Senior Research Fellow Center, Ehime University, 2-5 Bunkyo-cho, Matsuyama, Ehime 790-8577, Japan.
Phys Rev Lett. 2011 Jul 22;107(4):045701. doi: 10.1103/PhysRevLett.107.045701.
We report the discovery of a post-cotunnite phase of TiO2 by both density-functional ab initio calculations and high-pressure experiments. A pressure-induced phase transition to a hexagonal Fe2P-type structure (space group P62m) was predicted to occur at 161 GPa and 0 K and successfully observed by in situ synchrotron x-ray diffraction measurements at 210 GPa and 4000 K with a significant increase in opacity. This change in opacity is attributed to a reduction of band gap from 3.0 to 1.9 eV across the phase change. The Fe2P-type structure is proved to be the densest phase in major metal dioxides.
我们通过密度泛函从头计算和高压实验发现了钛 dioxide 的一种后钙钛矿相。预测在 161 GPa 和 0 K 下会发生一个向六方 Fe2P 型结构(空间群 P62m)的压力诱导相变,并通过在 210 GPa 和 4000 K 下进行的原位同步辐射 X 射线衍射测量成功观察到,同时伴随着明显的不透明度增加。这种不透明度的变化归因于带隙从 3.0 eV 减小到相变时的 1.9 eV。Fe2P 型结构被证明是主要金属氧化物中密度最大的相。