Room-temperature spin reorientation transition and low-temperature significant magnetothermal effect in Mn-doped DyFeO3 single crystals

被引:3
作者
Yang, Wanting [1 ,2 ]
Chen, Haiyang [3 ]
Shi, Chenfei [1 ,2 ]
Song, Huan [1 ,2 ]
Sun, Zhiqiang [1 ,2 ]
Xu, Xiaofan [4 ]
Yang, Jinhu [4 ]
Kang, Baojuan [1 ,2 ]
Feng, Zhenjie [1 ,2 ]
Jia, Rongrong [1 ,2 ,5 ]
Cao, Shixun [1 ,2 ,5 ]
机构
[1] Shanghai Univ, Mat Genome Inst, Dept Phys, Shanghai 200444, Peoples R China
[2] Shanghai Univ, Int Ctr Quantum & Mol Struct, Shanghai 200444, Peoples R China
[3] Shanghai Jiao Tong Univ, Sch Phys & Astron, Key Lab Artificial Struct & Quantum Control, Minist Educ, Shanghai 200240, Peoples R China
[4] Hangzhou Normal Univ, Dept Phys, Hangzhou 310036, Peoples R China
[5] Shanghai Univ, Shanghai Key Lab High Temp Supercond, Shanghai 200444, Peoples R China
基金
中国国家自然科学基金;
关键词
Rare earth orthoferrites; Spin reorientation; Magnetic phase transition; Magnetothermal effect; Adiabatic temperature change;
D O I
10.1016/j.ceramint.2024.01.132
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
Rare-earth orthoferrites (RFeO3) promise in spin storage and spin sensing, but the majority of the magnetic phase transition and intriguing properties occur at low temperatures. Searching for higher-temperature or even roomtemperature spintronics devices has been a critical challenge in the development of spintronics. We doped Mn ions into Fe sites of DyFeO3 in 10%-50 % ratios to coexist antiferromagnetic and ferromagnetic coupling in the ab plane and elevate their spin reorientation transition (SRT) temperatures. The structural, magnetic, and magnetothermal properties of the Mn-doped DyFeO3 single-crystal system are investigated. With increasing doping ratio, the Ne ' el temperature progressively falls, while the SRT temperature (TSR) continuously rises to the room temperature of 307 K with a 40 % doping ratio, making it promising for room-temperature spin storage devices. When the ratio reaches 50 % (half doping), the magnetic configuration of Dy sublattices changes and a significant magnetothermal effect is observed. Because of low-field metamagnetic phase transition, the magnetic entropy change along the c-axis approaches 10.41 J/kg & sdot;K for the half doping crystal at 5 K (0 J/kg & sdot;K for DyFeO3, 0.93 J/kg & sdot;K for orthorhombic DyMnO3). The large adiabatic temperature change contributed by magnon indicates the exceptional refrigeration efficiency in a direct way. Therefore, it is possible to convert DyFeO3 into a room-temperature spin storage device material or a magnetic refrigeration contender at low temperatures.
引用
收藏
页码:12279 / 12286
页数:8
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