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Updated: Feb 27, 2026

Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity
Published on: January 15, 2014
Spontaneously polarised crystalline water ice
Rachel L James1, Frank P Pijpers2, Lars Borchert3
1Department of Earth and Environmental Sciences, The University of Manchester, Manchester, UK.
Hexagonal ice (Ih) exhibits molecular orientation, challenging the long-held belief of random dipole directions. This discovery reveals ordered proton disposition and spontaneous polarization within crystalline water ice.
Area of Science:
- Solid-state physics
- Materials science
- Spectroscopy
Background:
- The conventional model of hexagonal ice (Ih) assumes random orientation of water molecular dipoles.
- This assumption has persisted for nearly a century in scientific literature.
- Understanding the precise structure of ice is crucial for various scientific disciplines.
Purpose of the Study:
- To investigate the molecular structure of hexagonal ice (Ih) using advanced spectroscopic techniques.
- To determine if hexagonal ice exhibits net molecular orientation.
- To challenge and potentially revise the existing structural model of ice Ih.
Main Methods:
- Utilizing vacuum-ultraviolet absorption spectroscopy to probe the ice structure.
- Preparing hexagonal ice (Ih) films via condensation of pure water vapor on an insulating substrate (MgF2).
- Analyzing Stark shifts in absorption spectra to detect molecular orientation and internal fields.
Main Results:
- Hexagonal ice (Ih) prepared from pure water vapor shows net molecular orientation.
- This orientation indicates ordered proton disposition, contradicting the random dipole model.
- Spontaneous polarization and internal electric fields of approximately 4 × 10^6 V m^-1 were observed in thin ice films.
Conclusions:
- The established model of hexagonal ice (Ih) requires revision due to observed molecular orientation.
- Proton order, not randomness, characterizes the structure of hexagonal ice.
- The findings reveal intrinsic electric fields within hexagonal ice, with implications for its physical properties.
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