Plokhikh Igor V, Tsirlin Alexander A, Khalyavin Dmitry D, Fischer Henry E, Shevelkov Andrei V, Pfitzner Arno
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.
Phys Chem Chem Phys. 2023 Feb 8;25(6):4862-4871. doi: 10.1039/d2cp04863a.
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.
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。