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    Ferroelectric control of magnetism, valley polarization, and skyrmions in monolayer TcIrGe2Se6

    Ruixiao Ma1, Zhangtong Ying1, Zirui Zhang1, Qiuyao Zhang1, Xinyuan Guan1, Shiwei Zhu1, Xiaoping Wu1,2, and Changsheng Song1,2,*

    • 1Department of Physics and Zhejiang Key Laboratory of Quantum State Control and Optical Field Manipulation, Zhejiang Sci-Tech University, Hangzhou 310018, China
    • 2Zhejiang-Mexico Joint Laboratory of Intelligent Optoelectronic Sensing, Zhejiang Sci-Tech University, Hangzhou 310018, China

    • *Contact author: cssong@zstu.edu.cn

    Phys. Rev. B 114, 194402 – Published 5 October, 2026

    DOI: https://doi.org/10.1103/9ctp-k5h4

    Abstract

    Two-dimensional (2D) triferroic materials, which simultaneously host ferroelectric, ferromagnetic, and ferrovalley orders, are regarded as ideal platforms for developing next-generation nonvolatile multistate memory devices. However, achieving coupling among these order parameters, stability above room temperature, and their coexistence with higher-order topology in an intrinsic monolayer remains challenging. Based on first-principles calculations, we predict that monolayer TcIrGe2Se6 (TIGS) is an intrinsic 2D triferroic semiconductor stable above room temperature. Specifically, this system possesses switchable out-of-plane ferroelectric polarization and polarization-controllable valley polarization, together with a ferromagnetic ground state stabilized by the supersuperexchange mechanism, with a Curie temperature reaching 405 K. More importantly, pronounced coupling among ferroelectric order, magnetic order, and valley physics is found in TIGS. As a result, polarization reversal modulates the magnetic interactions, reverses both the sign of the valley splitting and the DMI chirality, and modulates Berry-curvature-related transport responses. In addition, TIGS exhibits higher-order topological characteristics and supports a long-range-ordered skyrmion lattice. These results identify TIGS as a promising platform for exploring the cooperative interplay among 2D multiferroic coupling, higher-order topology, spin textures, and valley physics.

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