Micromagnetic calculation of hysteresis as a function of temperature in pseudo-single domain magnetite

被引:13
作者
Muxworthy, AR
Williams, W
机构
[1] Univ Oxford, Dept Earth Sci, Oxford OX1 3PR, England
[2] Univ Edinburgh, Dept Geol & Geophys, Edinburgh EH9 3JW, Midlothian, Scotland
关键词
D O I
10.1029/1999GL900176
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Using an unconstrained three-dimensional micromagnetic model, magnetic hysteresis was simulated in magnetite in the grain size range 0.08-0.3 mu m as a function of temperature between 100 K and the Curie temperature (851 K). For all temperatures in the cubic phase above the Verwey transition (T-v approximate to 120 K), 0.08 mu m grains switched by coherent rotation, and 0.3 mu m grains switched with an intermediate vortex phase. The mode of switching for 0.1 mu m grains was found to be dependent on both field direction and temperature. For all grain sizes in the monoclinic phase below T-v, switching was by coherent rotation, with the domain state rotating in the monoclinic magnetocrystalline anisotropy "easy" a-plane. Calculations for coercive force (H-c) as a function of temperature display similar trends to experimental data. Below T-v, the model correctly predicts the large increase in H-c. However, the absolute values of H-c are higher than the experimental data.
引用
收藏
页码:1065 / 1068
页数:4
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