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Oxygen vacancies as active sites for H2S dissociation on the rutile TiO2(110) surface: a first-principles study

机译:氧空位作为金红石TiO2(110)表面H2S分解的活性位点:一项第一性原理研究

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Spin-polarized DFT+U computations have been performed to investigate the role of oxygen vacancies in dissociating H2S on the rutile TiO2(110) surface. A bridged O(2)c atom is demonstrated to be the most energetically favorable oxygen vacancy site, which makes V(O(2)c) an electron donator center and induces an isolated defect level with narrowed band gaps. A H2S molecule is adsorbed dissociatively over V(O(2)c), but molecularly on the perfect surface. For H2S dissociation, the HS/H intermediate state reveals the best thermal stability on both defected and perfect surfaces. Moreover, potential energy surface analysis shows that V(O(2)c) reduces markedly the energy barriers for the paths along H2S dissociation. This indicates oxygen vacancies to be efficient trap centers for H2S dissociation, as evidenced by a significant interfacial charge transfer promoted by vacancies. This work could provide insights into the role of oxygen vacancies in facilitating the decomposition of H2S on rutile TiO2(110) surface.
机译:自旋极化DFT + U计算已进行以调查氧空位在金红石TiO2(110)表面上离解H2S中的作用。桥接的O(2)c原子被证明是能量上最有利的氧空位,这使V(O(2)c)成为电子供体的中心,并诱导了带隙狭窄的孤立缺陷能级。 H2S分子解离地吸附在V(O(2)c)上,但分子吸附在理想表面上。对于H2S离解,HS / H中间态在有缺陷的表面和完美的表面均显示出最佳的热稳定性。此外,势能表面分析表明,V(O(2)c)显着降低了沿H2S离解路径的能垒。这表明氧空位是H2S离解的有效陷阱中心,空位促进了界面电荷的大量转移。这项工作可以提供氧空位在促进金红石TiO2(110)表面上的H2S分解中的作用的见解。

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