一种钴基氧磷族化合物中巡游铁磁性的缺失
Absence of itinerant ferromagnetism in a cobalt-based oxypnictide
AI总结:
研究合成并表征层状 Sr₂CrCoAsO₃,发现其 CoAs 层未出现预期的巡游铁磁性,并结合计算与既有材料结果指出 Co−Co 键长是关键因素。
摘要:
我们报道了一种层状过渡金属有序氧磷族化合物 Sr₂CrCoAsO₃。该新材料通过真空条件下的固相反应合成。它具有共生结构,类钙钛矿 Sr₃Cr₂O₆ 单元与 ThCr₂Si₂ 型 SrCo₂As₂ 区块沿晶体学 c 轴共格堆叠。电阻率、磁化率和比热测量表明,CoAs 层具有金属导电性,而 CrO₂ 面内存在短程反铁磁有序。研究未观察到 CoAs 层中预期的巡游电子铁磁性。结合第一性原理计算以及此前关于其他基于 CoAs 层材料的报道,该结果表明 Co−Co 键长在巡游铁磁性的出现中起着关键作用。
英文摘要:
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.
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