论文标题
稀土和过渡金属钙钛矿类型高熵氧化物的磁性特性
Magnetic properties of rare earth and transition metal based perovskite type high entropy oxides
论文作者
论文摘要
高熵氧化物(HEO)是最近引入的一类氧化物材料,其特征是大量元素(即五个或更多)共享一个在单相结构中结晶的晶格位点。相当年轻的HEO家族的一个复杂例子是稀土过渡金属钙钛矿高熵氧化物。在这项综合研究中,我们提供了三种钙钛矿型高熵氧化物的磁性概述。这些化合物具有一个稀土位点,该位点由五个不同的稀土元素占据,而过渡金属位置则被单个过渡金属占据。通过这种方式,可以将与父二元氧化物(即正核核氧化物, - 冰淇淋和 - 有限岩)进行比较。 X射线吸收在边缘光谱(XANES),磁力测定法和Mössbauer光谱法被用于表征这些复杂材料。 通常,尽管稀土位点上的化学障碍,但我们发现与二元氧化物的磁性特性令人惊讶。但是,还观察到明显的差异和有趣的磁性特性,例如非共线性,自旋重新定位跃迁以及在环境温度下的大型强制性磁场。 RE A位置上的化学障碍和B位置上TM的性质在这些高熵氧化物的物理特性中都起着重要作用。
High entropy oxides (HEO) are a recently introduced class of oxide materials, which are characterized by a large number of elements (i.e. five or more) sharing one lattice site which crystallize in a single phase structure. One complex example of the rather young HEO family are the rare-earth transition metal perovskite high entropy oxides. In this comprehensive study, we provide an overview over the magnetic properties of three perovskite type high entropy oxides. The compounds have a rare-earth site which is occupied by five different rare-earth elements, while the transition metal site is occupied by a single transition metal. In this way a comparison to the parent binary oxides, namely the orthocobaltites, -chromites and -ferrites is possible. X-ray absorption near edge spectroscopy (XANES), magnetometry and Mössbauer spectroscopy are employed to characterize these complex materials. In general, we find surprising similarities to the magnetic properties of the binary oxides, despite the chemical disorder on the rare-earth site. However distinct differences and interesting magnetic properties are also observed such as noncollinearity, spin reorientation transitions as well as large coercive fields of up to 2\,T at ambient temperature. Both the chemical disorder on the RE A-site, and the nature of the TM on the B-site play an important role in the physical properties of these high entropy oxides.