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Phase transition and thermodynamic properties of TiO2 from first-principles calculations
  • ISSN号:1674-1056
  • 期刊名称:Chinese Physics B
  • 时间:0
  • 页码:269-274
  • 语言:英文
  • 分类:O414[理学—理论物理;理学—物理]
  • 作者机构:[1]School of Physical Science and Technology, Sichuan University, Chengdu 610064, China, [2]Laboratory for Shock Wave and Detonation Physics Research, Institute of Fluid Physics, Chinese Academy of Engineering Physics, Mianyang 621900, China, [3]International Centre for Materials Physics, Chinese Academy of Sciences, Shenyang 110016, China
  • 相关基金:Project supported by the National Natural Science Foundation of China (Grant No 10776022).
  • 相关项目:500万大气压范围内金属铁熔化熵的从头计算
中文摘要:

The pressure induced phase transitions of TiO2 from anatase to columbite structure and from rutile to columbite structure and the temperature induced phase transition from anatase to rutile structure and from columbite to rutile structure are investigated by ab initio plane-wave pseudopotential density functional theory method(DFT),together with quasi-harmonic Debye model.It is found that the zero-temperature transition pressures from anatase to columbite and from rutile to columbite are 4.55 GPa and 19.92 GPa,respectively.The zero-pressure transition temperatures from anatase to rutile and from columbite to rutile are 950 K and 1500 K,respectively.Our results are consistent with the available experimental data and other theoretical results.Moreover,the dependence of the normalized primitive cell volume V/V0 on pressure and the dependences of thermal expansion coefficient α on temperature and pressure are also obtained successfully.

英文摘要:

The pressure induced phase transitions of TiO2 from anatase to columbite structure and from rutile to columbite structure and the temperature induced phase transition from anatase to rutile structure and from columbite to rutile structure are investigated by ab initio plane-wave pseudopotential density functional theory method (DFT), together with quasi-harmonic Debye model. It is found that the zero-temperature transition pressures from anatase to columbite and from rutile to columbite are 4.55 GPa and 19.92 GPa, respectively. The zero-pressure transition temperatures from anatase to rutile and from columbite to rutile are 950 K and 1500 K, respectively. Our results are consistent with the available experimental data and other theoretical results. Moreover, the dependence of the normalized primitive cell volume V/Vo on pressure and the dependences of thermal expansion coefficient α on temperature and pressure are also obtained successfully.

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期刊信息
  • 《中国物理B:英文版》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国物理学会和中国科学院物理研究所
  • 主编:欧阳钟灿
  • 地址:北京 中关村 中国科学院物理研究所内
  • 邮编:100080
  • 邮箱:
  • 电话:010-82649026 82649519
  • 国际标准刊号:ISSN:1674-1056
  • 国内统一刊号:ISSN:11-5639/O4
  • 邮发代号:
  • 获奖情况:
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  • 被引量:406