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Updated: Mar 23, 2026

Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity
Published on: January 15, 2014
High yield, single crystal ice via the Bridgman method.
Patrick Bisson1, Henning Groenzin2, Irene Li Barnett3
1Department of Chemistry, Tufts University, Medford, Massachusetts 02155, USA.
Researchers developed a new ice-growth machine to create large, optically flawless single ice crystals. This advancement supports crucial surface chemistry research by providing reliable, high-yield samples for spectroscopy and scattering studies.
Area of Science:
- Surface science
- Materials science
- Crystallography
Background:
- Understanding ice and water surface chemistry is vital for environmental studies.
- Existing ice forms (snow, granular, polycrystalline) lack the required large surface areas of specific crystallographic planes for advanced research.
- Ice serves as a simplified model for studying the complex hydrogen bonding in liquid water.
Purpose of the Study:
- To develop a reliable and reproducible method for producing large single ice crystals with specific crystallographic orientations.
- To enable fundamental spectroscopy and scattering studies requiring well-defined ice surfaces.
- To advance the study of ice surface chemistry and its unique spectral signatures.
Main Methods:
- Design and construction of a computer-controlled ice-growth machine.
- Utilized the Stockbarger modified Bridgeman technique for controlled crystal growth.
- Employed Sum Frequency Generation (SFG) vibrational spectroscopy to characterize unique spectral signatures of different ice faces.
Main Results:
- The developed instrument reliably produces optically flawless, large single ice crystals.
- Achieved high yields with typical success rates of 95%.
- Demonstrated that each crystalline ice face possesses a unique spectral signature, indicating distinct surface chemistry and chemical activity.
Conclusions:
- The novel ice-growth machine provides a high-performance solution for obtaining large single ice crystals, surpassing previous literature reports.
- This method significantly supports surface chemistry research by supplying high-quality, well-oriented ice samples.
- The unique spectral signatures confirm distinct chemical properties for each ice crystallographic face.
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