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arXiv 1003.2068cond-mat.str-el
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反常压力对多铁性BiMnO3磁有序的影响

Anomalous pressure effect on the magnetic ordering in multiferroic BiMnO3

C. C. Chou, S. Taran, J. L. Her, C. P. Sun, C. L. Huang, H. Sakurai, A. A. Belik, E. Takayama-Muromachi, H. D. Yang

摘要:

我们报道了高压下不同批次合成的粉末和块体多铁性BiMnO 3样品的磁场依赖性直流磁化强度和压力依赖性(pmax ~ 16 kbar)交流磁化率Xp(T)。在TC ~ 100 K观察到明显的铁磁(FM)转变,并随磁场的增加而增强.磁滞行为类似于软铁磁体。交流磁化率数据表明,FM峰和它的温度(TC)同时随着压力的增加而降低。有趣的是,在高于一定压力(9 ~ 11 kbar)时,在Tp ~ 93 K处出现另一个峰,该峰也随压力的增加而减小,并且这两个峰在一定的中间压力范围(9 ~ 13 kbar)内持续存在。FM峰随着进一步施加压力而消失;然而,第二个峰持续到当前压力极限(pmax ~ 16 kbar)。这些功能被认为是源于复杂的相互作用的磁性和轨道结构的BiMnO 3受到压力。

英文摘要:

We report the magnetic field dependent dc magnetization and the pressure-dependent (pmax ~ 16 kbar) ac susceptibilities Xp(T) on both powder and bulk multiferroic BiMnO3 samples, synthesized in different batches under high pressure. A clear ferromagnetic (FM) transition is observed at TC ~ 100 K, and increases with magnetic field. The magnetic hysteresis behavior is similar to that of a soft ferromagnet. Ac susceptibility data indicate that both the FM peak and its temperature (TC) decrease simultaneously with increasing pressure. Interestingly, above a certain pressure (9 ~ 11 kbar), another peak appears at Tp ~ 93 K, which also decreases with increasing pressure, with both these peaks persisting over some intermediate pressure range (9 ~ 13 kbar). The FM peak disappears with further application of pressure; however, the second peak survives until present pressure limit (pmax ~ 16 kbar). These features are considered to originate from the complex interplay of the magnetic and orbital structure of BiMnO3 being affected by pressure.

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