. S., Rodríguez-Hernández, P., Munoz, A., Lopez-Moreno, S., and Bettinelli, M. Thu . "Monazite-type SrCrO4 under compression". United States. https://doi.org/10.1103/PhysRevB.94.134108. https://www.osti.gov/servlets/purl/1332350.
@article{osti_1332350,
title = {Monazite-type SrCrO4 under compression},
author = {Gleissner, J. and Errandonea, Daniel and Segura, A. and Pellicer-Porres, J. and Hakeem, M. A. and Proctor, J. E. and Raju, S. V. and Kumar, R. S. and Rodríguez-Hernández, P. and Munoz, A. and Lopez-Moreno, S. and Bettinelli, M.},
abstractNote = {We report a high-pressure study of monoclinic monazite-type SrCrO4 up to 26 GPa. Therein we combined x-ray diffraction, Raman, and optical-absorption measurements with ab initio calculations, to find a pressure-induced structural phase transition of SrCrO4 near 8-9 GPa. Evidence of a second phase transition was observed at 10-13 GPa. The crystal structures of the high-pressure phases were assigned to the tetragonal scheelite-type and monoclinic AgMnO4-type structures. Both transitions produce drastic changes in the electronic band gap and phonon spectrum of SrCrO4. We determined the pressure evolution of the band gap for the low- and high-pressure phases as well as the frequencies and pressure dependencies of the Raman-active modes. In all three phases most Raman modes harden under compression, however the presence of low-frequency modes which gradually soften is also detected. In monazite-type SrCrO4, the band gap blueshifts under compression, but the transition to the scheelite phase causes an abrupt decrease of the band gap in SrCrO4. Calculations showed good agreement with experiments and were used to better understand the experimental results. From x-ray-diffraction studies and calculations we determined the pressure dependence of the unit-cell parameters of the different phases and their ambient-temperature equations of state. The results are compared with the high-pressure behavior of other monazites, in particular PbCrO4. A comparison of the high-pressure behavior of the electronic properties of SrCrO4 (SrWO4) and PbCrO4 (PbWO4) will also be made. Lastly, the possible occurrence of a third structural phase transition is discussed.},
doi = {10.1103/PhysRevB.94.134108},
journal = {Physical Review B},
number = 13,
volume = 94,
place = {United States},
year = {Thu Oct 20 00:00:00 EDT 2016},
month = {Thu Oct 20 00:00:00 EDT 2016}
}

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Cited by: 28 works
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Figures / Tables:

Table I Table I: Structural parameters of the monazite structure (P21/n) at ambient pressure.

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