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A Photoelectron Spectroscopy Study of Stoichiometric and Reduced Anatase TiO2 (101) Surfaces: The Effect of Subsurface Defects on Water Adsorption at Near-Ambient Pressures

机译:化学计量和还原锐钛矿型TiO2(101)表面的光电子能谱研究:次表面缺陷对近环境压力下水吸附的影响

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摘要

X-ray photoelectron (XPS) experiments at normal and grazing emission are performed, demonstrating the labile nature of the anatase TiO2(101) surface after argon cluster ion sputtering and the propensity of oxygen vacancies to migrate subsurface at room temperature. Near-ambient XPS (NAP-XPS) shows that molecular water adsorbs on the anatase TiO2(101) surface at pressures of 0.6 mbar and above, at room temperature, in a mixed molecular and dissociated state. Water adsorbs in a similar fashion on both sputtered and stoichiometric surfaces and reaches a saturation point between 0.6 and 1.8 mbar at room temperature. This means there is little difference in reactivity with regards to water adsorption on both sputtered and stoichiometric surfaces, giving credence to the theory that anatase has superior photocatalytic activity over rutile due to the tendency of oxygen vacancies to lie subsurface, therefore being able to contribute to photocatalysis without being quenched by adsorbates.
机译:进行了正常和掠射发射的X射线光电子(XPS)实验,证明了氩簇离子溅射后锐钛矿型TiO2(101)表面的不稳定性质以及室温下氧空位迁移至地下的倾向。接近环境的XPS(NAP-XPS)表明,分子水在室温下以0.6 mbar或更高的压力以混合分子和离解态吸附在锐钛矿型TiO2(101)表面上。水在溅射表面和化学计量表面上的吸附方式相似,在室温下达到0.6至1.8 mbar的饱和点。这意味着在溅射表面和化学计量表面上,水的吸附反应性几乎没有差异,这证明了锐钛矿具有优于金红石的光催化活性的理论,这归因于氧空位位于表面之下的趋势,因此能够促进无需被吸附物淬灭即可进行光催化。

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