尖晶石Fe3O4电子结构的第一性原理研究

Riyajul Islam, Molongnenla, D. Saikia, J. P. Borah
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引用次数: 3

摘要

本文采用密度泛函理论框架下的LDA、带PBE泛函的GGA和GGA+U近似,对铁磁性立方尖晶石磁铁矿(Fe3O4)的结构、电子和磁性进行了比较研究。研究表明,与LDA相比,GGA的结构参数与实验数据的相对偏差较小。总DOS和能带结构表明Fe3O4具有半金属性质。发现GGA+U计算的带隙值比GGA和LDA计算的带隙值高,与实验值吻合较好。在所有近似中,Fe3O4的总磁矩几乎相等,而在GGA +U中,Fe和O的部分磁矩分别增大和减小。本文采用密度泛函理论框架下的LDA、带PBE泛函的GGA和GGA+U近似,对铁磁性立方尖晶石磁铁矿(Fe3O4)的结构、电子和磁性进行了比较研究。研究表明,与LDA相比,GGA的结构参数与实验数据的相对偏差较小。总DOS和能带结构表明Fe3O4具有半金属性质。发现GGA+U计算的带隙值比GGA和LDA计算的带隙值高,与实验值吻合较好。在所有近似中,Fe3O4的总磁矩几乎相等,而在GGA +U中,Fe和O的部分磁矩分别增大和减小。
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First principle investigation of the electronic structure of spinel Fe3O4
A comparative study of the structural, electronic and magnetic properties of ferrimagnetic cubic spinel magnetite (Fe3O4) has been performed in the present report, using LDA, GGA with PBE functional and GGA+U approximations within the framework of density functional theory. Study reveals smaller relative deviations in the structural parameters from the experimental data with GGA compared to LDA. Total DOS and band structure results demonstrate half metallic behavior of Fe3O4. The value of the band gap calculated by GGA+U is found to be higher than that calculated by GGA and LDA which is in good agreement with the experimental value. The total magnetic moments of Fe3O4 are found to be nearly equal in all the approximations whereas the values of the partial magnetic moments of Fe and O are increased and decreased respectively in GGA +U.A comparative study of the structural, electronic and magnetic properties of ferrimagnetic cubic spinel magnetite (Fe3O4) has been performed in the present report, using LDA, GGA with PBE functional and GGA+U approximations within the framework of density functional theory. Study reveals smaller relative deviations in the structural parameters from the experimental data with GGA compared to LDA. Total DOS and band structure results demonstrate half metallic behavior of Fe3O4. The value of the band gap calculated by GGA+U is found to be higher than that calculated by GGA and LDA which is in good agreement with the experimental value. The total magnetic moments of Fe3O4 are found to be nearly equal in all the approximations whereas the values of the partial magnetic moments of Fe and O are increased and decreased respectively in GGA +U.
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