High-pressure structural stability of multiferroic hexagonal RMnO3 (R = Y, Ho, Lu)

被引:38
|
作者
Gao, P. [1 ]
Chen, Z. [1 ]
Tyson, T. A. [1 ,2 ,3 ]
Wu, T. [1 ]
Ahn, K. H. [1 ,2 ,3 ]
Liu, Z. [4 ]
Tappero, R. [5 ]
Kim, S. B. [2 ,3 ]
Cheong, S-W. [2 ,3 ]
机构
[1] New Jersey Inst Technol, Dept Phys, Newark, NJ 07102 USA
[2] Rutgers State Univ, Rutgers Ctr Emergent Mat, Piscataway, NJ 08854 USA
[3] Rutgers State Univ, Dept Phys & Astron, Piscataway, NJ 08854 USA
[4] Carnegie Inst Sci, Geophys Lab, Washington, DC 20015 USA
[5] Brookhaven Natl Lab, Natl Synchrotron Light Source, Upton, NY 11973 USA
关键词
MAGNETIC-STRUCTURES; YMNO3; MANGANITES; CRYSTAL; LUMNO3; PHASE; TRANSITION; LATTICE; HOMNO3; ORDER;
D O I
10.1103/PhysRevB.83.224113
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Structural changes in RMnO3 (R = Y, Ho, Lu) under high pressure were examined by synchrotron x-ray diffraction methods at room temperature. Compression occurs more readily in the ab plane than along the c axis. With increased pressure, a pressure-induced hexagonal to orthorhombic phase transition was observed starting at similar to 22 GPa for Lu(Y)MnO3. When the pressure is increased to 35 GPa, a small volume fraction of Lu(Y)MnO3 is converted to the orthorhombic phase and the orthorhombic phase is maintained on pressure release. High-pressure infrared absorption spectroscopy and Mn K-edge near-edge x-ray absorption spectroscopy confirm that the hexagonal P6(3)cm structure is stable below similar to 20 GPa and the environment around the Mn ion is not changed. Shifts in the unoccupied p-band density of states with pressure are observed in the Mn K-edge spectra. A schematic pressure-temperature phase diagram is given for the small ion RMnO3 system.
引用
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页数:9
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