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Chinese Journal of High Pressure Physics  > 2005  >  19(3): 225-229 .
JIANG Xi, ZHOU Wen-Ge, LIU Yong-Gang, XIE Hong-Sen, ZHANG Huan, LIU Jing, MA Mai-Ning, LI Xiao-Dong, LI Yan-Chun. Equation of State of Cassiterite at Room Temperature and up to 13 GPa[J]. Chinese Journal of High Pressure Physics, 2005, 19(3): 225-229 . doi: 10.11858/gywlxb.2005.03.006
Citation: JIANG Xi, ZHOU Wen-Ge, LIU Yong-Gang, XIE Hong-Sen, ZHANG Huan, LIU Jing, MA Mai-Ning, LI Xiao-Dong, LI Yan-Chun. Equation of State of Cassiterite at Room Temperature and up to 13 GPa[J]. Chinese Journal of High Pressure Physics, 2005, 19(3): 225-229 . doi: 10.11858/gywlxb.2005.03.006
shu

Equation of State of Cassiterite at Room Temperature and up to 13 GPa

doi: 10.11858/gywlxb.2005.03.006
  • 1.

    Institute of Geochemistry, Chinese Academy of Science, Guiyang 550002, China;

  • 2.

    Institute of High Energy Physics, Chinese Academy of Science, Beijing 100039, China;

  • 3.

    Graduate School of Chinese Academy of Science, Beijing 100039, China

More Information
  • Corresponding author: JIANG Xi
  • Received Date: 20 Apr 2004
  • Rev Recd Date: 29 Aug 2004
  • Publish Date: 05 Sep 2005
    Abstract
  • At room temperature and up to 13 GPa, in situ energy dispersive X-ray diffraction measurements for a natural cassiterite, collected from Gejiu tin deposits, Yunnan, were performed by using diamond anvil cell instrument with synchrotron radiation at BSRF. The results show that cassiterite is stable up to 13 GPa and its parameters of unit-cell decrease with increasing pressure. On the other hand, the parameters of unit-cell we calculated are bigger than these of former experiments with synthetical cassiterite. According to Birch equation of state, KT(0)＝228 GPa. For natural cassiterite crystal, it is believed that Zr replacing to Sn may be the reason for expansion of unit-cell.

     

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