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Imaging surface structure and premelting of ice Ih with atomic resolution
Jiani Hong1, Ye Tian2, Tiancheng Liang1
1International Center for Quantum Materials, School of Physics, Peking University, Beijing, People's Republic of China.
Nature
|May 22, 2024
Summary
Researchers imaged ice surfaces at atomic resolution, revealing mixed stacking domains and the origins of premelting. This work clarifies ice surface structures and the premelting process.
Area of Science:
- Surface Science
- Condensed Matter Physics
- Physical Chemistry
Background:
- Ice surfaces influence crucial physical and chemical processes, including melting, friction, and atmospheric reactions.
- Despite extensive research, the precise atomic structures of ice interfaces remain poorly understood due to the delicate hydrogen-bonding network and complex premelting phenomena.
Purpose of the Study:
- To achieve atomic-resolution imaging of the basal (0001) surface of hexagonal water ice (ice Ih).
- To elucidate the atomic structure of ice surfaces and understand the molecular mechanisms behind ice premelting.
Main Methods:
- Utilized qPlus-based cryogenic atomic force microscopy (AFM) with a carbon monoxide-functionalized tip for high-resolution imaging.
- Employed density functional theory (DFT) calculations to investigate surface reconstruction and stabilization mechanisms.
Main Results:
- Atomic-resolution imaging revealed the ice-Ih surface comprises mixed Ih- and cubic (Ic)-stacking nanodomains forming periodic superstructures.
- DFT calculations indicated that surface reconstruction, stabilized by minimizing electrostatic repulsion from dangling OH bonds, is energetically favorable over the ideal ice surface.
- Observed surface disordering above 120 Kelvin, signifying the onset of premelting, which initiates at domain boundaries and is influenced by planar local structures.
Conclusions:
- The study provides definitive atomic-scale structural information for the basal ice surface, resolving long-standing debates.
- Identified the molecular origins of ice premelting, highlighting the role of domain boundaries and local structures.
- These findings may necessitate a paradigm shift in understanding ice physics and chemistry, with implications for various surface-dependent phenomena.

