Half-Metallicity and Magnetic Anisotropy in Double-Perovskite GdBaCo2O6 Films Prepared via Topotactic Oxidation

铁磁性 凝聚态物理 反铁磁性 磁化 居里温度 材料科学 钙钛矿(结构) 磁电阻 钴酸盐 磁各向异性 结晶学 化学 磁场 物理 量子力学 冶金
作者
Tsukasa Katayama,Shishin Mo,Akira Chikamatsu,Yuji Kurauchi,Hiroshi Kumigashira,Tetsuya Hasegawa
出处
期刊:Chemistry of Materials [American Chemical Society]
卷期号:35 (3): 1295-1300 被引量:7
标识
DOI:10.1021/acs.chemmater.2c03335
摘要

Double-perovskite GdBaCo2Ox is a promising material owing to its fascinating electronic and magnetic features, such as spin crossover, charge and spin-state ordering, magnetic-field or photo-induced antiferromagnetic-to-ferromagnetic phase transition, and large magnetoresistance (MR). These properties can be controlled by changing the oxygen content (x), and an increase of x is effective for stabilizing ferromagnetic order. However, a stoichiometric phase (x = 6) has not yet been obtained because the distorted coordination geometry prefers oxygen vacancies. In this study, we report the successful synthesis of GdBaCo2O6 epitaxial films via the topotactic oxidation of a film with x = 5.5. The transformation between x = 5.5 and 6 phases was reversible via low-temperature redox reactions. The x = 6 film exhibited ferromagnetic and metallic behavior below the Curie temperature (TC) of 110 K and semiconducting behavior above TC. The spontaneous magnetization of the x = 6 film was 4.8 μB/f.u., which is the largest in the double-perovskite cobaltite system owing to the ferromagnetic interaction between Co3.5+ and Gd3+. It also exhibited strong magnetic anisotropy along the a axis (1.7 × 107 erg/cm3) and anisotropic MR behavior associated with the Gd/Ba ordering along the c axis. Furthermore, theoretical calculations predicted that the half-metallicity of the x = 6 film originates from the double exchange interaction between intermediate-spin Co3+ and low-spin Co4+.

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