首页> 外文期刊>Inorganic Chemistry: A Research Journal that Includes Bioinorganic, Catalytic, Organometallic, Solid-State, and Synthetic Chemistry and Reaction Dynamics >High-pressure synthesis, crystal structure, and properties of In _2NiMnO_6 with antiferromagnetic order and field-induced phase transition
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High-pressure synthesis, crystal structure, and properties of In _2NiMnO_6 with antiferromagnetic order and field-induced phase transition

机译:具有反铁磁序和场致相变的In _2NiMnO_6的高压合成,晶体结构和性质

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摘要

In_2NiMnO_6, a new compound extending the family of double rare-earth perovskites R_2NiMnO_6 (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 (No. 14, cell choice 2), Z = 2, a = 5.13520(1) ?, b = 5.33728(1) ?, c = 7.54559(4) ?, 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 In_2NiMnO_6 is an antiferromagnet with a Néel temperature T_N of 26 K. Its antiferromagnetism puts it apart from other members of the R_2NiMnO_6 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 In_2NiMnO _6 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.
机译:使用高压高温技术(6 GPa和1600 K)制备了In_2NiMnO_6,这是一种将双族钙钛矿R_2NiMnO_6(R =稀土,Y)延伸到较小R离子的新化合物。在室温下通过同步加速器X射线粉末衍射研究了其晶体结构:空间群P2 _1 / n(第14号细胞选择2),Z = 2,a = 5.13520(1),b = 5.33728(1) α,c = 7.54559(4)α,β= 90.1343(1)。观察到Mn〜(4+)和Ni〜(2+)离子的有序度。直流和交流磁化强度和比热测量结果表明,In_2NiMnO_6是反铁磁体,Néel温度T_N为26K。它的反铁磁性使其与R_2NiMnO_6族的其他成员不同,后者观察到铁磁基态,这归因于超交换根据Kanamori-Goodenough法则,Mn〜(4+)和Ni〜(2+)离子之间的相互作用在5 K下从18 kOe观察到场致相变到铁磁态,表明In_2NiMnO _6接近反铁磁-铁磁跃迁边界。第一性原理计算使我们能够解释其反铁磁性和场致相变,并预测E *型反铁磁性基态。

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