在A和B位替代的石铁矿中实现斜旋弱铁磁性和负热膨胀
Kano Hatayama1, Jun Miyake1, Daiki Ono1
1Materials and Structures Laboratory, Institute of Integrated Research, Institute of Science Tokyo, Yokohama 226-8501, Japan.
Journal of the American Chemical Society
|November 28, 2025
概括
研究人员通过替代元素来修改多铁铁酸盐 (BiFeO3),从而诱导室温弱铁磁性和负热膨胀. 这一发现为基于BiFeO3的新功能材料铺平了道路.
科学领域:
- 材料科学
- 固态物理
- 磁性
背景情况:
- 石铁矿 (BiFeO3) 是一种具有复杂环状旋转秩序的关键多铁材料,可以防止净磁化.
- 研究对BiFeO3的修改对于释放其在先进应用中的潜力至关重要.
研究的目的:
- 探索同时在BiFeO3中替换A位点 (Ca2+) 和B位点 (Ru4+或Ir4+) 的效应.
- 调查由此产生的磁性,铁电和热膨胀特性.
主要方法:
- 在BiFeO3格子中,Ca2+替代Bi3+和Ru4+/Ir4+替代Fe3+.
- 晶体结构,磁性排序和热膨胀行为的特征.
主要成果:
- 在室温下抑制循环旋转调制和诱导倾斜弱铁磁.
- 保持极方方体晶体结构.
- 铁电过渡温度显著降低,在室温周围观察到1.77%的体积负热膨胀.
结论:
- 同时的A和B位置换有效调整BiFeO3的多铁性质.
- 设计的BiFeO3对功能材料应用具有有前途的特性,包括负热膨胀.
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