铁磁性
中子衍射
化学
超级交换
磁性结构
结晶学
单斜晶系
磁矩
铁磁性
八面体
晶体结构
磁化
磁化率
结构精修
凝聚态物理
核磁共振
磁场
物理
量子力学
作者
M. Retuerto,Angel Muñoz,María Jesús Martínez-Lope,J. A. Alonso,F. J. Mompeán,María Teresa Fernández-Díaz,Javier Sánchez-Benítez
出处
期刊:Inorganic Chemistry
[American Chemical Society]
日期:2015-10-29
卷期号:54 (22): 10890-10900
被引量:72
标识
DOI:10.1021/acs.inorgchem.5b01951
摘要
R2NiMnO6 (R = Tb, Ho, Er, Tm) perovskites have been prepared by soft-chemistry techniques followed by high oxygen-pressure treatments; they have been investigated by X-ray diffraction, neutron powder diffraction (NPD), and magnetic measurements. In all cases the crystal structure is defined in the monoclinic P21/n space group, with an almost complete order between Ni(2+) and Mn(4+) cations in the octahedral perovskite sublattice. The low temperature NPD data and the macroscopic magnetic measurements indicate that all the compounds are ferrimagnetic, with a net magnetic moment different from zero and a distinct alignment of Ni and Mn spins depending on the nature of the rare-earth cation. The magnetic structures are different from the one previously reported for La2NiMnO6, with a ferromagnetic structure involving Mn(4+) and Ni(2+) moments. This spin alignment can be rationalized taking into account the Goodenough-Kanamori rules. The magnetic ordering temperature (TCM) decreases abruptly as the size of the rare earth decreases, since TCM is mainly influenced by the superexchange interaction between Ni(2+) and Mn(4+) (Ni(2+)-O-Mn(4+) angle) and this angle decreases with the rare-earth size. The rare-earth magnetic moments participate in the magnetic structures immediately below TCM.
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