Surface melting: Difference between revisions
Jump to navigation
Jump to search
Carl McBride (talk | contribs) No edit summary |
m (→General reading: Added a publication) |
||
| (2 intermediate revisions by 2 users not shown) | |||
| Line 1: | Line 1: | ||
{{Stub-general}} | |||
==General reading== | ==General reading== | ||
*[http://dx.doi.org/10.1063/1.1750497 Max Born "Thermodynamics of Crystals and Melting", Journal of Chemical Physics '''8''' pp. 591-603 (1939)] | |||
*[http://dx.doi.org/10.1080/00107518908225509 J. G. Dash "Surface melting", Contemporary Physics '''30''' pp. 89-100 (1989)] | |||
*[http://dx.doi.org/10.1063/1.2169444 Robert Rosenberg "Why Is Ice Slippery?", Physics Today December 2005 pp. 50-55] | *[http://dx.doi.org/10.1063/1.2169444 Robert Rosenberg "Why Is Ice Slippery?", Physics Today December 2005 pp. 50-55] | ||
[[category: Confined systems]] | |||
[[category: complex systems]] | |||
Latest revision as of 11:26, 2 July 2009
|
This article is a 'stub' page, it has no, or next to no, content. It is here at the moment to help form part of the structure of SklogWiki. If you add sufficient material to this article then please remove the {{Stub-general}} template from this page. |