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Giant Anisotropic Magnetocaloric Effect in Double-perovskite Gd2CoMnO6 Single Crystals

机译:双钙钛矿Gd2CoMnO6单晶的巨大各向异性磁热效应

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摘要

The magnetocaloric effect (MCE) is described by the change in temperature of a material by magnetic field variation and is a crucial subject in magnetism; it is motivated by the desire to enhance energy-efficient magnetic refrigeration for clean technology. Despite the recent discovery of the giant cryogenic MCE in double perovskites, the role of magnetic anisotropy has not yet been clearly discussed, because of the averaging effect of polycrystalline samples. Here, we investigated the anisotropic MCE in the single-crystal double perovskite Gd2CoMnO6. In addition to the ferromagnetic order of the Co2+ and Mn4+ moments, the large Gd3+ moments align below T Gd = 21 K, exhibiting an isotropic nature. Because of the intricate temperature development of magnetically hysteretic behaviour and metamagnetism, the change in magnetic entropy along the c-axis appears to be relatively small. On the contrary, the smaller but almost reversible magnetization perpendicular to the c-axis leads to a large MCE with a maximum entropy change of 25.4 J/kg·K. The anisotropic MCE generates a giant rotational MCE, estimated as 16.6 J/kg·K. Our results demonstrate the importance of magnetic anisotropy for understanding the MCE and reveal essential clues for exploring suitable magnetic refrigerant compounds aiming at magnetic functional applications.
机译:磁热效应(MCE)由磁场变化引起的材料温度变化来描述,是磁学中的关键学科。其动机是希望提高清洁技术的节能磁制冷能力。尽管最近在双钙钛矿中发现了巨大的低温MCE,但由于多晶样品的平均作用,磁各向异性的作用尚未得到明确讨论。在这里,我们研究了单晶双钙钛矿Gd2CoMnO6中的各向异性MCE。除了Co 2 + 和Mn 4 + 的铁磁阶外,大的Gd 3 + 矩在T Gd = 21以下对齐。 K,表现出各向同性的性质。由于磁滞行为和超磁性的复杂温度发展,沿c轴的磁熵变化似乎相对较小。相反,垂直于c轴的较小但几乎可逆的磁化强度导致MCE较大,最大熵变为25.4 J / kg·K。各向异性的MCE产生一个巨大的旋转MCE,估计为16.6 J / kg·K。我们的结果证明了磁各向异性对于理解MCE的重要性,并揭示了探索针对磁功能应用的合适磁制冷剂化合物的基本线索。

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