Crystalline Water Structure in Room‐Temperature Clathrate State: Hydrogen‐Bonded Pentagonal Rings
Source abstract
Abstract
Water hydrogen bonding is extremely versatile; ≈20 ice structures and several types of clathrate hydrate structures are identified. These crystalline water structures form at temperatures below room temperature and/or at high pressure. Transmission electron microscopy is used to study a new crystalline water structure in a clathrate state that is prepared by sandwiching gas‐supersaturated water between graphene layers under ambient conditions. In this clathrate state, water molecules form a 3D hydrogen‐bonding network that encloses gas‐filled cages 2–4 nm in size. Herein, the crystalline water structure is derived by recording and analyzing electron diffraction patterns and performing first‐principles calculations. The structure consists purely of pentagonal rings and has a topology similar to that of water ice XVII. In the study, a mechanism for the formation of the clathrate state is proposed. The results improve the understanding of interactions among water and small nonpolar molecules and offer insights into the local structures of ambient liquid water.
Source: crossref · Quality: baseline
Research context
OpenAlex topics: High-pressure geophysics and materials · Methane Hydrates and Related Phenomena · Geological Studies and Exploration
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
Affiliations
Institute of Physics Academia Sinica Nangang Taipei 115201 Taiwan
Institute of Mathematics for Industry Kyushu University Fukuoka 819‐0395 Japan
Department of Physics Tamkang University New Taipei 251301 Taiwan
Center for Condensed Matter Sciences and Center of Atomic Initiative for New Materials National Taiwan University Taipei 10617 Taiwan
Funding
Ministry of Science and Technology, Taiwan · Academia Sinica
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