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ANISOTROPIC CURIE TEMPERATURE MATERIALS (PLENARY)

机译:各向异性居里温度材料(全体会议)

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摘要

Existence of anisotropic Curie temperature materials [E. R. Callen, Phys. Rev. 124, 1373 (1961); J. Appl. Phys. 32 S221 (1961)] is a longstanding prediction - materials that become paramagnetic at a lower temperature along certain crystal directions while remaining magnetically ordered in other directions up to a higher temperature. Validating Callen's theory, we show that all directions within the basal plane of monoclinic Fe_7S_8 (pyrrhotite) single crystal remain ordered up to 603 K while the c-axis becomes paramagnetic at 225 K. Results prompt a re-evaluation of existing magnetic materials with a focus on magnetic characteristics along different crystal orientations above instead of below the ordering temperatures. Theoretical guidelines for identifying new materials with large anisotropy of Curie temperature are also given, and analysis protocol to characterize them in a self-consistent manner is discussed. Materials with such a large directional dependence of Curie temperature open the possibility for uniquely new devices and phenomena, including energy storage and spintronics devices.
机译:各向异性居里温度材料的存在[E. R. Callen,物理学Rev.124,1373(1961); J.应用物理[32S221(1961)]是长期的预测-材料在较低温度下沿某些晶体方向变为顺磁性,而在其他方向上保持磁性有序,直至较高的温度。验证卡伦理论的结果,我们表明单斜晶Fe_7S_8(硫铁矿)单晶基面内的所有方向在603 K时仍保持有序,而c轴在225 K时变为顺磁性。结果促使人们对现有的磁性材料进行了重新评估。专注于沿着高于而不是低于订购温度的不同晶体取向的磁特性。还给出了识别具有居里温度各向异性的新材料的理论指导,并讨论了以自洽的方式表征它们的分析协议。居里温度对方向的依赖性如此大的材料为独特的新设备和现象打开了可能性,包括能量存储和自旋电子设备。

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