Equation of state of elbaite at high pressure up to 21.1 GPa and room temperature

被引:0
作者
Wei Chen
Shijie Huang
Zhilin Ye
Jiamei Song
Shanrong Zhang
Mengzeng Wu
Dawei Fan
Wenge Zhou
机构
[1] Institute of Geochemistry,Key Laboratory of High
[2] Chinese Academy of Sciences,Temperature and High
[3] University of Chinese Academy of Sciences,Pressure Study of the Earth’s Interior
[4] Guizhou Polytechnic of Construction,undefined
来源
Physics and Chemistry of Minerals | 2022年 / 49卷
关键词
Elbaite; Equation of state; Axial compression anisotropy; Synchrotron X-ray diffraction; High pressure;
D O I
暂无
中图分类号
学科分类号
摘要
The equation of the state of a natural elbaite sample has been investigated at room temperature and up to 21.1 GPa for the first time using in situ synchrotron X-ray diffraction in this study. No phase transition is observed on elbaite over the experimental pressure range. The pressure–volume data were fitted by the third-order Birch-Murnaghan equation of state (EoS) with the zero-pressure unit-cell volume V0 = 1540.7 (6) Å3, the zero-pressure bulk modulus KT0 = 114.7 (7) GPa, and its pressure derivative K'T0 = 4.2 (1), while obtained V0 = 1540.1 (4) Å3 and KT0 = 116.4 (4) GPa when fixed K'T0 = 4. Furthermore, the axial compressional behavior of elbaite was also fitted with a linearized third-order Birch-Murnaghan EoS, the obtained axial moduli for a-axis and c-axis are Ka0 = 201 (4) GPa and Kc0 = 60 (1) GPa, respectively. The axial compressibilities of a-axis and c-axis are βa = 1.66 × 10–3 GPa−1 and βc = 5.56 × 10–3 GPa−1 with an anisotropic ratio of βa: βc = 0.30: 1.00, which shows an intense axial compression anisotropy. The potential influencing factors on the bulk moduli and the anisotropic linear compressibilities of tourmalines were further discussed.
引用
收藏
相关论文
共 287 条
  • [1] Andreozzi GB(2020)Crystal-chemical behavior of Fe Phys Chem Miner 47 25-59
  • [2] Bosi F(2000) in tourmaline dictated by structural stability: insights from a schorl with formula Na Rev Miner Geochem 41 35-32
  • [3] Celata B(2007)(Fe J Appl Cryst 40 26-419
  • [4] Capizzi LS(2014)Al) Z Kristallogr 229 405-861
  • [5] Stagno V(2021)(Al Am Miner 106 851-410
  • [6] Beckett-Brown CE(2003)Fe Geology 31 407-155
  • [7] Angel RJ(2016))(Si Contrib Miner Pet 171 31-1015
  • [8] Angel RJ(2017)O Lithos 284–285 138-924
  • [9] Bujak M(2019))(BO Am Mineral 104 1005-1268
  • [10] Zhao J(1947)) Phys Rev 71 809-306