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Oxygen vacancy ordering and magnetism in the rare earth stabilised perovskite form of 'SrCoO_(3-δ)'

机译:稀土稳定钙钛矿形式“ SrCoO_(3-δ)”的氧空位排序和磁性

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We have demonstrated that SrCoO_(3-δ) can be stabilised into phase pure perovskite forms by the introduction of small amounts ~5% of certain rare earth ions (Sm~(3+)-Yb~(3+)). At the same doping levels, La~(3+) and Pr~(3+) crystallise with the same isostructural trigonal structure as Sr_6Co_5O_(15); while the Nd~(3+) composition shows a mixture of both structure types. Powder X-ray diffraction showed only a simple cubic perovskite structure, however, a combination of electron and neutron diffraction has revealed a tetragonal (P4/mmm) a_p×a_p×2a_p superstructure. Strontium and the rare earth ions are disordered over a single site, while the oxygen vacancies are localised on the apical O_2 sites. Magnetisation measurements show that these materials undergo transitions to a spin-glass state at temperatures below 150 K, and that significant coupling occurs between the rare earth ions and the mixed Co~(3+/4+) ions. Magnetisation measurements as a function of applied field reveals that below the transition temperature ferromagnetic ordering takes place at relatively large fields.
机译:我们已经证明,通过引入少量〜5%的某些稀土离子(Sm〜(3 +)-Yb〜(3+)),可以将SrCoO_(3-δ)稳定为纯钙钛矿形式。在相同的掺杂水平下,La〜(3+)和Pr〜(3+)以与Sr_6Co_5O_(15)相同的等构三角形结构结晶;而Nd〜(3+)组成则显示两种结构类型的混合。粉末X射线衍射仅显示简单的立方钙钛矿结构,但是,电子和中子衍射的组合显示出四方(P4 / mm)a_p×a_p×2a_p超结构。锶和稀土离子在单个位点上无序,而氧空位位于顶端的O_2位点。磁化测量表明,这些材料在低于150 K的温度下会转变为自旋玻璃态,并且稀土离子与Co〜(3 + / 4 +)混合离子之间发生了显着耦合。根据施加磁场的磁化测量表明,在转变温度以下,铁磁有序发生在相对较大的磁场中。

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