Fe3O4 surface electronic structures and stability from GGA plus U

被引:129
作者
Yu, Xiaohu [1 ]
Huo, Chun-Fang [1 ]
Li, Yong-Wang [1 ]
Wang, Jianguo [1 ]
Jiao, Haijun [1 ,2 ]
机构
[1] Univ Rostock, Leibniz Inst Katayse eV, D-18059 Rostock, Germany
[2] Chinese Acad Sci, Inst Coal Chem, State Key Lab Coal Convers, Taiyuan 030001, Shanxi, Peoples R China
基金
中国国家自然科学基金;
关键词
Magnetite; Fe3O4; Surface termination; Stability; Magnetism; SCANNING-TUNNELING-MICROSCOPY; TOTAL-ENERGY CALCULATIONS; IRON-OXIDE; FILMS; STM; RECONSTRUCTION; TERMINATION; WATER;
D O I
10.1016/j.susc.2012.02.003
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The electronic structures, stabilities and magnetic properties of the Fe3O4(111), (110) and (001) surfaces have been computed at the level of density functional theory by including the Hubbard parameter (U) for describing the on-site Coulomb interaction of iron 3d electrons. Among the six Fe3O4(111) terminations, the Fe-tet1 (exposing tetrahedral coordinated iron) and Fe-oct2 (exposing octahedral coordinated iron) terminations are more stable and have metallic character. For the Fe3O4(110) surface, strong surface distortion has been found; the A-layer termination (exposing tetrahedral coordinated iron) has metallic character, while the B-layer termination (exposing tetrahedral and octahedral coordinated iron) has half-metal character. For the Fe3O4(001) surface, both A-layer (exposing tetrahedral coordinated iron) and B-layer (exposing octahedral coordinated iron) terminations have half-metal character. The surface stability of (111) > (001) > (110) on the basis of the computed surface energies agrees well with the experimental findings, and explains reasonably the observed diversity and complexity of the experiments. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:872 / 879
页数:8
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