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Long-Range Antiferromagnetic Ordering in B‑Site Ordered Double Perovskite Ca2ScOsO6

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Figshare2016-03-01 更新2026-04-29 收录
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https://figshare.com/articles/dataset/Long_Range_Antiferromagnetic_Ordering_in_B_Site_Ordered_Double_Perovskite_Ca_sub_2_sub_ScOsO_sub_6_sub_/2298130
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A new Os-based B-site ordered double perovskite with the chemical composition of Ca2ScOsO6 was successfully synthesized. The crystal structure of the title compound was determined by employing the powder X-ray diffraction method and was found to crystallize in the monoclinic P21/n space group with the cell constants of a = 5.4716(1) Å, b = 5.6165(1) Å, c = 7.8168 (1) Å, and β = 89.889 (2)°. The temperature-dependent magnetic susceptibility data suggest that this novel S = 3/2 compound undergoes an antiferromagnetic transition at ∼69 K. Fitting the high-temperature susceptibility data (100–300 K) to Currie–Weisse behavior showed C = 1.734 emu·K/mol (μeff = 3.72 bohr magnetons) and θ = −341 K, which is indicative of dominant antiferromagnetic interactions. Temperature-dependent specific heat measurements exhibit a λ shape anomaly at 69 K, which is consistent with a long-range ordering of the spins. Because of a triangular arrangement of antiferromagnetically ordered magnetic ions, the system exhibits some degree of geometric magnetic frustration (GMF), but not strongly. Spin-dimer analysis, employing extended Hückel theory, reveals that a dominant exchange interaction exists (along the a crystallographic axis in perovskite layer), which violates the perfect condition for GMF.

本研究成功合成了一种化学组成为Ca₂ScOsO₆的新型锇(Os)基B位有序双钙钛矿。通过粉末X射线衍射法解析得到该标题化合物的晶体结构,结果显示其属单斜晶系P2₁/n空间群,晶胞参数为a=5.4716(1) Å、b=5.6165(1) Å、c=7.8168(1) Å,β=89.889(2)°。变温磁化率测试数据表明,该自旋量子数S=3/2的新型化合物在约69 K处发生反铁磁相变。将100~300 K区间的高温磁化率数据拟合至居里-外斯(Curie-Weiss)模型,得到居里常数C=1.734 emu·K/mol(有效磁矩μeff=3.72玻尔磁子(bohr magnetons))以及外斯温度θ=-341 K,这表明体系中存在占主导地位的反铁磁相互作用。变温比热测量结果显示,在69 K处存在λ型反常峰,该结果与自旋的长程有序行为一致。由于反铁磁有序的磁性离子呈三角排列,该体系表现出一定程度的几何磁阻挫(geometric magnetic frustration, GMF),但阻挫程度并不强烈。采用扩展休克尔理论(extended Hückel theory)进行自旋二聚体分析后发现,体系中存在占主导地位的交换相互作用(沿钙钛矿层内的晶轴a方向),这破坏了几何磁阻挫的完美形成条件。
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2016-03-01
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