尖晶石
八面体
反向
磁矩
离子
凝聚态物理
材料科学
化学
物理
结晶学
冶金
数学
量子力学
几何学
作者
Y.H. Hou,Yu‐Jun Zhao,Liu Hon,Huangzhong Yu,Xichun Zhong,Weidong Qiu,Dechang Zeng,Wen Li
标识
DOI:10.1088/0022-3727/43/44/445003
摘要
Partially inverse spinel CoFe 2 O 4 , which may be prepared through various heat treatments, differs remarkably from the ideal inverse spinel in many properties. The structure of partially inverse spinel CoFe 2 O 4 as well as its electronic and magnetic properties through a systemic theoretical calculation of (Co 1− x Fe x ) Tet (Co x Fe 2− x ) Oct O 4 ( x = 0, 0.25, 0.5, 0.75 and 1.0) have been investigated by the generalized gradient approximation (GGA) + U approach. It is found that the Co and Fe ions prefer their high spin configurations with higher spin moments at octahedral sites in all the studied cases, in line with experimental observations. The Co ions at the octahedral sites favour being far away from each other in the partial inverse spinels, which also show half metallicity at certain inversion degrees.
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