在稀土矿中,压力诱导的电荷高于室温
Yu Samoshkina1, M Rautskii1, D Neznakhin2
1Kirensky Institute of Physics, Federal Research Center KSC SB RAS, Krasnoyarsk 660036, Russia. uliag@iph.krasn.ru.
Dalton transactions (Cambridge, England : 2003)
|March 7, 2024
概括
稀土矿薄膜表现出接近室温的电荷排序 (CO) 阶段,由内部应变驱动. 这一发现为开发高温CO的材料开辟了道路,用于先进的磁性应用.
科学领域:
- 材料科学 材料科学 材料科学
- 凝聚物质物理学 凝聚物质物理学
- 固态化学 固态化学
背景情况:
- 稀土矿通常在室温以下显示电荷排序 (CO).
- 了解CO相形成对于利用独特的材料特性至关重要.
研究的目的:
- 在Pr1-xSr xMnO3/YSZ和La0.7Sr0.3MnO3/YSZ膜中研究CO相的形成.
- 探索内部应变在诱导高温CO的作用.
主要方法:
- 测量磁性易感度的测量方法
- 电子磁共振是一种电子磁共振.
- 电子显微镜的电子显微镜
主要成果:
- 在Pr1-xSr xMnO3/YSZ膜中观察到室温附近和室温以上的电荷排序 (CO) 阶段.
- CO 阶段形成伴随着马氏体转变的迹象.
- 与结晶体大小和边界相关的内部应变被确定为CO相诱导的关键因素.
结论:
- 内部应变可以在稀土矿中诱导高温CO.
- 这一发现支持开发具有增强磁热,磁电和多铁性质的材料.
- 矿中的压力诱导现象为研究提供了新的方向.
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