Phase Change with Discontinuity of Temperature: Warm Water in Contact with Cold Ice

Chapter
Part of the Lecture Notes of the Unione Matematica Italiana book series (UMILN, volume 13)

Abstract

Let us consider warm water on cold ice, for instance water flowing on a frozen lake. On the surface of the lake, there is a discontinuity of temperature between the temperature T 2 of the liquid water which is larger than the water freezing temperature T 0 and the temperature T 1 of the ice of the lake which is lower than T 0. It is to be known if the water freezes or if the ice thaws, [111, 153].

Keywords

Free Boundary Water Layer Freeze Ground Temperature Discontinuity Phase Change Temperature 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag Berlin Heidelberg 2012

Authors and Affiliations

  1. 1.Dipartimento di Ingegneria CivileUniversità di Roma “Tor Vergata”RomaItaly

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