A possible existence of phase change of deuterated ice VII at about 11 GPa by X-ray and Raman studies

18th APS-SCCM; 24th AIRAPT

Kadobayashi, H.^1 ; Hirai, H.^1 ; Matsuoka, T.^2 ; Ohishi, Y.^3 ; Yamamoto, Y.^4

Geodynamics Research Center, Ehime University, Ehime, Matsuyama

790-8577, Japan^1

KYOKUGEN, Osaka University, Osaka, Toyonaka

560-8531, Japan^2

Japan Synchrotron Radiation Research Institute, Harima

679-5198, Japan^3

National Institute of Advanced Industrial Science and Technology, Tsukuba

305-8568, Japan^4

关键词: Diamond-anvil cell;    Diffraction lines;    High-pressure experiment;    Pressure ranges;    Raman studies;    Situ X-ray diffractometry;    Tetragonal structure;    Vibrational modes;   

Others  :  https://iopscience.iop.org/article/10.1088/1742-6596/500/18/182017/pdf
DOI  :  10.1088/1742-6596/500/18/182017

来源: IOP

【 摘 要 】

High pressure experiments were performed with deuterated ice VII using diamond anvil cell in a pressure range of 0.1 MPa to 60 GPa at room temperature in order to further understanding a long-argued issue of phase change in ice VII at approximately 11 GPa. In-situ X-ray diffractometry revealed splitting of diffraction lines of cubic ice VII above 11GPa, which were indexed as a tetragonal structure. The tetragonal structure survived at least up to 60 GPa. Pressure versus volume curves of cubic and tetragonal structures were obtained and the bulk moduli were calculated. Raman spectroscopy showed that the full width at half maximum of O-D vibrational mode decreased with increasing pressure, and showed minimum value at 11 GPa, and then it became broader again above this pressure. The squared vibrational frequency changed linearly with pressure, and the slope changed at about 14 GPa, indicating existence of phase change. All experimental results evidently supported the existence of phase change of ice VII at approximately 11 GPa.