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Geometric frustration in the mixed layer pnictide oxides

机译:混合层中的几何挫败pnictide氧化物

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摘要

We present results from a Monte Carlo investigation of a simple bilayer modelwith geometrically frustrated interactions similar to those found in the mixedlayer pnictide oxides $(Sr_{2}Mn_{3}Pn_{2}O_{2}, Pn=As,Sb).$ Our model iscomposed of two inequivalent square lattices with nearest neighbor intra- andinterlayer interactions. We find a ground state composed of two independentN\'{e}el ordered layers when the interlayer exchange is an order of magnitudeweaker than the intralayer exchange, as suggested by experiment. We observethis result independent of the number of layers in our model. We find evidencefor local orthogonal order between the layers, but it occurs in regions ofparameter space that are not experimentally realized. We conclude thatfrustration caused by nearest neighbor interactions in the mixed layer pnictideoxides is not sufficient to explain the long--range orthogonal order that isobserved experimentally, and that it is likely that other terms (e.g., localanisotropies) in the Hamiltonian are required to explain the magnetic behavior.
机译:我们提出的蒙特卡洛研究结果是一个简单的双层模型的研究,该模型具有类似于在混合层氧化锡$(Sr_ {2} Mn_ {3} Pn_ {2} O_ {2,Pn = As,Sb)中发现的几何受阻相互作用我们的模型由两个不等价的方格组成,它们具有最近的相邻层间和层间相互作用。如实验所表明的,当层间交换比层内交换弱一个数量级时,我们发现一个由两个独立的N ordered'el阶有序层组成的基态。我们观察到的结果与模型中的层数无关。我们找到了层之间局部正交顺序的证据,但是它发生在参数空间的区域中,而该区域没有通过实验实现。我们得出的结论是,混合层氧化锡在混合层中由最邻近相互作用引起的挫败感不足以解释实验观察到的长距离正交顺序,并且可能需要哈密顿量中的其他术语(例如局部各向异性)来解释磁行为。

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