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Infinite-layer iron oxide with a square-planar coordination

机译:方平面配位的无限层氧化铁

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摘要

Conventional high-temperature reactions limit the control of coordination polyhedra in transition-metal oxides to those obtainable within the bounds of known coordination geometries for a given transition metal. For example, iron atoms are almost exclusively coordinated by three-dimensional polyhedra such as tetrahedra and octahedra. However, recent works have shown that binary metal hydrides act as reducing agents at low temperatures, allowing access to unprecedented structures. Here we show the reaction of a perovskite SrFeO_3 with CaH_2 to yield SrFeO_2, a new compound bearing a square-planar oxygen coordination around Fe~(2+). SrFeO_2 is isostructural with 'infinite layer' cupric oxides, and exhibits a magnetic order far above room temperature in spite of the two-dimensional structure, indicating strong in-layer magnetic interactions due to strong Fe d to O p hybridization. Surprisingly, SrFeO_2 remains free from the structural instability that might well be expected at low temperatures owing to twofold orbital degeneracy in the Fe~(2+) ground state with D_(4h) point symmetry. The reduction and the oxidation between SrFeO_2 and SrFeO_3 proceed via the brownmillerite-type intermediate SrFeO_(2.5), and start at the relatively low temperature of ~400 K, making, the material appealing for a variety of applications, including oxygen ion conduction, oxygen gas absorption and catalysis.
机译:常规的高温反应将过渡金属氧化物中配位多面体的控制限制在给定过渡金属的已知配位几何范围内可获得的配位多面体。例如,铁原子几乎完全由三维多面体(例如四面体和八面体)配位。但是,最近的研究表明,二元金属氢化物在低温下起还原剂的作用,允许进入前所未有的结构。在这里,我们显示了钙钛矿SrFeO_3与CaH_2的反应生成SrFeO_2,这是一种在Fe〜(2+)周围带有方形氧配位的新化合物。 SrFeO_2是具有“无限层”氧化铜的同构结构,尽管具有二维结构,但仍显示出远高于室温的磁序,这表明由于Fe d与O p的强杂交而引起的强层内磁相互作用。出人意料的是,由于在具有D_(4h)点对称性的Fe〜(2+)基态中的两倍轨道简并性,SrFeO_2仍然没有在低温下可能发生的结构不稳定性。 SrFeO_2和SrFeO_3之间的还原和氧化过程是通过褐闪石型中间体SrFeO_(2.5)进行的,起始温度为约400 K的较低温度,使得该材料吸引了多种应用,包括氧离子传导,氧气体吸收和催化。

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