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Evolution of the intrinsic electronic phase separation in La0.6Er0.1Sr0.3MnO3 perovskite

机译:La0.6Er0.1Sr0.3MnO3钙钛矿中本征电子相分离的演化

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摘要

Magnetic and electronic transport properties of perovskite manganite La0.6Er0.1Sr0.3MnO3 have been thoroughly examined through the measurements of magnetization, electron paramagnetic resonance(EPR), and resistivity. It was found that the substitution of Er3+ for La3+ ions introduced the chemical disorder and additional strain in this sample. An extra resonance signal occurred in EPR spectra at high temperatures well above TC gives a strong evidence of electronic phase separation(EPS). The analysis of resistivity enable us to identify the polaronic transport mechanism in the paramagnetic region. At low temperature, a new ferromagnetic interaction generates in the microdomains of Er3+-disorder causing the second increase of magnetization. However, the new ferromagnetic interaction does not improve but decreases electronic transport due to the enhancement of interface resistance among neighboring domains. In view of a really wide temperature region for the EPS existence, this sample provides an ideal platform to uncover the evolution law of different magnetic structures in perovskite manganites.
机译:通过测量磁化强度,电子顺磁共振(EPR)和电阻率,对钙钛矿锰矿La0.6Er0.1Sr0.3MnO3的磁性和电子输运性质进行了彻底检查。结果发现,Er 3 + 取代La 3 + 离子引入了化学无序和附加应变。在远高于TC的高温下,EPR谱中出现了一个额外的共振信号,为电子相分离(EPS)提供了有力的证据。电阻率分析使我们能够确定顺磁区域中的极化传输机制。在低温下,在Er 3 + 无序的微区中产生新的铁磁相互作用,引起磁化强度的第二次增加。但是,由于相邻域之间界面电阻的增加,新的铁磁相互作用不会改善,但会降低电子传输。鉴于EPS存在一个非常宽的温度区域,该样本提供了一个理想的平台,以揭示钙钛矿锰矿中不同磁性结构的演化规律。

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