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Ferromagnetism with strong magnetocrystalline anisotropy in A-site ordered perovskite YBaCo2O6 epitaxial thin films prepared via wet-chemical topotactic oxidation†
Journal of Materials Chemistry C ( IF 6.4 ) Pub Date : 2018-02-27 00:00:00 , DOI: 10.1039/c7tc05422j
Tsukasa Katayama 1, 2, 3, 4, 5 , Akira Chikamatsu 1, 2, 3, 4 , Yasushi Hirose 1, 2, 3, 4 , Makoto Minohara 4, 6, 7, 8 , Hiroshi Kumigashira 4, 6, 7, 8 , Isao Harayama 4, 9, 10, 11 , Daiichiro Sekiba 4, 9, 10, 11 , Tetsuya Hasegawa 1, 2, 3, 4
Affiliation  

A-site cation-ordered perovskite cobaltite, RBaCo2Ox (R = rare earth element), exhibits fascinating physical properties, such as spin-state ordering and high oxygen conductivity, because of the large tetragonal distortion of the Co orbital. However, the distorted coordination geometry prefers oxygen vacancies, resulting in a difficulty in obtaining the stoichiometric phase (x = 6). For example, x in YBaCo2Ox, which has largely distorted Co orbitals because of the small size of Y3+, has so far been limited to 5.52. To expand the available range of x, in this study, we performed a low-temperature topotactic oxidation of YBaCo2O5.3 epitaxial films using a strong oxidizing agent NaClO. The x value can be varied in a wide range of 5.3–6.0, maintaining the A-site cation-ordered perovskite structure, by changing the pH and temperature of NaClO. The single crystalline film with x = 6 exhibits large tetragonal distortion (c/a = 0.968) because of the small ionic radius of Y3+ and substrate-induced tensile strain. Unlike antiferromagnetic insulating YBaCo2O5.5, the fully oxidized film with x = 6 exhibits in-plane ferromagnetism and metallicity with a Curie temperature of 130 K possibly because of the double-exchange interaction between Co3+ and Co4+. Moreover, the YBaCo2O6 film exhibits huge magnetic anisotropy with a magnetic anisotropy constant of 1.5 × 108 erg cm−3, demonstrating that the A-site cation-ordered perovskite structure is promising for obtaining high magnetocrystalline anisotropic materials.

中文翻译:

通过湿化学全能氧化法制备的 A位置有序钙钛矿YBaCo 2 O 6外延薄膜中具有强磁晶各向异性的铁磁性

由于Co轨道的大四方形畸变,A位阳离子排序的钙钛矿型钴矿RBaCo 2 O x(R =稀土元素)表现出令人着迷的物理特性,例如自旋态有序性和高氧导率。然而,扭曲的配位几何形状倾向于氧空位,导致难以获得化学计量相(x= 6)。例如,X在YBaCo 2 ö X,这在很大程度上是因为扭曲Y的小尺寸的共同轨道3+,迄今被限制在5.52。为了扩大x的可用范围,在这项研究中,我们进行了YBaCo的低温全位氧化5.3外延膜中使用2 O 5.3的强氧化剂NaClO。的X值可在宽范围的5.3-6.0变化,维持A位阳离子有序钙钛矿结构中,通过改变次氯酸钠的pH和温度。x = 6的单晶膜由于Y 3+的小离子半径和基体诱导的拉伸应变而表现出较大的四方畸变( c / a = 0.968)。不同于反铁磁绝缘YBaCo 2 O 5.5,具有x的完全氧化膜= 6表现出居里温度为130 K的面内铁磁性和金属性,可能是由于Co 3+和Co 4+之间的双重交换相互作用。此外,YBaCo 2 O 6膜表现出巨大的磁各向异性,其磁各向异性常数为1.5×10 8 erg cm -3,表明A位阳离子序的钙钛矿结构有望获得高磁晶各向异性材料。
更新日期:2018-02-27
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