原子分辨率成像显示在石墨上的二维无形冰中无核结晶
Zi-Feng Yuan1, Ye Tian2, Binze Tang1
1International Center for Quantum Materials, School of Physics, Peking University, Beijing, 100871, China.
Nature communications
|September 29, 2025
概括
研究人员在石墨上可视化了二维冰结晶,揭示了非经典的碎形到紧的途径. 吸附的水分子促进了这种独特的排序机制,为2D结晶过程提供了新的见解.
科学领域:
- 表面科学是一门学科.
- 材料科学 材料科学 材料科学
- 物理化学 物理化学
背景情况:
- 二维 (2D) 结晶对于自然现象和技术至关重要.
- 了解二维结晶的原子尺度机制是一个挑战.
- 经典的核化理论往往无法解释二维结晶过程.
研究的目的:
- 在石墨表面研究二维冰结晶的微观机制.
- 在结晶过程中观察原子尺度的短暂状态.
- 阐明吸附水分子在结晶途径中的作用.
主要方法:
- 使用基于qPlus的冷原子力显微镜 (AFM) 进行原子分辨率成像.
- 分子动力学 (MD) 模拟.分子动力学 (MD) 模拟.
- 结合AFM和MD方法来研究二维无形双层冰.
主要成果:
- 随着温度的增加,在2D冰结晶过程中观察到碎形到紧形的过渡.
- 确定了一种非经典的结晶路径,涉及碎形岛屿的树突延伸和随后的紧增长.
- 证明了外平面吸附水分子在促进结网络重组中的关键作用.
结论:
- 这项研究揭示了2D结晶的非经典排序机制,它偏离了经典的核化理论.
- 吸附的水分子充当中介,指导从无序到有序的六角冰结构的过渡.
- 这些发现为2D极限的结晶现象提供了一般的见解,适用于各种接口和薄膜.
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