BADDELEYITE-TYPE HIGH-PRESSURE PHASE OF TIO2

被引:185
作者
SATO, H
ENDO, S
SUGIYAMA, M
KIKEGAWA, T
SHIMOMURA, O
KUSABA, K
机构
[1] OSAKA UNIV, EXTREME MAT RES CTR, TOYONAKA, OSAKA 560, JAPAN
[2] NATL INST RES INORGAN MAT, TSUKUBA 305, JAPAN
[3] NATL LAB HIGH ENERGY PHYS, TSUKUBA, IBARAKI 305, JAPAN
[4] TOHOKU UNIV, INST MAT RES, SENDAI, MIYAGI 980, JAPAN
关键词
D O I
10.1126/science.251.4995.786
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A high-pressure phase of TiO2, 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 ZrO2 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.
引用
收藏
页码:786 / 788
页数:3
相关论文
共 15 条