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首页> 外文期刊>International Journal of Quantum Chemistry >UNDERSTANDING OF HOMOGENEOUS SPONTANEOUS PRECIPITATION FOR MONODISPERSED TiO2 ULTRAFINE POWDERS WITH RUTILE PHASE AROUND ROOM TEMPERATURE
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UNDERSTANDING OF HOMOGENEOUS SPONTANEOUS PRECIPITATION FOR MONODISPERSED TiO2 ULTRAFINE POWDERS WITH RUTILE PHASE AROUND ROOM TEMPERATURE

机译:室温下呈金红石相的单分散TiO2超细粉末的均相自发沉淀

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Monodispersed TiO2 ultrafine particles were obtained from aqueous TiOCl2 solution with a 0.67 M Ti4+ concentration prepared by diluting TiCl4 with the homogeneous precipitation process in the range 17-230 C. With the spontaneous hydrolysis of TiOCl2, which means the natural decrease of the pH value in the aqueous solution, all monodispersed precipitates were crystallized with the anatase or rutile TiO2 phase during the reactions. The TiO2 precipitate with the pure rutile phase was fully formed at temperatures below 65 C, which did not involve the evaporation of H2O, and above 155 C, which were available by suppressing it. The TiO2 precipitate with the rutile phase, including a small amount of the anatase phase, started to be formed at intermediate temperatures above 70 C, showing the full formation of the anatase phase above 95 C under the free evaporation of H2O. However, in the case of completely suppressing H2O evaporation at temperatures above 70 C, the TiO2 precipitate with the anatase phase that had already been formed by rapid reaction was fully transformed with the reaction time into the precipitate with the rutile phase by the vapor pressure of H2O. Therefore, the formation of TiO2 precipitates with the rutile phase around RT would be caused by the existence of capillary pressure between the agglomerated needle-shaped particles or the ultrafine clusters, together with the slow reaction rate. 21 refs.
机译:由浓度为0.67 M的TiOCl2水溶液获得的单分散TiO2超细颗粒,该浓度是通过在17-230 C范围内进行均匀沉淀过程稀释TiCl4制备的。随着TiOCl2的自发水解,意味着pH值自然降低。在水溶液中,反应过程中所有的单分散沉淀物都用锐钛矿或金红石型TiO2相结晶。具有纯金红石相的TiO2沉淀物在低于65°C(不涉及H2O蒸发)的温度和高于155°C(可通过抑制其蒸发)的温度下完全形成。在高于70 C的中间温度下开始形成具有金红石相(包括少量锐钛矿相)的TiO2沉淀,表明在水的自由蒸发下高于95 C的锐钛矿相完全形成。但是,在70℃以上的温度下完全抑制H2O蒸发的情况下,通过快速反应已经形成的具有锐钛矿相的TiO2沉淀物随反应时间的增加而完全转化为金红石相的沉淀物。水因此,RT周围金红石相形成的TiO2沉淀物的形成是由于团聚的针状颗粒或超细团簇之间存在毛细压力,并且反应速度慢。 21个参考

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