Competition Between Multiferroic and Magnetic Soliton Lattice States in DyFeO
arXiv:2502.11592 · doi:10.1103/kwrl-x4hw
Abstract
Simultaneous breaking of time reversal and inversion symmetries in multiferroics couples ferroelectricity to magnetism and is a source of unusual physical phenomena that can be used in next-generation electronic devices. A notable example is DyFeO, which under applied magnetic fields exhibits a giant linear magnetoelectric response and a large spontaneous electric polarization induced by coexisting orders of Fe and Dy spins. Here, we use high-resolution neutron diffraction to show that at zero field DyFeO hosts an incommensurate magnetic soliton lattice formed by spatially ordered Dy domain walls with an average domain size of 231(8) Å. The long-ranged interaction between the domain walls is mediated by magnons propagating through the Fe subsystem and is analogous to the Yukawa force in particle physics. An applied magnetic field destroys the long-ranged incommensurate order, unlocks the linear magnetoelectric response and stabilizes the ferroelectric state. The magnetic domain walls are electrically charged and the soliton array dimerizes when both electric and magnetic fields are applied. Numerical simulations with experimental parameters suggest, that the generic competition between the ferroelectric and incommensurate states can be effectively controlled by an applied electric field.
References in corpus (6)
- Tomonaga-Luttinger Liquid Behavior and Spinon Confinement in YbAlO
- Ground state and magnetic phase transitions of orthoferrite DyFeO_3
- Magnetic ground state of the Ising-like antiferromagnet DyScO
- Role of Dy on the magnetic properties of orthorhombic DyFeO3
- Low-energy spin dynamics in rare-earth perovskite oxides
- Slow spin dynamics and quantum tunneling of magnetization in the dipolar antiferromagnet DyScO