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arXiv 0904.4014cond-mat.mtrl-scicond-mat.str-el
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多铁性体系LiCu2O2的研究I样品表征及磁性与多铁性的关系

Studies of Multiferroic System LiCu2O2 I Sample Characterization and Relationship between Magnetic Properties and Multiferroic Nature

Yukio Yasui, Kenji Sato, Yoshiaki Kobayashi, Masatoshi Sato

摘要:

单晶样品的LiCu 2 O2与自旋1/2 Cu 2+链的边共享CuO 4正方形平面(带状链),其特征在于通过X射线衍射,热重分析,和磁性测量。既没有发现原子缺陷,也没有发现Cu和Li原子的混合,这表明可以排除晶格缺陷被认为是报告的多铁性行为的可能起源。在比热和中子磁布拉格反射数据中发现的异常清楚地表明,该系统在TN 1 =24.5 K和TN 2 =22.8 K处具有连续的磁转变。基于中子散射和~ 7 Li-NMR测量的结合研究确定的中间相(TN_2 <T<TN_1)和低温相(T<TN_2)的磁结构,我们可以一致地理解这样一个事实,即通过考虑现有的理论,仅在TN_2以下观察到多铁性。

英文摘要:

Single-crystal samples of LiCu2O2 with spin 1/2 Cu2+ chains of edge-sharing CuO4 square planes (ribbon chains), have been characterized by X-ray diffraction, thermogravimetric analysis, and magnetic measurements. Neither the atomic deficiency nor the mixing of Cu and Li atoms has been found, indicating that lattice defects conceived as a possible origin of the reported multiferroic behavior can be excluded. Anomalies found in the data of specific heat and neutron magnetic Bragg reflections show clear evidence that the system exhibits successive magnetic transitions at TN1=24.5 K and TN2=22.8 K. Based on the magnetic structures in the intermediate (TN2<T<TN1) and low temperature (T<TN2) phases, determined by the combined studies of neutron scattering and 7Li-NMR measurements, we can consistently understand the fact that the multiferroic properties are observed only below TN2 by considering existing theories.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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