120°磁性结构inCu2OSO4

V. Favre, G. Tucker, C. Ritter, R. Sibille, P. Manuel, M. Frontzek, M. Kriener, Lin Yang, H. Berger, A. Magrez, N. Casati, I. Živković, H. Rønnow
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引用次数: 1

摘要

本文报道了三维$^9$ (Cu$^{2+}$)磁绝缘体Cu2OSO4在粉末和单晶上的磁性能。这种化合物的磁性原子形成层,其几何结构可以描述为通过二聚体耦合的链系统或每3个自旋被二聚体取代的Kagom\'e晶格。比热和直流磁化率在20k处显示出磁跃迁,中子散射也证实了这一点。从比热数据中提取的磁熵符合每Cu$^{2+}$ S=1/2$的自由度,从直流磁化率中提取的有效矩也是如此。通过对粉末和单晶的中子衍射确定了基态,基态对应于一个$\sim120$度的自旋结构,其中铁磁内二聚体排列导致净铁磁矩。没有证据表明晶格对称性在2k以下会发生变化。我们的研究结果表明,\sample \代表了一种新型的模型晶格,具有受挫的相互作用,可以探索磁序,热和量子涨落之间的相互作用。
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Ferrimagnetic 120∘magnetic structure inCu2OSO4
We report magnetic properties of a 3d$^9$ (Cu$^{2+}$) magnetic insulator Cu2OSO4 measured on both powder and single crystal. The magnetic atoms of this compound form layers, whose geometry can be described either as a system of chains coupled through dimers or as a Kagom\'e lattice where every 3rd spin is replaced by a dimer. Specific heat and DC-susceptibility show a magnetic transition at 20 K, which is also confirmed by neutron scattering. Magnetic entropy extracted from the specific heat data is consistent with a $S=1/2$ degree of freedom per Cu$^{2+}$, and so is the effective moment extracted from DC-susceptibility. The ground state has been identified by means of neutron diffraction on both powder and single crystal and corresponds to a $\sim120$ degree spin structure in which ferromagnetic intra-dimer alignment results in a net ferrimagnetic moment. No evidence is found for a change in lattice symmetry down to 2 K. Our results suggest that \sample \ represents a new type of model lattice with frustrated interactions where interplay between magnetic order, thermal and quantum fluctuations can be explored.
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