arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1104.4575cond-mat.supr-con
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斜方晶系铁磷属化合物中电子-晶格耦合引起的轨道密度波

Orbital density wave induced by electron-lattice coupling in orthorhombic iron pnictides

Da-Yong Liu, Ya-Min Quan, Dong-Meng Chen, Liang-Jian Zou, Hai-Qing Lin

摘要:

本文基于二轨道和五轨道哈伯德模型,研究了铁磷属元素的四方-正交结构相变的磁性和轨道性质。与电子相互作用相互作用的电子-晶格耦合被自洽地处理。我们的研究结果表明,轨道极化稳定的自旋密度波(SDW)秩序在四相和正交相。然而,铁轨道密度波(F-ODW)只发生在正交相,而不是在四氢呋喃酮。在实际五轨道模型中,对于条纹状反铁磁相,Fe的磁矩在中间库仑相互作用区较小。SDW/ODW正交相的各向异性费米面与最近的角分辨光电子能谱实验结果一致。这些结果表明,磁相变驱动的ODW秩序主要产生于电子晶格耦合。

英文摘要:

In this paper we explore the magnetic and orbital properties closely related to a tetragonal-orthorhombic structural phase transition in iron pnictides based on both two- and five-orbital Hubbard models. The electron-lattice coupling, which interplays with electronic interaction, is self-consistently treated. Our results reveal that the orbital polarization stabilizes the spin density wave (SDW) order in both tetragonal and orthorhombic phases. However, the ferro-orbital density wave (F-ODW) only occurs in the orthorhombic phase rather than in the tetragonal one. Magnetic moments of Fe are small in the intermediate Coulomb interaction region for the striped antiferromangnetic phase in the realistic five orbital model. The anisotropic Fermi surface in the SDW/ODW orthorhombic phase is well in agreement with the recent angle-resolved photoemission spectroscopy experiments. These results suggest a scenario that the magnetic phase transition is driven by the ODW order mainly arising from the electron-lattice coupling.

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