在氧化铁纳米粒子中,水静压诱导的可逆相变化
Arkaprava Das1, Anumeet Kaur2, Parwinder Kaur3
1Chimie des Interaction Plasma surface, Université of Mons, Mons, Belgium. arkapravadas222@gmail.com.
Nanoscale
|June 18, 2024
概括
水位压力在立方和四角相之间可逆地转化磁铁氧化物纳米粒子 (γ-Fe2O3). 使用钻石天细胞观察到的这种行为与纳米颗粒的核心外结构和自旋玻璃特性有关.
科学领域:
- 材料科学 材料科学 材料科学
- 纳米技术纳米技术
- 固态物理 固态物理
背景情况:
- 磁石 (γ-Fe2O3) 纳米粒子具有独特的磁性和结构性质.
- 了解压力诱导的相位转换对于先进的材料应用至关重要.
研究的目的:
- 为了研究在maghemite纳米颗粒中的水静压诱导的可逆相变.
- 阐明结构变化,核心纳米结构和旋转玻璃行为之间的关系.
主要方法:
- 使用热弧等离子体合成maghemite纳米粒子.
- 在现场高压研究使用钻石细胞 (DAC).
- 通过瑞特维尔德精细化和传输电子显微镜 (TEM) 分析结构和相位变化.
主要成果:
- 在高达2.58 GPa的压力下观察到γ-Fe2O3纳米粒子的可逆立方四角形相变.
- 在0.55GPa时,立方和金属铁相的共存.
- 核心外纳米结构表现出旋转玻璃行为,影响磁化和异构性.
结论:
- 可逆相变是由压力诱导的自旋玻璃外行为的变化和内部应力驱动的.
- 原子的重新排列和四角性是由表面核化障碍和旋转障碍引起的.
- "内部应力模型"有效地解释了回到立方相的过渡.
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