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首页> 外文期刊>International Journal of Quantum Chemistry >The effect of F--doping and temperature on the structural and textural evolution of mesoporous TiO2 powders
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The effect of F--doping and temperature on the structural and textural evolution of mesoporous TiO2 powders

机译:F掺杂和温度对介孔TiO2粉末结构和组织演变的影响

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Mesoporous F--doped TiO2 powders were prepared by hydrolysis of titanium tetraisopropoxide (TTIP) in a mixed NH4F-H2O solution. Effects of F- ion content and calcination temperatures on the phase composition and porosity of mesoporous titania were investigated by X-ray diffraction (XRD), transmission electron microscopy (TEM), scanning electron microscopy (SEM) and BET surface areas. The results showed the BET surface area (S-BET) of the pure and doped powders dried at 100degreesC ranged from 260 to 310m(2)/g as determined by nitrogen adsorption. With increasing calcination temperatures, the SBET values of the calcined titania powders decreased due to the increase in crystalline size. The pore size distribution was bimodal with fine intra-particle pore and larger inter-particle pore as determined by nitrogen adsorption isotherms. The peak pore diameter of intra-particle pore increases with increasing F- ion content. At 700degreesC, all the titania powders exhibit monomodal pore size distributions due to the complete collapse of the intra-particle pores. The crystallization of anatase was obviously enhanced due to F(-)doping at 400degreesC and 500degreesC. Moreover, with increasing F- ion concent, F- ions not only suppressed the formation of brookite phase at low temperature, but also prevented phase transition of anatase to rutile at high temperature. (C) 2003 Elsevier Inc. All rights reserved. [References: 38]
机译:通过在混合NH4F-H2O溶液中水解四异丙氧基钛(TTIP)制备介孔的F掺杂TiO2粉末。通过X射线衍射(XRD),透射电子显微镜(TEM),扫描电子显微镜(SEM)和BET表面积研究了F离子含量和煅烧温度对介孔二氧化钛相组成和孔隙率的影响。结果表明,通过氮气吸附测定,在100℃下干燥的纯净粉末和掺杂粉末的BET表面积(S-BET)为260至310m(2)/ g。随着煅烧温度的升高,由于晶体尺寸的增加,煅烧二氧化钛粉末的SBET值降低。孔径分布是双峰的,具有通过氮吸附等温线确定的细颗粒内孔和较大的颗粒间孔。颗粒内孔的峰值孔径随着F-离子含量的增加而增加。在700°C下,由于颗粒内孔的完全塌陷,所有二氧化钛粉末均表现出单峰孔径分布。由于在400℃和500℃下的F(-)掺杂,锐钛矿的结晶明显增强。而且,随着F-离子浓度的增加,F-离子不仅抑制了低温下的板钛矿相的形成,而且阻止了锐钛矿在高温下向金红石相的转变。 (C)2003 Elsevier Inc.保留所有权利。 [参考:38]

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