Suppr超能文献

反萤石层对 Eu 基 1111 化合物 EuTAsF(T = Zn、Mn 和 Fe)中磁序的影响。

Effect of antifluorite layer on the magnetic order in Eu-based 1111 compounds, EuTAsF (T = Zn, Mn, and Fe).

作者信息

Plokhikh Igor V, Tsirlin Alexander A, Khalyavin Dmitry D, Fischer Henry E, Shevelkov Andrei V, Pfitzner Arno

机构信息

Laboratory for Multiscale Materials Experiments, Paul Scherrer Institut, PSI, Villigen, CH-5232, Switzerland.

Felix Bloch Institute for Solid-State Physics, University of Leipzig, 04103, Leipzig, Germany.

出版信息

Phys Chem Chem Phys. 2023 Feb 8;25(6):4862-4871. doi: 10.1039/d2cp04863a.

Abstract

The 1111 compounds with an alternating sequence of fluorite and antifluorite layers serve as structural hosts for the vast family of Fe-based superconductors. Here, we use neutron powder diffraction and density-functional-theory (DFT) band-structure calculations to study magnetic order of Eu in the [EuF] fluorite layers depending on the nature of the [TAs] antifluorite layer that can be non-magnetic semiconducting (T = Zn), magnetic semiconducting (T = Mn), or magnetic metallic (T = Fe). Antiferromagnetic transitions at ∼ 2.4-3 K due to an ordering of the Eu magnetic moments were confirmed in all three EuTAsF compounds. Whereas in EuTAsF (T = Zn and Mn), the commensurate = (½ ½ 0) stripe order pattern with magnetic moments within the - plane is observed, the order in EuFeAsF is incommensurate with = (0 0.961(1) ½) and represents a cycloid of Eu magnetic moments confined within the -plane. Additionally, the Mn sublattice in EuMnAsF features a robust G-type antiferromagnetic order that persists at least up to room temperature, with magnetic moments along the -direction. Although DFT calculations suggest stripe antiferromagnetic order in the Fe-sublattice of EuFeAsF as the ground state, neutron diffraction reveals no evidence of long-range magnetic order associated with Fe. We show that the frustrating interplane interaction between the adjacent [EuF] layers is comparable with in-plane - interactions already in the case of semiconducting fluorite layers [TAs] (T = Zn and Mn) and becomes dominant in the case of the metallic [FeAs] ones. The latter, along with a slight orthorhombic distortion, is proposed to be the origin of the incommensurate magnetic structure observed in EuFeAsF.

摘要

具有萤石层和反萤石层交替序列的1111化合物是大量铁基超导体家族的结构主体。在此,我们利用中子粉末衍射和密度泛函理论(DFT)能带结构计算,研究了[EuF]萤石层中Eu的磁有序,其取决于[TAs]反萤石层的性质,[TAs]反萤石层可以是非磁性半导体(T = Zn)、磁性半导体(T = Mn)或磁性金属(T = Fe)。在所有三种EuTAsF化合物中均证实了由于Eu磁矩有序化导致的约2.4 - 3 K的反铁磁转变。在EuTAsF(T = Zn和Mn)中,观察到具有 - 平面内磁矩的相称 = (½ ½ 0)条纹有序图案,而EuFeAsF中的有序是不相称的, = (0 0.961(1) ½),代表限制在 - 平面内的Eu磁矩的摆线。此外,EuMnAsF中的Mn亚晶格具有稳健的G型反铁磁有序,至少持续到室温,磁矩沿 - 方向。尽管DFT计算表明EuFeAsF的Fe亚晶格中的条纹反铁磁有序是基态,但中子衍射未发现与Fe相关的长程磁有序的证据。我们表明,相邻[EuF]层之间令人沮丧的面间相互作用在半导体萤石层[TAs](T = Zn和Mn)的情况下已经与面内 - 相互作用相当,而在金属[FeAs]层的情况下占主导地位。后者与轻微的正交畸变一起,被认为是EuFeAsF中观察到的不相称磁结构的起源。

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验