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arXiv 2601.09092cond-mat.mtrl-sci
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在强磁场下GdMnO3中发现意外的II型多铁相

Unexpected type-II multiferroic phase in GdMnO3 under high magnetic fields

Huazhong University of Science and Technology(华中科技大学);Southeast University(东南大学);Chinese Academy of Sciences(中国科学院);University of Texas at Austin(德克萨斯大学奥斯汀分校)

Ming Yang, Jun Chen, Junfeng Wang, Chao Dong, Chengliang Lu, Gang Xu, Jinguang Cheng, Jianshi Zhou, Shuai Dong

AI总结:

在强磁场下,GdMnO3中发现了一种新的II型多铁相,其磁性诱导极化高达1500μC/m²,通过多探针实验和模型模拟揭示了非单调的相变行为。

摘要:

钙钛矿锰氧化物,具有小A位离子,作为II型多铁材料的第一和经典分支,是展现磁性诱导铁电性的理想系统。尽管其在低磁场下的磁电相图已建立,但在此研究中,在高达60T的强磁场下,GdMnO3中发现了一种未识别的相,具有较大的磁性诱导极化(最高达1500μC/m²)。基于多探针实验,构建了完整的相图,呈现出依次极性-非极性-极性-非极性的转变。这种非单调的演变可通过模型模拟很好地模拟,而自旋-晶格耦合是重新进入的铁电相的关键因素。

英文摘要:

Perovskite manganites with small A-site ions, as the first and canonical branch of type-II multiferroics, are ideal systems to exhibit magnetism-induced ferroelectricity. Despite their established magnetoelectric phase diagrams under low magnetic fields, here an unidentified phase with a large magnetism-induced polarization (up to 1500 μC/m2) is revealed in GdMnO3 under high magnetic fields up to 60 T. Based on multiprobe experiments, a complete phase diagram is constructed with successive polar-nonpolar-polar-nonpolar transitions. Such a nonmonotonic evolution is well mimicked by model simulation, while the spin-lattice coupling is the key ingredient for the reentrant ferroelectric phase.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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