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α-Fe2O3单离子磁晶各向异性的计算及Morin转变的解释
引用本文:李华,姜寿亭,梅良模,郭贻诚,杨桂林,徐游,翟宏如.α-Fe2O3单离子磁晶各向异性的计算及Morin转变的解释[J].物理学报,1988,37(1):36-42.
作者姓名:李华  姜寿亭  梅良模  郭贻诚  杨桂林  徐游  翟宏如
作者单位:(1)南京大学物理系; (2)山东大学物理系
摘    要:本文根据晶场理论计算了α-Fe2O3的单离子磁晶各向异性。采用点电荷模型,计及近邻及次近邻对晶场的贡献,并考虑到近邻O2-离子对次近邻Fe3+离子的电屏蔽效应,在六级微扰近似下,得到单离子各向异性场Hsi=102.3×102Oe。这一结果结合Artman等人对磁偶极各向异性的计算,导出了α-Fe2O3的Morin转变温度T 关键词

收稿时间:2/2/1987 12:00:00 AM

CALCULATION OF MAGNETIC SINGLE-ION ANISOTROPY AND THE MORIN TRANSITION IN HEMATITE
LI HUA,JIANG SHOU-TING,MEI LIANG-MO,GUO YI-CHENG,YANG GUEI-LIN,XU YOU and ZHAI HONG-RU.CALCULATION OF MAGNETIC SINGLE-ION ANISOTROPY AND THE MORIN TRANSITION IN HEMATITE[J].Acta Physica Sinica,1988,37(1):36-42.
Authors:LI HUA  JIANG SHOU-TING  MEI LIANG-MO  GUO YI-CHENG  YANG GUEI-LIN  XU YOU and ZHAI HONG-RU
Abstract:A calculation of magnetic single-ion anisotropy in hematite (α-Fe2O3) has been made, based on point-charge model in crystalline field. The nearest-neighbor O2- ions and the nexi-nearest-neighbor Fe3+ ions were chosen as ligands and the effect of electrostatic shield provided by the O2- ions was taken into account. Considering the sixth order perturbation, we ob-tained an equivalent single-ion anisotropy field Hsi=102.3×102 Oe. Making use of this results in conjunction with the computed equivalent dipolar anisotropy field by Artmen et al,. the Morin transition temperature in hematite TM=261 K was obtained, which is in good agreement with the experimental value. Based on the linear approximation principle, we got the TM-n relation for low n value in α-(Fe-1nAln)2O3. With this relation the dependence of the-Morin transition temperature, TM, on n in low n value range could be explained quite well.
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