High-pressure Raman measurements of H2O ice using synthetic diamond anvils
reveal major changes associated with the transition to the nonmolecular, sy
mmetric hydrogen-bonded state. At 60 GPa the strongly pressure-dependent O-
H symmetric stretching mode disappears, and the translational modes exhibit
frequency and damping anomalies. With further increase in pressure, a sing
le peak appears and becomes the dominant feature in the spectrum in the meg
abar range. The band is assigned to the predicted Raman-active O-O mode of
the nonmolecular phase, consistent with the formation of cuprite-type ice X
with static, symmetric hydrogen bonds.