Structural and magnetic phase transitions occurring in Pr0.7Sr0.3MnO3 manganite at high pressures

被引:0
|
作者
N. T. Dang
D. P. Kozlenko
S. E. Kichanov
L. S. Dubrovinsky
Z. Jirák
D. M. Levin
E. V. Lukin
B. N. Savenko
机构
[1] Joint Institute for Nuclear Research,Bayerisches Geoinstitut
[2] Tula State University,Institute of Physics
[3] University of Bayreuth,undefined
[4] Academy of Sciences of the Czech Republic,undefined
来源
JETP Letters | 2013年 / 97卷
关键词
Manganite; JETP Letter; Magnetic Phase Transition; Oxygen Octahedra; Applied High Pressure;
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摘要
The crystal and magnetic structures and the vibrational spectra of Pr0.7Sr0.3MnO3 manganite are studied within the pressure range up to 25 GPa by methods of X-ray diffraction and Raman spectroscopy. Neutron diffraction studies have been performed at pressures up to 4.5 GPa. The magnetic phase transition from the ferromagnetic phase (TC = 273 K) to the A-type antiferromagnetic phase (TN = 153 K) is found at P ≈ 2 GPa. This transition is characterized by a broad pressure range corresponding to the phase separation. The Raman spectra of Pr0.7Sr0.3MnO3 measured under high pressures significantly differ from the corresponding spectra of the isostructural doped A1 − xA′xMnO3 manganites, (where A is a rare-earth ion and A′ is an alkaline-earth ion) with the smaller average ionic radius 〈rA〉 of A and A′ cations. Namely, the former spectra do not include clearly pronounced stretching phonon modes. At P ∼ 7 GPa, there appears the structural phase transition from the orthorhombic phase with the Pnma space group to the orthorhombic high-pressure phase with the Imma symmetry. In the vicinity of the phase transition, anomalies in the pressure dependences of the lattice parameters, unit cell volume, and phonon frequencies corresponding to the characteristic lattice vibration modes are observed.
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页码:540 / 545
页数:5
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