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高压合成、晶体结构及具有反铁磁有序和场诱导相变的 In2NiMnO6 的性能。

High-pressure synthesis, crystal structure, and properties of In2NiMnO6 with antiferromagnetic order and field-induced phase transition.

机构信息

International Center for Materials Nanoarchitectonics (WPI-MANA), National Institute for Materials Science (NIMS) , 1-1 Namiki, Tsukuba, Ibaraki 305-0044, Japan.

出版信息

Inorg Chem. 2013 Dec 16;52(24):14108-15. doi: 10.1021/ic401917h. Epub 2013 Dec 3.

Abstract

In2NiMnO6, a new compound extending the family of double rare-earth perovskites R2NiMnO6 (R = rare earth, Y) to smaller R ions, was prepared using a high-pressure and high-temperature technique (6 GPa and 1600 K). Its crystal structure was investigated by synchrotron X-ray powder diffraction at room temperature: space group P2(1)/n (No. 14, cell choice 2), Z = 2, a = 5.13520(1) Å, b = 5.33728(1) Å, c = 7.54559(4) Å, and β = 90.1343(1)°. A significant degree of ordering of Mn(4+) and Ni(2+) ions was observed. The dc and ac magnetization and specific heat measurements showed that In2NiMnO6 is an antiferromagnet with a Néel temperature TN of 26 K. Its antiferromagnetism puts it apart from other members of the R2NiMnO6 family where a ferromagnetic ground state was observed, which is attributed to the superexchange interaction between Mn(4+) and Ni(2+) ions according to the Kanamori-Goodenough rules. A field-induced phase transition to a ferromagnetic state was observed from 18 kOe at 5 K, indicating that In2NiMnO6 is close to the antiferromagnetic-ferromagnetic transition boundary. First-principles calculations allowed us to explain its antiferromagnetism and the field-induced phase transition and predict the E* type antiferromagnetic ground state.

摘要

在 In2NiMnO6 中,一种新的化合物通过高温高压技术(6 GPa 和 1600 K)扩展了双稀土钙钛矿 R2NiMnO6(R = 稀土,Y)家族至更小的 R 离子。其晶体结构通过室温同步加速器 X 射线粉末衍射进行了研究:空间群 P2(1)/n(No. 14,晶胞选择 2),Z = 2,a = 5.13520(1) Å,b = 5.33728(1) Å,c = 7.54559(4) Å,β = 90.1343(1)°。观察到 Mn(4+)和 Ni(2+)离子具有显著程度的有序排列。直流和交流磁化强度和比热测量表明,In2NiMnO6 是一种反铁磁体,奈尔温度 TN 为 26 K。它的反铁磁性使其与 R2NiMnO6 家族的其他成员区分开来,在其他成员中观察到铁磁基态,这归因于根据 Kanamori-Goodenough 规则 Mn(4+)和 Ni(2+)离子之间的超交换相互作用。在 5 K 时从 18 kOe 观察到场诱导的铁磁态相变,表明 In2NiMnO6 接近反铁磁-铁磁相变边界。第一性原理计算允许我们解释其反铁磁性和场诱导的相变,并预测 E*型反铁磁基态。

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