磁制冷
反铁磁性
凝聚态物理
材料科学
稀土
磁化
自旋电子学
自旋(空气动力学)
磁场
铁磁性
热力学
物理
冶金
量子力学
作者
Canglong Li,S.S. Zheng,Godfrey Okumu Barasa,Yan Feng Zhao,Lei Wang,Cuiling Wang,Yang Lu,Yang Qiu,Junye Cheng,Yongsong Luo
标识
DOI:10.1016/j.ceramint.2021.09.059
摘要
The heavy rare-earth GdFeO3-type RFeO3 (R = Dy, Ho and Er) orthoferrites (space group Pnma, N 62) show spin reorientation transition characterized by a turning point on the magnetization curves. The basic Arrott plots curves showing positive slopes confirm the second-order nature of the spin reorientation and the transition temperature TSR is estimated to be ∼45 K, ∼53 K and ∼94 K for DyFeO3, HoFeO3 and ErFeO3, respectively. In addition, magnetic entropy change −ΔSM of the three samples is calculated to be 11.4, 9.8 and 7.4 J kg−1 K−1 at 10 K and 50 kOe, respectively. The field sensitive antiferromagnetic state and competitive magnetocaloric performances in RFeO3 have been attracting considerable interest for the possible applications in spintronic devices.
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