Factors Affecting Dissolution: Polymorphism, Amorphism and Pseudopolymorphism
Polymer Classification: Crystallinity
Molecular and Ionic Solids
Crystal Growth: Principles of Crystallization
Recrystallization: Solid–Solution Equilibria
Ionic Crystal Structures
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Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity
Published on: January 15, 2014
Arpa Hudait1, Valeria Molinero1
1Department of Chemistry, The University of Utah , 315 South 1400 East, Salt Lake City, Utah 84112-0850, United States.
Atmospheric ice crystals primarily form hexagonal ice from vapor, not disordered ice, except under extreme supersaturation. This finding clarifies ice polymorph formation in clouds and has implications for atmospheric aerosol interactions.
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