4.6 Article

The magnetic P-T phase diagram of langasite Ba3TaFe3Si2O14 at high hydrostatic pressures up to 38 GPa

Journal

APPLIED PHYSICS LETTERS
Volume 103, Issue 16, Pages -

Publisher

AMER INST PHYSICS
DOI: 10.1063/1.4822422

Keywords

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Funding

  1. EFRee, an Energy Frontier Research Center
  2. U.S. Department of Energy, Office of Science
  3. Russian Foundation for Basic Research [13-02-12419-ofi-m, 11-02-12089, 11-02-00291-a, 14-02-01033-a, 14-02-00483-a, 13-02-00358-a]
  4. RAS
  5. Russian Ministry of science and education Program [GK 16.740.11.0740]
  6. Siberian Federal University [F11.VVS]
  7. DOE [DE-FG0202ER45955]
  8. CDAC/NNSA
  9. DOE-NNSA [DENA0001974]
  10. DOE-BES [DE-FG02-99ER45775, DE-AC02-06CH11357]
  11. NSF
  12. Division Of Materials Research
  13. Direct For Mathematical & Physical Scien [1126249] Funding Source: National Science Foundation

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The langasite-type crystals with 3d ions are considered as a class of multiferroics in which ferroelectricity can be induced by the magnetic ordering. In this paper, the high-pressure magnetic states of the langasite-type powdered sample Ba3TaFe3Si2O14 have been investigated in a diamond anvil cell by the nuclear forward scattering of synchrotron radiation technique at different temperatures in hydrostatic conditions. In the pressure range of 0 < P < 19.5 GPa, an increase of the Neel temperature T-N from 27 to 41 K was observed in the antiferromagnetic phase of the material. At pressures similar to 19.5 GPa, a transition to another magnetic phase with huge increase in the Neel temperature to similar to 120 K was found. We attribute this change to the structural transition at similar to 19.5 GPa which is evidenced by a drastic change of Raman spectra at this pressure. A tentative magnetic P-T phase diagram of Ba3TaFe3Si2O14 is proposed. (C) 2013 AIP Publishing LLC.

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