Ice XIII
From Wikipedia, the free encyclopedia
Ice XIII is a monoclinic crystalline form of ice formed by cooling water to below 130 K at 500 MPa. It is the proton-ordered form of ice V.
Ordinary water ice is known as ice Ih, (in the Bridgman nomenclature). Different types of ice, from ice II to ice XIV, have been created in the laboratory at different temperatures and pressures.
[edit] References
- Chaplin, Martin (2007-11-11). Ice-five and ice-thirteen structures. Water Structure and Science. Retrieved on 2008-01-02.
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