Wang Weipeng, Shen Xi, Wang Wei, Guan Xiangxiang, Yao Yuan, Wang Yanguo, Yu Richeng
Beijing National Laboratory of Condensed Matter Physics, Institute of Physics, Chinese Academy of Sciences , Beijing 100190, P. R. China.
School of Physical Sciences, University of Chinese Academy of Sciences , Beijing 100049, P. R. China.
Inorg Chem. 2017 Mar 20;56(6):3207-3213. doi: 10.1021/acs.inorgchem.6b02347. Epub 2017 Mar 1.
One of the core issues for the A/B site doping in the bismuth layer magnetoelectric materials is to find out the evolution of the magnetic structure, crystal structure and elemental distribution, and the coupling effects between spin and lattice with the increase of ion substitution. Here, we have conducted systematic structural and physical property studies on the series samples of BiTiFeCoO. This work presents that BiTiFeCoO forms a single four layer perovskite-like structure for 0 ≤ x < 0.67, while a three layer perovskite-like structure block begins to arise for x ≥ 0.67. With different cobalt content, the sample demonstrates antiferromagnetism, spin state determined magnetism, or magnetic anisotropy determined magnetism. The weak ferromagnetism is considered to be induced by the larger displacement of Co ions from the center of octahedra and the change of the spin state of Co ions. It is also observed that Fe and Co elements are homogeneously substituted in the three layer structure block, accompanied by the rotation (and/or distortion) of BO octahedra.
铋层状磁电材料中A/B位掺杂的核心问题之一是弄清楚随着离子取代的增加,磁结构、晶体结构和元素分布的演变,以及自旋与晶格之间的耦合效应。在此,我们对BiTiFeCoO系列样品进行了系统的结构和物理性质研究。这项工作表明,对于0≤x<0.67,BiTiFeCoO形成单一的四层钙钛矿-like结构,而对于x≥0.67,开始出现三层钙钛矿-like结构块。随着钴含量的不同,样品表现出反铁磁性、自旋态决定的磁性或磁各向异性决定的磁性。弱铁磁性被认为是由Co离子从八面体中心的较大位移和Co离子自旋态的变化所诱导的。还观察到Fe和Co元素在三层结构块中均匀取代,同时伴随着BO八面体的旋转(和/或畸变)。