节点文献
Pressure-induced phase transition of wulfenite
【摘要】 The in-situ high-pressure structures of wulfenite have been investigated by means of angular dis-persive X-ray diffraction with diamond anvil cell and synchrotron radiation.In the pressure up to 22.9 GPa, a pressure-induced scheelite-to-fergusonite transition is observed at about 10.6 GPa.The pressure dependence for the lattice parameters of wulfenite is reported, and the axial compression coefficients Ka0 =-1.36×10-3 GPa-1 and Kc0 =-2.78×10-3 GPa-1 are given.The room-temperature isothermal bulk modulus is also obtained by fitting the P-V data using the Murnaghan equation of state.
【Abstract】 The in-situ high-pressure structures of wulfenite have been investigated by means of angular dis-persive X-ray diffraction with diamond anvil cell and synchrotron radiation.In the pressure up to 22.9 GPa, a pressure-induced scheelite-to-fergusonite transition is observed at about 10.6 GPa.The pressure dependence for the lattice parameters of wulfenite is reported, and the axial compression coefficients Ka0 =-1.36×10-3 GPa-1 and Kc0 =-2.78×10-3 GPa-1 are given.The room-temperature isothermal bulk modulus is also obtained by fitting the P-V data using the Murnaghan equation of state.
【Key words】 wulfenite; high-pressure; phase transition; synchrotron radiation; X-ray diffraction;
- 【文献出处】 中国物理C ,Chinese Physics C , 编辑部邮箱 ,2009年11期
- 【分类号】P618.42
- 【被引频次】1
- 【下载频次】43