Pressure-induced softening of shear modes in ZnO

被引:59
作者
Decremps, F [1 ]
Zhang, JZ
Li, BS
Liebermann, RC
机构
[1] SUNY Stony Brook, Inst Mineral Phys, Stony Brook, NY 11794 USA
[2] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
[3] Univ Paris 06, CNRS, UMR 7602, F-75252 Paris 05, France
关键词
D O I
10.1103/PhysRevB.63.224105
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The room-temperature elastic moduli C-1J corresponding to the pure longitudinal and transverse modes in single crystals of the wurtzite phase of ZnO have been determined from ultrasonic wave velocities measurements as a function of pressure up to 10 GPa. All the moduli exhibit a linear dependence on pressure, with positive values for the longitudinal moduli (dC(11)/dP = 5.32 and dC(33)/dP = 3.78) but negative values for the shear moduli (dC(44)/dP = -0.35 and dC(66)/dP = -0.30). All modes exhibit anomalous travel time above P-Tr = 7.5 GPa, indicating the onset of a transition to the rocksalt (B1) phase. Using recent improvements for ultrasonic measurements in multianvil apparatus, this experimental study on the phase-transformation mechanism is extended to simultaneous high pressures and high temperatures. At high temperatures, P-Tr decrease and the pressure derivatives of the elastic shear modes become more negative. Thus, the elastic shear softening observed at room temperature is enhanced at elevated temperatures.
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页数:5
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