Division of Materials Physics, Graduate School of Engineering Science, Osaka University, Toyonaka, Osaka 560-8531, Japan.
Condensed Matter Research Center, Institute of Materials Structure Science, High Energy Accelerator Research Organization, Tsukuba 305-0801, Japan.
Nat Commun. 2017 Jun 5;8:15457. doi: 10.1038/ncomms15457.
Despite remarkable progress in developing multifunctional materials, spin-driven ferroelectrics featuring both spontaneous magnetization and electric polarization are still rare. Among such ferromagnetic ferroelectrics are conical spin spiral magnets with a simultaneous reversal of magnetization and electric polarization that is still little understood. Such materials can feature various multiferroic domains that complicates their study. Here we study the multiferroic domains in ferromagnetic ferroelectric MnGeO using neutron diffraction, and show that it features a double-Q conical magnetic structure that, apart from trivial 180 commensurate magnetic domains, can be described by ferromagnetic and ferroelectric domains only. We show unconventional magnetoelectric couplings such as the magnetic-field-driven reversal of ferroelectric polarization with no change of spin-helicity, and present a phenomenological theory that successfully explains the magnetoelectric coupling. Our measurements establish MnGeO as a conceptually simple multiferroic in which the magnetic-field-driven flop of conical spin spirals leads to the simultaneous reversal of magnetization and electric polarization.
尽管在开发多功能材料方面取得了显著进展,但同时具有自发磁化和电极化的自旋驱动铁电体仍然很少见。在这些铁磁铁电体中,存在锥形自旋螺旋磁体,其磁化和极化同时反转,这仍然知之甚少。这些材料可以具有各种多铁畴,这使得它们的研究变得复杂。在这里,我们使用中子衍射研究了铁磁铁电体 MnGeO 中的多铁畴,并表明它具有双 Q 锥形磁结构,除了平凡的 180 度准同型磁畴外,它只能由铁磁畴和铁电畴来描述。我们展示了非传统的磁电耦合,例如铁电极化的磁场驱动反转而自旋螺旋度没有变化,并提出了一个成功解释磁电耦合的唯象理论。我们的测量结果确立了 MnGeO 作为一个概念简单的多铁体,其中锥形自旋螺旋的磁场驱动翻转导致磁化和极化的同时反转。