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Monoxide carbon frequency shift as a tool for the characterization of TiO2 surfaces: Insights from first principles spectroscopy

机译:一氧化碳碳频移作为表征TiO2表面的工具:第一原理光谱学的见解

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The adsorption and vibrational frequency of CO on defective and undefective titanium dioxide surfaces is examined applying first-principles molecular dynamics simulations. In particular, the vibrational frequencies are obtained beyond the harmonic approximation, through the time correlation functions of the atomic trajectories. In agreement with experiments, at low CO coverages we find an upshift in the vibration frequency with respect to the free CO molecule, of 45 and 35 cm~(-1) on the stoichiometric rutile (110) and anatase (101) faces, respectively. A band falling 8 cm~(-1) below the frequency corresponding to the perfect face is observed for the reduced rutile (110) surface in the low vacancy concentration limit, where the adsorption is favored on Ti~4 sites. At a higher density of defects, adsorption on Ti ~3 sites becomes more stable, accompanied by a downshift in the stretching band. In the case of anatase (101), we analyze the effect of subsurface oxygen vacancies, which have been shown to be predominant in this material. Interestingly, we find that the adsorption of CO on five coordinate Ti atoms placed over subsurface vacancies is favored with respect to other Ti ~4 sites (7.25 against 6.95 kcal/mol), exhibiting a vibrational redshift of 20 cm~(-1). These results provide the basis to quantitatively assess the degree of reduction of rutile and anatase surfaces via IR spectroscopy, and at the same time allow for the assignment of characteristic bands in the CO spectra on TiO_2 whose origin has remained ambiguous.
机译:应用第一性原理分子动力学模拟研究了在有缺陷和无缺陷的二氧化钛表面上CO的吸附和振动频率。特别地,通过原子轨迹的时间相关函数,获得了超出谐波近似的振动频率。与实验相一致,在低CO覆盖率下,我们发现化学计量金红石(110)和锐钛矿(101)面上的振动频率相对于游离CO分子分别上升了45和35 cm〜(-1)。 。在低空位浓度限制下,金红石(110)表面减少时,观察到一个比完美面孔对应的频率低8 cm〜(-1)的带,在Ti〜4位上吸附更为有利。在较高的缺陷密度下,Ti〜3位上的吸附变得更稳定,并伴随着拉伸带的下降。在锐钛矿(101)的情况下,我们分析了表面氧空位的影响,这种空位已被证明在该材料中占主导地位。有趣的是,我们发现,相对于其他Ti〜4位(7.25对6.95 kcal / mol),CO在位于地下空位上的五个配位Ti原子上的吸附更为有利,表现出20 cm〜(-1)的振动红移。这些结果提供了通过红外光谱定量评估金红石和锐钛矿表面还原程度的基础,同时允许在起源仍不明确的TiO_2上的CO光谱中分配特征带。

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