As the pressure is raised and the O···O
distance contracts, ice-seven appears to undergo a
continuous transition into cubic ice-ten (ice X)
(still
space group, a, b, c = 2.78 Å at
62 GPa, 300 K [719])
where the ice protons are equispaced (and equally
bonded) between the oxygen atoms
in a molecular crystal [1621]. The oxygen atoms are arranged
in a body-centered cubic arrangement (8 neighbors)
and the hydrogen atoms in a body-centered truncated
cubic arrangement (12 neighbors).
The melting curve for ice-ten has been proposed at high temperatures (1000-2400 K) [612a]. As ice X is approached with increasing pressure from very hot liquid water and the O-H energy minima draw near to each other, the protons rapidly swap positions giving many short-lived OH- and H3O+ ions [612b]. In the ice X, however, protons are less mobile than in ice VII as there is only one energy minimum for each O-H-O bond,
Ice-ten looks identical as seen from the x, y or z direction.
Ice-ten has triple points with ice-seven and ice-eight (100 K, 62 GPa) and ice-seven and water (~1000 K, ~47 GPa) [612b].
Interactive Jmol structures are given.
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This page was last updated by Martin Chaplin on 10 April, 2012