在压力下在Fe4O5中进行Verwey类型的电荷排序和位置选择性Mott转换
Samar Layek1,2, Eran Greenberg3,4, Stella Chariton3
1School of Physics and Astronomy, Tel Aviv University, 69978 Tel Aviv, Israel.
Journal of the American Chemical Society
|June 1, 2022
概括
高压将混合价值Fe4O5从绝缘体转化为金属,使其电荷排序和磁矩崩. 这项研究揭示了这种复杂的氧化铁中压力调节的电子和磁性状态.
科学领域:
- 凝聚物质物理
- 材料科学
- 固态化学
背景情况:
- 电子相关性驱动的金属绝缘体转换是凝聚物质的基本作用.
- 混合价值化合物经常表现出电荷排序 (CO),导致复杂的相位.
- 磁铁 (Fe3O4) 是一种混合价值材料的经典例子,具有争论的电荷排序.
研究的目的:
- 在高压下研究混合价值Fe4O5的电子,磁性和结构性质.
- 了解Fe4O5中的电荷排序及其转换的性质.
- 提供一个微观的解释,将Fe4O5的行为与其他带电物质结合起来.
主要方法:
- 高分辨率的X射线衍射.
- 电阻测量
- 密度函数理论加动平均场理论 (DFT+DMFT) 的计算.
主要成果:
- 在环境条件下,Fe4O5是一种具有Verwey类型电荷排序的窄隙绝缘体.
- 在压力下 (高达100 GPa),Fe4O5表现出电子和磁性转换.
- 在~84 GPa时发生选择性绝缘体到金属的过渡,伴随着价值变化和CO崩.
结论:
- Fe4O5显示压力诱导的电荷顺序调整,与"trimeron"/"dimeron"状态相竞争.
- 这项研究将Fe4O5的CO机制与磁铁和稀土酸盐的机制统一.
- 为Fe4O5提供了一个全面的压力-温度相图.
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