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Combined investigation of water sorption on TiO_2 rutile (110) single crystal face: XPS vs. periodic DFT

机译:TiO_2金红石(110)单晶面上水吸附的组合研究:XPS与周期性DFT

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摘要

XPS and periodic DFT calculations have been used to investigate water sorption on the TiO_2 rutile (110) face. Two sets of XPS spectra were collected on the TiO_2 (110) single crystal clean and previously exposed to water: the first set with photoelectrons collected in a direction parallel to the normal to the surface; and the second set with the sample tilted by 70°, respectively. This tilting procedure promotes the signals from surface species and reveals that the first hydration layer is strongly coordinated to the surface and also that, despite the fact that the spectra were recorded under ultra-high vacuum, water molecules subsist in upper hydration layers. In addition, periodic DFT calculations were performed to investigate the water adsorption process to determine if molecular and/or dissociative adsorption takes place. The first step of the theoretical part was the optimisation of a dry surface model and then the investigation of water adsorption. The calculated molecular water adsorption energies are consistent with previously published experimental data and it appears that even though it is slightly less stable, the dissociative water sorption can also take place. This assumption was considered, in a second step, on a larger surface model where molecular and dissociated water molecules were adsorbed together with different ratio. It was found that, due to hydrogen bonding stabilisation, molecular and dissociated water molecules can coexist on the surface if the ratio of dissociated water molecules is less than ≈33%. These results are consistent with previous experimental works giving a 10-25% range.
机译:XPS和定期DFT计算已用于研究TiO_2金红石(110)面上的水吸附。在纯净的TiO_2(110)单晶上收集了两组XPS光谱,并预先将它们暴露在水中:第一组在平行于表面法线的方向上收集了光电子;第二组在垂直于表面法线的方向上收集了光电子。第二组样本分别倾斜70°。这种倾斜过程促进了来自表面物质的信号,并揭示了第一水合层与表面具有很强的配位性,而且尽管光谱是在超高真空下记录的,但水分子仍存在于上水合层中。此外,定期进行DFT计算以研究水吸附过程,以确定是否发生分子和/或解离吸附。理论部分的第一步是优化干燥表面模型,然后研究吸水率。计算得出的分子对水的吸附能与先前发表的实验数据一致,并且看来,即使它的稳定性稍差,但也可能发生解离水的吸附。在第二步中,在较大的表面模型中考虑了该假设,在该模型中,分子和离解的水分子以不同的比例吸附在一起。已发现,由于氢键稳定作用,如果离解的水分子的比例小于约33%,则分子和离解的水分子可以共存于表面。这些结果与以前的实验工作相符,给出了10-25%的范围。

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