Effects of vacancy defects on Fe properties incorporated in MgO

被引:2
|
作者
Yang, Kaishuai [1 ,2 ,3 ]
Wang, Xianlong [1 ,2 ]
Zhang, Jie [1 ]
Cheng, Ya [1 ,2 ]
Zhang, Chuanguo [1 ]
Zeng, Zhi [1 ,2 ,3 ]
Lin, Haiqing [3 ]
机构
[1] Chinese Acad Sci, Inst Solid State Phys, Key Lab Mat Phys, Hefei 230031, Anhui, Peoples R China
[2] Univ Sci & Technol China, Hefei 230026, Anhui, Peoples R China
[3] Beijing Computat Sci Res Ctr, Beijing 100084, Peoples R China
基金
中国国家自然科学基金;
关键词
vacancy defect; defect concentration; Fe-bearing MgO; AUGMENTED-WAVE METHOD; EARTHS LOWER MANTLE; MAGNESIUM-OXIDE; SPIN TRANSITION; HIGH-PRESSURE; AB-INITIO; DOPED MGO; CONDUCTIVITY; (MG; FE)O; IRON;
D O I
10.1088/1361-648X/aacabd
中图分类号
O469 [凝聚态物理学];
学科分类号
070205 ;
摘要
Distributions of Fe in MgO containing Mg vacancy, O vacancy, and Schottky defect are investigated based on the density functional theory (DFT). Our results show that since Mg vacancy will remove electrons from MgO, Fe tends to get close to Mg vacancy but far from O vacancy. The Mg vacancy can decrease the magnetic moment of iron and change its valence state from 2+ to 3+, which leads to similar to 5% decrease of Fe-O bond length comparable to the effect of 30GPa external pressure. Furthermore, iron incorporation can increase the Schottky defect concentration of MgO especially in the enviromnent of the Earth's lower mantle, where similar to 20 mol% Fe-bearing MgO locates at extreme high temperature conditions.
引用
收藏
页数:7
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