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A class of rare antiferromagnetic metallic oxides: double perovskite AMn(3)V(4)O(12) (A = Na+, Ca2+, and La3+) and the site-selective doping effect

机译:一类罕见的反铁磁金属氧化物:双钙钛矿AMn(3)V(4)O(12)(A = Na +,Ca2 +和La3 +)和位点选择性掺杂效应

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摘要

We have investigated the structural, electronic, and magnetic properties of A-site-ordered double-perovskitestructured oxides, AA\u273B4O12 (A = Na, Ca, and La) with Mn and V at A\u27 and B sites, respectively, using firstprinciple calculations based on the density functional theory. Our calculation results show that the antiferromagnetic phase is the ground state for all the compounds. By changing the A-site ions from Na+ to Ca2+ and then to La3+, the transfer of charge between Mn and O ions was changed from 1.56 to 1.55 and then to 1.50, and that between the V and O ions changed from 2.01 to 1.95 and then to 1.93, revealing the cause for the unusual site-selective doping effect. Mn 3d electrons dominate the magnetic moment and are localized, with an intense hybridization with O 2p orbitals, which indicates that the magnetic exchange interaction between Mn ions is mediated through O and that the super exchange mechanism will take effect. These materials have a large one-electron bandwidth W, and the ratio of the on-site Coulomb repulsion U to W is less than the critical value (U/W)c, which leads to metallic behavior of AMn3V4O12. This is further evidenced by the large number of free electrons contributed by V at the Fermi surface. These calculations, in combination with the reported experimental data, prove that these double perovskites belong to the rare antiferromagnetic metallic oxides.
机译:我们使用以下方法研究了A位点有序双钙钛矿结构化氧化物A \ u273B4O12(A = Na,Ca和La)在A \ u27和B位分别具有Mn和V的结构,电子和磁性质基于密度泛函理论的第一性原理计算。我们的计算结果表明,所有化合物的反铁磁相均为基态。通过将A-位离子从Na +变为Ca2 +,然后变为La3 +,Mn和O离子之间的电荷转移从1.56改变为1.55,然后变为1.50,V和O离子之间的电荷转移从2.01改变为1.95,并且然后达到1.93,揭示了异常的站点选择性掺杂效应的原因。 Mn 3d电子支配着磁矩并被局域化,并与O 2p轨道发生强烈杂化,这表明Mn离子之间的磁交换相互作用是通过O介导的,并且超交换机制将起作用。这些材料具有较大的单电子带宽W,并且现场库仑排斥力U与W之比小于临界值(U / W)c,这导致AMn3V4O12的金属行为。 V在费米表面上贡献的大量自由电子进一步证明了这一点。这些计算与所报告的实验数据相结合,证明这些双重钙钛矿属于稀有的反铁磁性金属氧化物。

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