Local A-Site Layering in Rare-Earth Orthochromite Perovskites by Solution Synthesis

被引:16
|
作者
Daniels, Luke M. [1 ]
Kashtiban, Reza J. [2 ]
Kepaptsoglou, Demie [3 ]
Ramasse, Quentin M. [3 ]
Sloan, Jeremy [2 ]
Walton, Richard I. [1 ]
机构
[1] Univ Warwick, Dept Chem, Coventry CV4 7AL, W Midlands, England
[2] Univ Warwick, Dept Phys, Coventry CV4 7AL, W Midlands, England
[3] SciTech Daresbury Campus, SuperSTEM Lab, Daresbury WA4 4AD, England
基金
英国工程与自然科学研究理事会;
关键词
chromites; electron energy loss spectroscopy (EELS); hydrothermal synthesis; magnetism; perovskites; HYDROTHERMAL SYNTHESIS; INTERCONNECT MATERIAL; POWDER DIFFRACTION; PHASE-TRANSITIONS; MULTIFERROICS; CHROMITES; OXIDES; POLARIZATION; MANGANITES;
D O I
10.1002/chem.201604766
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Cation size effects were examined in the mixed A-site perovskites La0.5Sm0.5CrO3 and La0.5Tb0.5CrO3 prepared through both hydrothermal and solid-state methods. Atomically resolved electron energy loss spectroscopy (EELS) in the transmission electron microscope shows that while the La and Sm cations are randomly distributed, increased cation-radius variance in La0.5Tb0.5CrO3 results in regions of localised La and Tb layers, an atomic arrangement exclusive to the hydrothermally prepared material. Solid-state preparation gives lower homogeneity resulting in separate nanoscale regions rich in La3+ and Tb3+. The A-site layering in hydrothermal La0.5Tb0.5CrO3 is randomised upon annealing at high temperature, resulting in magnetic behaviour that is dependent on synthesis route.
引用
收藏
页码:18362 / 18367
页数:6
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