Absence of itinerant ferromagnetism in a cobalt-based oxypnictide

Hua-Xun Li, Hao Jiang, Yi-Qiang Lin, Jia-Xin Li, Shi-Jie Song, Qin-Qing Zhu, Zhi Ren, Guang-Han Cao
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Abstract

We report a layered transition-metal-ordered oxypnictide Sr$_{2}$CrCoAsO$_{3}$. The new material was synthesized by solid-state reactions under vacuum. It has an intergrowth structure with a perovskite-like Sr$_3$Cr$_2$O$_6$ unit and ThCr$_2$Si$_2$-type SrCo$_2$As$_2$ block stacking coherently along the crystallographic $c$ axis. The measurements of electrical resistivity, magnetic susceptibility, and specific heat indicate metallic conductivity from the CoAs layers and short-range antiferromagnetic ordering in the CrO$_{2}$ planes. No itinerant-electron ferromagnetism expected in CoAs layers is observed. This result, combined with the first-principles calculations and the previous reports of other CoAs-layer-based materials, suggests that the Co$-$Co bondlength plays a crucial role in the emergence of itinerant ferromagnetism.
钴基氧化物中不存在巡回铁磁性
我们报告了一种层状过渡金属有序氧化锑Sr$_{2}$CrCoAsO$_{3}$。这种新材料是在真空条件下通过固态反应合成的。它具有一种互生结构,其中有类似于透辉石的 Sr$_3$Cr$_2$O$_6$ 单元和 ThCr$_2$Si$_2$ 型 SrCo$_2$As$_2$ 嵌段沿晶体学 $c$ 轴连续堆叠。电电阻率、磁感应强度和比热的测量结果表明,CoAs 层具有金属导电性,CrO$_{2}$ 面具有短程反铁磁有序性。在 CoAs 层中没有观察到预期的巡回电子铁磁性。这一结果与第一性原理计算结果以及以前关于其他 CoAs 层基材料的报道相结合,表明 Co$-$Co 键长度在铁磁性的出现中起着关键作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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