天然黄铜矿原位高温高压X射线衍射研究

范大伟 魏舒怡 刘景 谢鸿森

范大伟, 魏舒怡, 刘景, 谢鸿森. 天然黄铜矿原位高温高压X射线衍射研究[J]. 高压物理学报, 2013, 27(6): 828-832. doi: 10.11858/gywlxb.2013.06.006
引用本文: 范大伟, 魏舒怡, 刘景, 谢鸿森. 天然黄铜矿原位高温高压X射线衍射研究[J]. 高压物理学报, 2013, 27(6): 828-832. doi: 10.11858/gywlxb.2013.06.006
FAN Da-Wei, WEI Shu-Yi, LIU Jing, XIE Hong-Sen. X-Ray Diffraction Investigation of Chalcopyrite under High Pressure and Temperature[J]. Chinese Journal of High Pressure Physics, 2013, 27(6): 828-832. doi: 10.11858/gywlxb.2013.06.006
Citation: FAN Da-Wei, WEI Shu-Yi, LIU Jing, XIE Hong-Sen. X-Ray Diffraction Investigation of Chalcopyrite under High Pressure and Temperature[J]. Chinese Journal of High Pressure Physics, 2013, 27(6): 828-832. doi: 10.11858/gywlxb.2013.06.006

天然黄铜矿原位高温高压X射线衍射研究

doi: 10.11858/gywlxb.2013.06.006
详细信息
    通讯作者:

    范大伟 E-mail:fandawei@vip.gyig.ac.cn

X-Ray Diffraction Investigation of Chalcopyrite under High Pressure and Temperature

  • 摘要: 在金刚石压腔高压装置(DAC)上,采用外加温实验技术和同步辐射角度色散X射线衍射技术,在最高温度628 K和最高压力32.0 GPa条件下,对天然黄铜矿进行了相变及热状态方程研究。实验样品在约6.0 GPa条件下发生了Chalcopyrite-Rocksalt相变。获得了天然黄铜矿的高温高压实验数据,并根据二阶Birch-Murnaghan状态方程,对所获得的实验数据进行了状态方程拟合,首次获得了天然黄铜矿Rocksalt相的体弹模量K0=109(3) GPa,体弹模量的温度导数(dK/dT)p=-0.033(4) GPaK-1和热膨胀系数0=2.0(2)10-5 K-1。

     

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出版历程
  • 收稿日期:  2012-03-17
  • 修回日期:  2012-05-03
  • 发布日期:  2013-12-15

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