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[高压高温下金红石相转变的拉曼表征]

[Raman characterization of rutile phase transitions under high-pressure and high-temperature].

作者信息

Xiao Wan-Sheng, Zhang Hong, Tan Da-Yong, Weng Ke-Nan, Li Yan-Chun, Luo Chong-Ju, Liu Jing, Xie Hong-Sen

机构信息

Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.

出版信息

Guang Pu Xue Yu Guang Pu Fen Xi. 2007 Jul;27(7):1340-3.

Abstract

The pressure-induced phase transition of rutile-structured TiO2 was investigated by in-situ Raman spectrum method in a laser-heated diamond anvil cell (DAC). The experiment was conducted at 35 GPa under quasihydrostatic conditions using argon as medium. At room temperature, the rutile-type TiO2 begins to transform to baddeleyite-type phase at 13.4 GPa and completes at 21 GPa, and this new high-pressure structure retains up to 35 GPa, the upmost pressure used in this study. At the pressure of 29.4 GPa the sample of baddeleyite-type TiO2 was heated by an YAG laser to about 1 000-1500 degrees C, and then the baddeleyite phase transformed to a Pbca phase. The Pbca phase was heated again at 35.0 GPa and it was still stable. The sample then began to be decompressed, and the Pbca phase of TiO2 transformed to baddeleyite structure at 26.3 GPa, which stayed stable to 11.4 GPa. The formation of Pbca phase from baddeleyite phase needs the condition of high temperature, it transforms back to badde-leyite structure completely at pressure of a little below that on its formation, which suggests the boundary of the two phases can be determined at about 28 GPa. At 7. 6 GPa, and the Raman spectrum shows the characteristics of the mixture of two phases of baddeleyite-type and alpha-PbO2-type, which indicates that the baddeleyite phase transforms to alpha-PbO2 phase at about 7 GPa. The alpha-PbO2-type TiO2 is metastable under ambient condition.

摘要

采用原位拉曼光谱法,在激光加热金刚石对顶砧(DAC)中研究了金红石结构TiO₂的压力诱导相变。实验在准静水压条件下,以氩气为介质,在35 GPa压力下进行。室温下,金红石型TiO₂在13.4 GPa开始转变为斜锆石型相,并在21 GPa时完成转变,这种新的高压结构在本研究使用的最高压力35 GPa下保持稳定。在29.4 GPa压力下,用YAG激光将斜锆石型TiO₂样品加热至约1000 - 1500℃,然后斜锆石相转变为Pbca相。在35.0 GPa再次加热时,Pbca相仍然稳定。随后样品开始减压,TiO₂的Pbca相在26.3 GPa转变为斜锆石结构,并在11.4 GPa保持稳定。斜锆石相形成Pbca相需要高温条件,在略低于其形成压力时完全转变回斜锆石结构,这表明两相边界可在约28 GPa确定。在7.6 GPa时,拉曼光谱显示出斜锆石型和α - PbO₂型两相混合的特征,这表明斜锆石相在约7 GPa转变为α - PbO₂相。α - PbO₂型TiO₂在环境条件下是亚稳的。

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