Ice phases: Difference between revisions
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*[[Ice XIII]] | *[[Ice XIII]] | ||
*[[Ice XIV]] | *[[Ice XIV]] | ||
*[[Ice XV]] | |||
*[[Low density amorphous ice]] | *[[Low density amorphous ice]] | ||
*[[High density amorphous ice]] | *[[High density amorphous ice]] | ||
Revision as of 17:39, 30 March 2009
- Ice Ih (hexagonal ice)
- Ice Ic (cubic ice)
- Ice II
- Ice III
- Ice IV
- Ice V
- Ice VI
- Ice VII
- Ice VIII
- Ice IX
- Ice X
- Ice XI
- Ice XII
- Ice XIII
- Ice XIV
- Ice XV
- Low density amorphous ice
- High density amorphous ice
- Nano-ice
- Very high density amorphous ice
- Entropy of ice phases
Interesting reading
- Robert Rosenberg "Why Is Ice Slippery?", Physics Today December pp. 50-55 (2005)
- "VIIth Symposium on the Physics and Chemistry of Ice", Le Journal de Physique Colloques 48 No. C1 (1987)