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arXiv 0906.0416cond-mat.str-el
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锰氧化物中场致电子有序引起的巡回变磁性

Itinerant metamagnetism in manganites caused by the field-induced electronic nematic order

Tian Gao, Shixun Cao, Shujuan Yuan, Chao Jing, Baojuan Kang, Jincang Zhang

摘要:

观察并研究了钙钛矿型La_(1-x)Ca_xMn_(0.90)Cu_(0.10)O_3系统(x = 0.30)的巡回变磁转变。在10 K < T < 150 K的恒定低温下,随着磁场H的增加,出现了从低磁态到高磁态的连续二阶变磁性跃迁。然而,在一个超低的温度,T = 2.5 K,在H = 3.5 T的变磁性跳跃成为一个强大的一级转变,和另一个变磁性转变发生在更高的磁场H = 7.0 T。由于在本系统中没有电荷有序符号,因此不能使用相分离模型或先前的马氏体/奥氏体相变方案来理解。理论上电子有序相的形成被证明是两个连续的变磁性转变的原因,这两个转变将有序相与低场(H < 3.5 T)和高场(H > 7.0 T)各向同性相分开。

英文摘要:

Itinerant metamagnetism transition is observed and studied in perovskite La1-xCaxMn0.90Cu0.10O3 system for x = 0.30. At a constant low temperature, 10 K < T < 150 K, there is a continuous second-order metamagnetism jump from a low magnetic state to a high one with the magnetic field H increasing. However, at an exceeding low temperature, T = 2.5 K, the metamagnetism jump at H = 3.5 T becomes to be a robust first-order transition, and another metamagnetism transition occurs at a higher field H = 7.0 T. Since there is no charge ordering sign in the present system, it can not be understood by using the phase separation model or the prior martensite/austenitic phase transition scenario. A theoretical electronic nematic order phase formation is evidenced to answer for the two consecutive metamagnetic transitions, which separate the nematic phase from the low-field (H < 3.5 T) and high-field (H > 7.0 T) isotropic phases.

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