直接观察矿薄膜中透的情况
Liuwan Zhang1, Casey Israel, Amlan Biswas
1Department of Physics, University of Texas, Austin, TX 78712, USA.
概括
在LaPrCaMnO3膜中的铁磁域在冷却时增长,但没有变暖,导致电阻变化. 这种磁性不均性解释了材料的磁电阻特性.
科学领域:
- 凝聚物质物理学 凝聚物质物理学
- 材料科学 材料科学 材料科学
- 磁力学 磁力学 是一种
背景情况:
- La0.33Pr0.34Ca0.33MnO3 具有复杂的磁性和电子性质.
- 了解域动力学对于解释矿矿中的磁电阻至关重要.
研究的目的:
- 为了研究铁磁域在La0.33Pr0.34Ca0.33MnO3薄膜中的温度依赖性行为.
- 为了将域增长和磁性与电阻变化和磁阻变化相关联.
主要方法:
- 跨金属绝缘体过渡的电阻测量.
- 在冷却和变暖周期期间对磁域进行成像和分析.
主要成果:
- 铁磁域在金属绝缘体过渡温度 (TP1) 和以下冷却时增长,而在加热期间保持静态,直到接近TP1.1.
- 平均磁化率的下降与电阻率的跳跃有关.
- 观察到局部磁性歇斯底里和不均性,一些域持续在TP2.2以上.
结论:
- 观察到的域动态和磁性不均性是理解La0.33Pr0.34Ca0.33MnO3.3中的磁阻的关键.
- 在冷却和变暖期间不对称的域增长有助于电阻性歇斯底里.
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