This MedLibrary.org supplementary page on Ice VI is provided directly from the open source Wikipedia as a service to our readers. Please see the note below on authorship of this content, as well as the Wikipedia usage guidelines. To search for other content from our encyclopedia supplement, please use the form below:
Related Sponsors
Ice VI is a tetragonal crystalline form of ice formed by cooling water to 270 K at 1.1 GPa. It exhibits Debye relaxation. A proton-ordered form of ice VI has been predicted but not proven, as ice XV near 108-80 K.
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.
References
- Chaplin, Martin (2007-11-11). "Ice-six structure". Water Structure and Science. Retrieved on 2008-01-02.
|
|||||||
 |
This material-related article is a stub. You can help Wikipedia by expanding it. |
 |
This physical chemistry-related article is a stub. You can help Wikipedia by expanding it. |
 |
This inorganic compound-related article is a stub. You can help Wikipedia by expanding it. |
Wikipedia content modification information:
- This page was last modified on 23 October 2008, at 19:28.
Wikipedia Authorship and Review
Wikipedia content provided here is not reviewed directly by MedLibrary.org. Wikipedia content is authored by an open community of volunteers and is not produced by or in any way affiliated with MedLibrary.org.
Wikipedia Usage Guidelines
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article on "Ice VI".
The URL for this specific entry is:
All Wikipedia text is available under the terms of the GNU Free Documentation License. (See Copyrights for details). Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc.