Transactions of the Indian Institute of Metals ( IF 1.5 ) Pub Date : 2021-05-07 , DOI: 10.1007/s12666-021-02270-1 Feng Zhou , Ming Zhang , Zhou Pu , Boquan Li
The interaction between O2 and magnetite (Fe3O4) (1 1 1) surface is investigated using density functional theory (DFT). The calculated results show that O2 perpendicular to the Fetet-terminated and parallel to the Feoct-terminated are the two of the most stable configurations, which is converted to a similar structure after optimization. The adsorbed O2 gains charges from the nearest Fe atom, while the Fe atom gets compensation from the surface. Further analysis of two stable structures show that there is a strong interaction between O2 and Fe3O4 (1 1 1) surface, and the O–O bond is elongated and weakened after adsorption.
中文翻译:
氧与(Fe 3 O 4)(1 1 1)表面相互作用的原子尺度研究
利用密度泛函理论(DFT)研究了O 2与磁铁矿(Fe 3 O 4)(1 1 1)表面之间的相互作用。计算结果表明,垂直于Fe tet端基和平行于Fe oct端基的O 2是最稳定的两个构型,经过优化后转化为相似的结构。吸附的O 2从最近的Fe原子获得电荷,而Fe原子从表面获得补偿。对两种稳定结构的进一步分析表明,O 2和Fe 3 O 4之间存在很强的相互作用 (1 1 1)表面,并且O–O键在吸附后被拉长和减弱。