Bulletin of the American Physical Society
APS March Meeting 2020
Volume 65, Number 1
Monday–Friday, March 2–6, 2020; Denver, Colorado
Session D04: Water Dynamics in Different Environments: Experiment and Theory II. Ice
2:30 PM–5:06 PM,
Monday, March 2, 2020
Room: 109
Sponsoring
Units:
DCP DCOMP DBIO DSOFT
Chair: Teresa Head-Gordon, University of California, Berkeley
Abstract: D04.00002 : Atomic imaging of edge structure and growth of a two-dimensional hexagonal ice
Presenter:
Runze Ma
(International Center for Quantum Materials, Peking University)
Authors:
Runze Ma
(International Center for Quantum Materials, Peking University)
Duanyun Cao
(International Center for Quantum Materials, Peking University)
Chongqin Zhu
(Department of Earth and Environmental Sciences, University of Pennsylvania)
Ye Tian
(International Center for Quantum Materials, Peking University)
Jinbo Peng
(International Center for Quantum Materials, Peking University)
Jing Guo
(International Center for Quantum Materials, Peking University)
Ji Chen
(School of Physics, Peking University)
Xin-Zheng Li
(School of Physics, Peking University)
Joseph S Francisco
(Department of Earth and Environmental Sciences, University of Pennsylvania)
Xiao Cheng Zeng
(Department of Physics, University of Nebraska–Lincoln)
Limei Xu
(International Center for Quantum Materials, Peking University)
Enge Wang
(International Center for Quantum Materials, Peking University)
Ying Jiang
(International Center for Quantum Materials, Peking University)
Here we show that noncontact atomic force microscopy with a CO-terminated tip allows real-space imaging of the edge structures of a 2D bilayer of hexagonal ice grown on an Au(111) surface. We find a new edge type that coexists with the zigzag edge commonly observed in 2D hexagonal crystals, and freeze samples during growth to identify intermediate structures.
When combined with MD simulations, these allow us to reconstruct growth processes that in the case of the zigzag edge involve addition of water molecules to the existing edge and a collective bridging mechanism. Armchair edge growth, in contrast, involves local seeding and edge reconstruction and thus is in stark contrast to conventional views of ice growth. The growth mechanism we have uncovered might also occur at the surface of bilayer hexagonal ice and might support a bilayer-on-bilayer ice growth to 3D ice transformation.
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