HK911
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Question: What is the best way to melt ice?
The discussion centers on effective methods to melt ice quickly using only conduction and convection, without the use of chemicals or external heat sources. Key strategies include breaking the ice into smaller pieces to maximize surface area and utilizing pressure changes to influence melting rates. Participants suggest using gravity and friction, such as placing a heavy object on the ice or employing a vertical tube to enhance airflow. The consensus indicates that increasing pressure can lower the melting point of ice, although practical methods to achieve this within the constraints of the experiment are debated.
PREREQUISITESStudents, researchers, and educators in physics or chemistry, as well as anyone interested in experimental methods for thermal dynamics and material science.
Lojzek said:No, pressure should be increased to melt ice. But I calculated this effect is to weak to achive impressing results: about 5*10^-5 of the mass of ice will melt for each bar of pressure increase.
This metod would make sense only if we were limited to very short times.
TeTeC said:I cannot show that increasing pressure will work better than decreasing pressure, but I can explain why increasing pressure leads to melting :
http://www.bae.uky.edu/~snokes/BAE549thermo/gasesv1.jpg"
You can see on this diagram that when you are bellow the triple point temperature and around the 1 kPa, increasing the pressure will lead to melting. But it only works for water.
As I've said, I don't know which way is the fastest.
Schrödinger's Dog said:Ok why would increasing pressure work better than decreasing pressure and heating? Not sure I get that?
HK911 said:Thank you very much for the comments. Changing the pressure would be best, but unfortunately, we can't use any external source. The only external sources we can use are the room temperature and gravity for instance.
billiards said:Water (H2O) is unusual in that the solid phase is less dense than the liquid phase, hence ice floats on water - a rare physical property which actually is essential for life as we know it*.
This relates to the fact that under typical surface conditions (i.e. what might be considered normal pressures and temperatures at the surface of a planet) H2O has a negative Clapeyron slope - that basically means that the melting temperature goes down as the pressure is increased. Consider this: imagine you had a body of water all at the same temperature, from experience we know that the ice will form at the surface of the water (I guess we have to be careful here - maybe that happens because the air above the surface is colder, but I believe in laboratories we can control the conditions and can convince ourselves that it is not because of the colder air at the surface); now where is the pressure the greatest? Of course, the pressure is greatest at the bottom of the water because it has a load of water on top of it, but the ice doesn't form at the bottom - the ice forms at the top where the pressure is lowest. So does this not mean that water has a higher freezing point at lower pressures?
That's my understanding anyway.
*If ice was denser than water then the oceans would have completely frozen, because there wouldn't have been an insulating cap of ice at the top to stop all the water from getting very cold (and then freezing solid), life needs liquid water, ergo, if the oceans were frozen we wouldn't have life.