白长石
金红石
相(物质)
衍射
材料科学
分析化学(期刊)
相变
金刚石顶砧
钻石
高压
结晶学
矿物学
化学
热力学
冶金
光学
地质学
物理
锆石
地球化学
有机化学
色谱法
作者
Hiromasa Sato,S. Endo,Masashi Sugiyama,Takumi Kikegawa,Osamu Shimomura,Keiji Kusaba
出处
期刊:Science
[American Association for the Advancement of Science]
日期:1991-02-15
卷期号:251 (4995): 786-788
被引量:194
标识
DOI:10.1126/science.251.4995.786
摘要
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.
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