First results on a systematic study of ice by Raman scattering and X-ray diffraction in the megabar range are reported. Our discussion, which is based on the dynamical features of ice and its phase diagram, focuses on the possible occurrence of a symmetric state (ice X). It is concluded that above 62 GPa, delocalization of the proton occurs along O−O directions and ice may be symmetric from the statistical viewpoint.
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Pruzan et al. (1997) studied this question.
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