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arXiv 1503.00029cond-mat.str-elcond-mat.mtrl-sci
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化学压力对双钙钛矿SrCaCoOsO6和Ca2CoOsO6磁基态的影响

Effects of chemical pressure on the magnetic ground states of the osmate double perovskites SrCaCoOsO6 and Ca2CoOsO6

Ryan Morrow, Jiaqiang Yan, Michael A. McGuire, John W. Freeland, Daniel Haskel, Patrick M. Woodward

摘要:

随着Ca含量的增加,双钙钛矿体系Sr 2-xCaxCoOsO 6的磁性基态由反铁磁体(x = 0)变为自旋玻璃(x = 1),再变为亚铁磁体(x = 2)。这种交叉是由控制磁交换相互作用相对强度的化学压力效应驱动的。研究了SrCaCoOsO 6和Ca 2CoOsO 6的合成、晶体结构和磁性,并与Sr 2CoOsO 6进行了比较。两种化合物均为单斜晶体结构,具有Co2+和Os 6+的岩盐有序性和a-a-b+八面体倾斜,但随着较小的Ca 2+离子取代Sr 2+,平均Co-O-Os键角从SrCaCoOsO 6的158.0(3)度演变为Ca 2CoOsO 6的150.54(9)度。虽然这种变化似乎很小,但它对磁性有着深远的影响,将磁性基态从Sr 2CoOsO 6的反铁磁性(TN 1 = 108 K,TN 2 = 70 K)改变为SrCaCoOsO 6的自旋玻璃(Tf 1 = 32 K,Tf 2 = 13 K),再改变为Ca 2CoOsO 6的亚铁磁性(TC = 145 K)。在前两个化合物中,观察到的两个转变是一致的Co和Os子晶格之间的弱耦合。

英文摘要:

The magnetic ground state in the double perovskite system Sr2-xCaxCoOsO6 changes from an antiferromagnet (x = 0), to a spin glass (x = 1), to a ferrimagnet (x = 2) as the Ca content increases. This crossover is driven by chemical pressure effects that control the relative strength of magnetic exchange interactions. The synthesis, crystal structure, and magnetism of SrCaCoOsO6 and Ca2CoOsO6 are investigated and compared with Sr2CoOsO6. Both compounds adopt a monoclinic crystal structure with rock salt ordering of Co2+ and Os6+ and a-a-b+ octahedral tilting, but the average Co-O-Os bond angle evolves from 158.0(3) degrees in SrCaCoOsO6 to 150.54(9) degrees in Ca2CoOsO6 as the smaller Ca2+ ion replaces Sr2+. While this change may seem minor it has a profound effect on the magnetism, changing the magnetic ground state from antiferromagnetic in Sr2CoOsO6 (TN1 = 108 K, TN2 = 70 K), to a spin glass in SrCaCoOsO6 (Tf1 = 32 K, Tf2 = 13 K), to ferrimagnetic in Ca2CoOsO6 (TC = 145 K). In the first two compounds the observation of two transitions is consistent with weak coupling between the Co and Os sublattices.

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