Structure of Single-Crystal Rutile (TiO2) Prepared by High-Temperature Ultracentrifugation

被引:16
|
作者
Mashimo, Tsutomu [1 ]
Bagum, Rabaya [1 ]
Ogata, Yudai [1 ]
Tokuda, Makoto [1 ]
Okube, Maki [3 ]
Sugiyama, Kazumasa [3 ]
Kinemuchi, Yoshiaki [4 ]
Isobe, Hiroshi [2 ]
Yoshiasa, Akira [2 ]
机构
[1] Kumamoto Univ, Inst Pulsed Power Sci, Kumamoto 8608555, Japan
[2] Kumamoto Univ, Fac Sci, Kumamoto 8608555, Japan
[3] Tohoku Univ, Inst Mat Sci, Sendai, Miyagi 9808577, Japan
[4] Natl Inst Adv Ind Sci & Technol, Nagoya, Aichi 4638560, Japan
关键词
METAL DIOXIDES; HIGH-PRESSURE; SEDIMENTATION;
D O I
10.1021/acs.cgd.6b01818
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
We report the preparation of single-crystal rutile (TiO2) with a unique structure prepared by ultracentrifugation. at high temperature (strong gravitational field). Single-crystal rutile was subjected along the c-axis direction to a gravitational field of 0.4 x 10(6) G at 400 degrees C, and the uniquely structured single crystal rutile, which did not conform to Pauling's third rule, was quenched at ambient conditions. The anisotropy (a/c ratio) of the tetragonal phase increased by 2%. The (Ti-Oa)/(Ti-Ob) and Os/Ou ratios increased by 1.6% and 3%, respectively, and approached 1; Ti-Oa and Ti-Ob are the two Ti-O interatomic distances, and Os and Ou are the shared edge Oa-Oa and the unshared edge Oa-Ob, respectively. This means that the TiO6 octahedral group became isotropic. Os was expanded from its normal size, in contradiction to the usual laws, by the strong gravitational force. Such a structural change has not previously been achieved under high-pressure or high-temperature conditions, and may be related to structural stabilization induced by a unique uniaxially distorted crystalline state under ultracentrifugation. Ab initio simulations supported the experimental results.
引用
收藏
页码:1460 / 1464
页数:5
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