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arXiv 1805.00543cond-mat.str-el
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双钙钛矿结构Sr $_2$ FeOsO $_6$中磁激发能隙的起源

Origin of magnetic excitation gap in double perovskite Sr$_2$FeOsO$_6$

A. E. Taylor, R. Morrow, M. D. Lumsden, S. Calder, M. H. Upton, A. I. Kolesnikov, M. B. Stone, R. S. Fishman, A. Paramekanti, P. M. Woodward, A. D. Christianson

摘要:

Sr $_2$ FeOsO $_6$是一种绝缘的双钙钛矿化合物,在140 K($T_{N1}$)和67 K($T_{N2}$)下经历反铁磁转变。为了研究引起这种行为的潜在的电子和磁相互作用,我们进行了非弹性中子散射(INS)和共振非弹性X射线散射(RIXS)的多晶样品的Sr $_2$ FeOsO $_6$的实验。INS数据表明,自旋激发谱在T $_{N1}$以下仍然是无间隙的,然而在T $_{N2}$以下,产生6.8 meV的间隙。RIXS数据揭示了T $_{2g}$多重峰的分裂,与在其他5d $^3$锇基双钙钛矿中看到的一致。总之,这些结果表明,自旋轨道耦合是重要的基态选择在3d-5d PDMATHAMT双钙钛矿材料。

英文摘要:

Sr$_2$FeOsO$_6$ is an insulating double perovskite compound which undergoes antiferromagnetic transitions at 140 K ($T_{N1}$) and 67 K ($T_{N2}$). To study the underlying electronic and magnetic interactions giving rise to this behavior we have performed inelastic neutron scattering (INS) and resonant inelastic x-ray scattering (RIXS) experiments on polycrystalline samples of Sr$_2$FeOsO$_6$. The INS data reveal that the spectrum of spin excitations remains ungapped below T$_{N1}$, however below T$_{N2}$ a gap of 6.8 meV develops. The RIXS data reveals splitting of the T$_{2g}$ multiplet consistent with that seen in other 5d$^3$ osmium based double perovskites. Together these results suggest that spin-orbit coupling is important for ground state selection in 3d-5d$^3$ double perovskite materials.

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