[Raman characterization of rutile phase transitions under high-pressure and high-temperature].

The pressure-induced phase transition of rutile-structured TiO2 was investigated by in-situ Raman spectrum method in a laser-heated diamond anvil cell (DAC). The experiment was conducted at 35 GPa under quasihydrostatic conditions using argon as medium. At room temperature, the rutile-type TiO2 begins to transform to baddeleyite-type phase at 13.4 GPa and completes at 21 GPa, and this new high-pressure structure retains up to 35 GPa, the upmost pressure used in this study. At the pressure of 29.4 GPa the sample of baddeleyite-type TiO2 was heated by an YAG laser to about 1 000-1500 degrees C, and then the baddeleyite phase transformed to a Pbca phase. The Pbca phase was heated again at 35.0 GPa and it was still stable. The sample then began to be decompressed, and the Pbca phase of TiO2 transformed to baddeleyite structure at 26.3 GPa, which stayed stable to 11.4 GPa. The formation of Pbca phase from baddeleyite phase needs the condition of high temperature, it transforms back to badde-leyite structure completely at pressure of a little below that on its formation, which suggests the boundary of the two phases can be determined at about 28 GPa. At 7. 6 GPa, and the Raman spectrum shows the characteristics of the mixture of two phases of baddeleyite-type and alpha-PbO2-type, which indicates that the baddeleyite phase transforms to alpha-PbO2 phase at about 7 GPa. The alpha-PbO2-type TiO2 is metastable under ambient condition.

[Raman scattering study of water up to 600 MPa at 290 K].

Raman scattering studies of the stretching band from liquid water have been conducted up to 600 MPa at 290 K. It is shown that (r1)(max) decreases with increasing pressure initially and reaches the minimum at about 200 MPa, and increases at higher pressure up to about 400 MPa, then decreases with increasing pressure up to 600 MPa. And this is also in accordance with the behavior of r(oo) under pressure. The authors conclude that, just like ice phase transition ice ( I h) --> ice(II) --> ice (V), there also probably exists water phase transition water ( I h) --> water (III) --> water (V).