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Magnetic characterization and low-temperature heat transport properties of the orthoferrites RFeO3(R = rare earth and Y) single crystals

机译:Orthoferites RFEO 3 (R =稀土和Y)单晶的磁性表征和低温热传递性能

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Summary form only given. Orthoferrites RFeO(except R=Y, La and Lu) possess two sets of magnetic sublattice, that is, Fe sub-system and R sub-system. Magnetic properties and interactions between the two sub-systems including Fe-Fe, R-Fe, and R-R interactions depend on external parameters, such as temperature, magnetic field, etc. So real magnetic materials can exhibt rich low temperature characteristics. We have successfully grown the orthoferrites RFeO(R = Dy, Ho and Y) and HoYFeO(x = 0 .1 and 0 .3) by the floating zone technique using a four-mirror image furnace. The halogen lamp power and crystal growth atmosphere were identified to be the most important parameters. High-quality single crystals have been demonstrated by the X-ray diffraction data and X-ray Laue photograph. The magnetic transitions with decreasing temperature and the field-induced magnetic phase transitions in RFeO for the rare earth ions and Fe can be characterized by low-temperature magnetization and specific heat measurements. In addition, we report the low-temperature heat transport measurements of these orthoferrites single crystals to probe the magnetic properties and find that they show strong magnetic field dependence. The characteristic fields have a good correspondence with some transformations of the magnetic structure. These special behaviors demonstrate the magnetic field-induced transitions of the Fe and R spin structure.
机译:摘要表格仅给出。 Orthoferrites RFEO(r = y,la和lu除外)拥有两组磁性子块,即FE子系统和R子系统。包括Fe-Fe,R-Fe和R-R相互作用的两个子系统之间的磁性和相互作用取决于外部参数,例如温度,磁场等。因此,实际磁性材料可以表现出丰富的低温特性。我们已经成功地通过使用四镜像炉通过浮区技术成功地生长了Orthoferrites RFeo(r = dy,Ho和Y)和Hoyfeo(x = 0.1和0.3)。鉴定卤素灯功率和晶体生长气氛是最重要的参数。通过X射线衍射数据和X射线LAUE照片证明了高质量的单晶。通过降低稀土离子和Fe的RFEO中的温度和现场诱导的磁相转变的磁性转变可以通过低温磁化和特定的热测量来表征稀土离子和Fe的磁相转变。此外,我们报告了这些矫正单晶的低温热传输测量,以探测磁性,并发现它们显示出强大的磁场依赖性。特征领域与磁结构的一些变换具有良好的对应关系。这些特殊行为展示了Fe和R旋转结构的磁场诱导的转变。

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