Export citation

Export citation

Choose format for download:

Download Citation

    Field-induced magnetization plateau and high-field phase diagram of the multiferroic manganite ErMn2O5: An analogy to YMn2O5

    Yinfa Feng1, Haowen Wang1,*, Shuhan Zheng2, Meifeng Liu2,3, Leili Tan2, Chao Dong1, Chengliang Lu1, and Junfeng Wang1

    • *Contact author: wanghaowen1@hust.edu.cn

    Phys. Rev. B 112, 094450 – Published 25 September, 2025

    DOI: https://doi.org/10.1103/16xl-dntg

    Abstract

    The complex magnetoelectric (ME) features of the multiferroic manganites RMn2O5 (R: rare earth elements, Bi) are of particular interest due to their giving rise to some fascinating phenomena such as topological ME behaviors. Here we systematically report the magnetic and electric properties of orthorhombic ErMn2O5 single crystals under DC and pulsed magnetic fields. Based on the anomalies in the experimental data along three crystalline axes, the magnetic field-temperature (H-T) phase diagram of ErMn2O5 is well established and reveals a significant anisotropy. In the case of H//a, at 1.6 K, two magnetic transitions occur at Hc1∼12 T and Hc2∼30 T, corresponding to the reversal and saturation of ferroelectric polarizations, respectively. As the temperature increases, Hc1 slowly shifts towards lower magnetic fields and eventually becomes vague above 10 K. In contrast, Hc2 is insensitive to temperature and remains robust up to 40 K. As a result, two field-induced ME phases are clearly identified above 10 T. For H//b, the low-temperature modulated incommensurate phase with weak ferroelectricity (ICM2/X) is gradually suppressed with increasing H, and finally replaced by the commensurate phase with a large polarization (CM/FE1) above 20 T. When the magnetic field is applied along the easy c axis, 1/2- and 3/4-like magnetization plateaus induced by Er3+ spins are observed below 5 K, which were not accessed earlier. The corresponding ferroelectric anomalies are triggered by the 4f−3d interaction between the Er and Mn ions, reflecting the rearrangement of the manganese subsystem. Hence, the successive ME phase transitions are well demonstrated in the low-H region, i.e., ICM2/X → CM/FE1 → ICM3/X′. Intriguingly, the CM/FE1 phase reappears instead of the ICM3/X′ phase above 50 T at low temperatures. Possible origins for all ME phases and magnetization plateaus are discussed. These findings could contribute to an in-depth understanding for the effect of rare earth ions in this family of RMn2O5.

    Physics Subject Headings (PhySH)

    Authorization Required

    We need you to provide your credentials before accessing this content.

    Supplemental Material (Subscription Required)

    References (Subscription Required)

    Outline

    Information

    Sign In to Your Journals Account

    Filter

    Filter

    Article Lookup

    Enter a citation