Experimental evidence for a high-pressure isostructural phase transition in osmium

被引:132
作者
Occelli, F [1 ]
Farber, DL
Badro, J
Aracne, CM
Teter, DM
Hanfland, M
Canny, B
Couzinet, B
机构
[1] Lawrence Livermore Natl Lab, Div Earth Sci, Livermore, CA 94550 USA
[2] Lawrence Livermore Natl Lab, IGPP, Livermore, CA USA
[3] Inst Phys Globe, Lab Mineral Cristallog, Paris, France
[4] Sandia Natl Labs, Org 9753, Albuquerque, NM USA
[5] Univ Paris 06, Lab Phys Milieux Condenses, F-75252 Paris 05, France
关键词
D O I
10.1103/PhysRevLett.93.095502
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
We have measured the isothermal equation of state (EOS) of osmium to 75 GPa under hydrostatic conditions at room temperature using angle-dispersive x-ray diffraction. A least-squares fit of this data using a third-order Birch-Murnaghan EOS yields an isothermal bulk modulus K-0=411+/-6 GPa, showing osmium is more compressible than diamond. Most importantly, we have documented an anomaly in the compressibility around 25 GPa associated with a discontinuity in the first pressure derivative of the c/a ratio. This discontinuity plausibly arises from the collapse of the small hole-ellipsoid in the Fermi surface near the L point.
引用
收藏
页码:095502 / 1
页数:4
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