| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1517440 | Journal of Physics and Chemistry of Solids | 2008 | 5 Pages |
Abstract
We report new shock-compression data for single-crystal MgO at 114 and 192 GPa. Our data together with the existing shock-wave data revealed a volume discontinuity at 170±10 GPa along with the MgO Hugoniot. The discontinuity gives a volume increase of 1.9%, indicating a possible phase transition from a rock-salt structure (B1) to a high-temperature phase along with the MgO Hugoniot. We re-examined the Hugoniot data on polycrystalline sample (Mg0.6, Fe0.4)O up to 200 GPa [M.S. Vassiliou, T.J. Ahrens, The equation of state of Mg0.6Fe0.4O to 200 GPa, Geophys. Res. Lett. 9 (1982) 127-130], which showed similar discontinuity with a 2.2% volume increase at 135±10 GPa. Our results add to fundamental understandings of the behavior of MgO and the lower mantle mineral magnesiowüstite (Mg, Fe)O at ultrahigh pressure and temperature.
Related Topics
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Authors
Li Zhang, Zizheng Gong, Yingwei Fei,