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利用原子分辨率对冰 Ih 的表面结构和预融冰进行成像。

Imaging surface structure and premelting of ice Ih with atomic resolution.

机构信息

International Center for Quantum Materials, School of Physics, Peking University, Beijing, People's Republic of China.

Beijing Key Laboratory of Environmental Science and Engineering, School of Materials Science and Engineering, Beijing Institute of Technology, Beijing, People's Republic of China.

出版信息

Nature. 2024 Jun;630(8016):375-380. doi: 10.1038/s41586-024-07427-8. Epub 2024 May 22.

Abstract

Ice surfaces are closely relevant to many physical and chemical properties, such as melting, freezing, friction, gas uptake and atmospheric reaction. Despite extensive experimental and theoretical investigations, the exact atomic structures of ice interfaces remain elusive owing to the vulnerable hydrogen-bonding network and the complicated premelting process. Here we realize atomic-resolution imaging of the basal (0001) surface structure of hexagonal water ice (ice Ih) by using qPlus-based cryogenic atomic force microscopy with a carbon monoxide-functionalized tip. We find that the crystalline ice-Ih surface consists of mixed Ih- and cubic (Ic)-stacking nanodomains, forming periodic superstructures. Density functional theory reveals that this reconstructed surface is stabilized over the ideal ice surface mainly by minimizing the electrostatic repulsion between dangling OH bonds. Moreover, we observe that the ice surface gradually becomes disordered with increasing temperature (above 120 Kelvin), indicating the onset of the premelting process. The surface premelting occurs from the defective boundaries between the Ih and Ic domains and can be promoted by the formation of a planar local structure. These results put an end to the longstanding debate on ice surface structures and shed light on the molecular origin of ice premelting, which may lead to a paradigm shift in the understanding of ice physics and chemistry.

摘要

冰面与许多物理和化学性质密切相关,如融化、冻结、摩擦、气体吸收和大气反应。尽管进行了广泛的实验和理论研究,但由于脆弱的氢键网络和复杂的预熔过程,冰界面的确切原子结构仍然难以捉摸。在这里,我们通过使用基于 qPlus 的低温原子力显微镜和一氧化碳功能化尖端实现了对六方水冰(冰 Ih)的(0001)基面结构的原子分辨率成像。我们发现,结晶冰-Ih 表面由混合的 Ih 和立方(Ic)堆叠纳米域组成,形成周期性超结构。密度泛函理论表明,这种重构表面主要通过最小化悬空 OH 键之间的静电排斥来稳定理想冰表面。此外,我们观察到随着温度的升高(高于 120 开尔文),冰表面逐渐变得无序,这表明预熔过程的开始。表面预熔从 Ih 和 Ic 域之间的缺陷边界开始,并可通过形成平面局部结构来促进。这些结果结束了关于冰表面结构的长期争论,并揭示了冰预熔的分子起源,这可能导致对冰物理和化学的理解发生范式转变。

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