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Temperature dependence of magnetic anisotropy constant in iron chalcogenide Fe3Se4: Excellent agreement with theories

机译:硫铁矿Fe3Se4的磁各向异性常数的温度依赖性:与理论的良好一致性

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摘要

Magnetic hysteresis loops were measured for ferrimagnetic iron chalcogenide Fe3Se4 nanoparticles in the whole temperature range below the Curie temperature TC (315 K). The coercivity of the material is huge, reaching about 40 kOe at 10 K. The magnetic anisotropy constant K was determined from the magnetic hysteresis loop using the law of approach to saturation. The deduced anisotropy constant at 10 K is 5.22 × 106 erg/cm3, which is over one order of magnitude larger than that of Fe3O4. We also demonstrated that the experimental magnetic hysteresis loop is in good agreement with the theoretical curve calculated by Stoner and Wohlfarth for a noninteracting randomly oriented uniaxial single-domain particle system. Moreover, we show that K is proportional to the cube of the saturation magnetization Ms, which confirms earlier theoretical models for uniaxial magnets.
机译:在低于居里温度TC(315 K)的整个温度范围内,对亚铁磁性硫族元素铁Fe3Se4纳米粒子的磁滞回线进行了测量。材料的矫顽力很大,在10 K时达到约40 kOe。磁各向异性常数K由磁滞回线使用饱和法则确定。推导的10ducK处的各向异性常数为5.22×10 6 erg / cm 3 ,比Fe3O4大一个数量级。我们还证明了实验性磁滞回线与Stoner和Wohlfarth计算的非相互作用随机取向单轴单畴粒子系统的理论曲线非常吻合。此外,我们表明K与饱和磁化强度Ms的立方成正比,这证实了单轴磁体的早期理论模型。

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