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一系列具有三角磁晶格的 Glaserite 体系中的磁基态交叉。

Magnetic Ground State Crossover in a Series of Glaserite Systems with Triangular Magnetic Lattices.

机构信息

Department of Chemistry and Center for Optical Materials Science and Engineering Technologies (COMSET) , Clemson University , Clemson , South Carolina 29634-0973 , United States.

出版信息

Inorg Chem. 2019 Feb 18;58(4):2813-2821. doi: 10.1021/acs.inorgchem.8b03418. Epub 2019 Feb 7.

DOI:10.1021/acs.inorgchem.8b03418
PMID:30730713
Abstract

The magnetic properties are reported for three members of the glaserite series of compounds, NaBaM(VO), M = Mn, MnCo, and Co. Large single crystals are grown using a high-temperature hydrothermal synthesis method. This structure type exhibits a triangular magnetic lattice in which MO octahedra are interconnected with nonmagnetic (VO) groups. All the structures crystallize at room temperature with rigid trigonal symmetry (space group P3̅ m1); however, at lower temperatures both NaBaMn(VO) and NaBaMnCo(VO) undergo a structural transition to lower symmetry (monoclinic, C2/ c). The bulk magnetic measurements indicate that Mn- and Co-structures are antiferromagnetic and ferromagnetic, respectively. NaBaMnCo(VO) does not show any long-range ordering down to 0.5 K, although a broad heat capacity anomaly near 1.2 K suggests short-range magnetic order or freezing into a spin-glass-like state related to the chemical disorder and resulting competing magnetic interactions. The magnetic structures of NaBaMn(VO) and NaBaCo(VO) were determined using neutron powder diffraction. At zero magnetic field, NaBaMn(VO) possesses an antiferromagnetic structure with the moments ordered in a Néel-type arrangement and aligned along the C axis of the octahedra. Under applied magnetic field at 0.3 K, the evolution of the magnetic structure toward a fully polarized state is observed. NaBaCo(VO) represents a ferromagnetic (FM) magnetic structure with Co moments aligned parallel to the c-axis direction. The relationships between these structures and magnetic properties are discussed.

摘要

报道了 Glaserite 系列化合物的三个成员 NaBaM(VO)(M=Mn、MnCo 和 Co)的磁性。使用高温水热合成方法生长出大单晶。该结构类型表现出三角形磁晶格,其中 MO 八面体与非磁性(VO)基团相连。所有结构在室温下均以刚性三角对称(空间群 P3̅ m1)结晶;然而,在较低温度下,NaBaMn(VO)和 NaBaMnCo(VO)都经历了结构向低对称性(单斜,C2/ c)的转变。体磁测量表明 Mn-和 Co-结构分别为反铁磁和铁磁。NaBaMnCo(VO) 即使在 0.5 K 以下也没有显示出任何长程有序,尽管在 1.2 K 附近的宽热容异常表明存在短程磁有序或冻结成与化学无序和竞争磁相互作用有关的自旋玻璃状状态。使用中子粉末衍射确定了 NaBaMn(VO)和 NaBaCo(VO)的磁结构。在零磁场下,NaBaMn(VO)具有反铁磁结构,其中磁矩按奈尔型排列并沿八面体的 C 轴取向。在 0.3 K 的外加磁场下,观察到磁结构向完全极化状态的演化。NaBaCo(VO)代表具有平行于 c 轴方向的 Co 磁矩的铁磁(FM)磁结构。讨论了这些结构与磁性质之间的关系。

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