Song Guang, Chen Yuting, Li Guannan, Gao Benling
Department of Physics, Huaiyin Institute of Technology Huaian 223003 China.
Jiangsu Provincial Key Laboratory of Palygorskite Science and Applied Technology, Huaiyin Institute of Technology Huaian 223003 China.
RSC Adv. 2019 Jan 15;9(4):2143-2151. doi: 10.1039/c8ra08507b. eCollection 2019 Jan 14.
Perovskite ScMnO has been synthesized under high temperature and high pressure. The magnetic ordering of this compound was proposed to be in the E-AFM state in previous theoretical research. Such magnetic ordering would lead the Mn ions to be off-centered in the MnO octahedra; however, this is not detected experimentally. To address this issue, we systematically investigate the magnetic, orbital, and electric structures of perovskite ScMnO with first-principles calculations. It is found that its magnetic ground state is G-AFM and the magnetic ordering can explain the puzzle very well. Moreover, there is an unreported three-dimensional alternating cooperative orbital ordering in perovskite ScMnO. The antiferromagnetic coupling between the nearest-neighbor Mn ions is stabilized by the strong octahedral distortions that decrease the ferromagnetic interaction between the e orbitals of the Mn ions. In addition, we find that perovskite ScMnO is a bipolar antiferromagnetic semiconductor in which completely spin-polarized currents with reversible spin polarization can be tuned simply by applying a gate voltage. Such controllability of the spin polarization of the current opens up new avenues for future spintronic devices. Our results not only suggest that the G-AFM phase is the ground magnetic state for perovskite ScMnO, but also enrich research in orbital ordering in rare-earth manganites.
钙钛矿型ScMnO是在高温高压下合成的。在先前的理论研究中,该化合物的磁有序被认为处于E型反铁磁(E-AFM)状态。这种磁有序会导致Mn离子在MnO八面体中偏离中心位置;然而,实验中并未检测到这种情况。为了解决这个问题,我们用第一性原理计算系统地研究了钙钛矿型ScMnO的磁、轨道和电结构。结果发现,其磁基态为G型反铁磁(G-AFM),这种磁有序能够很好地解释这个谜团。此外,在钙钛矿型ScMnO中存在一种未被报道的三维交替协同轨道有序。最近邻Mn离子之间的反铁磁耦合通过强烈的八面体畸变得以稳定,这种畸变降低了Mn离子e轨道之间的铁磁相互作用。此外,我们发现钙钛矿型ScMnO是一种双极反铁磁半导体,在其中通过施加栅极电压就可以简单地调控具有可逆自旋极化的完全自旋极化电流。电流自旋极化的这种可控性为未来的自旋电子器件开辟了新途径。我们的结果不仅表明G-AFM相是钙钛矿型ScMnO的基态磁状态,而且丰富了稀土锰氧化物中轨道有序的研究。