Science. 1991 Feb 15;251(4995):786-8. doi: 10.1126/science.251.4995.786.
A high-pressure phase of TiO(2), which had been observed by shock-wave experiments and remained unresolved, has been studied by in situ x-ray diffraction. The single phase was formed at 20 gigapascals and 770 degrees C with the use of sintered-diamond multianvils; it has the same structure as baddeleyite, the stable phase of ZrO(2) at ambient conditions. The coordination number of Ti increases from six to seven across the rutile to baddeleyite transition, and the volume is reduced by approximately 9 percent.
一种高压相的 TiO(2),此前曾通过冲击波实验观察到,但仍未得到解决,现已通过原位 X 射线衍射进行研究。在使用烧结金刚石多砧的条件下,于 200GPa 和 770°C 下形成单相,其结构与在环境条件下稳定的 ZrO(2)的单斜相相同。在金红石到斜锆石的转变过程中,Ti 的配位数从六增加到七,体积减少了约 9%。