High-pressure experiments identify ice-VII to ice-X transition at 30.9 GPa with 2.5-fold bulk modulus increase and an intermediate tetragonal phase at 5.1 GPa, with implications for planetary interiors.
Phase diagram of H 2 O: Thermody- namic functions of the phase transitions of high-pressure ices.Solar System Research 2010, 44, 202–222
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Bond strengthening in dense H2O and implications to planetary composition
High-pressure experiments identify ice-VII to ice-X transition at 30.9 GPa with 2.5-fold bulk modulus increase and an intermediate tetragonal phase at 5.1 GPa, with implications for planetary interiors.