peanutaxis said:
Why is the triple point slightly above 0°C? (0.0100°C)
This seems straightforward enough to reason out from simple principles. Let us see whether that is so.
Zero degrees is, at least traditionally, the freezing/melting point of pure water under ordinary atmospheric pressure -- dry air at 1 atm.
Under these conditions, the water/ice mixture will be out-gassing water vapor. We are not at the triple point yet.
So we allow the mixture to outgas until the ambient partial pressure of water vapor is high enough so that equilibrium is attained. And we remove the air. Now we have water, ice and water vapor.
The pressure of the vapor on the water/ice mixture is far less than 1 atm.
Water expands when it freezes and contracts when it melts. One effect of that original 1 atm pressure was to force the equilibrium in the direction of melting more ice. Like the idea of ice skates melting a track in the ice. Now that we have removed the pressure,
the equilibrium shifts in the direction of allowing more ice to freeze. The freezing temperature has been elevated.
If you get confused trying to figure how the freezing temperature shifts, think about the trick of using salt and ice to make ice cream in an old fashioned ice cream freezer. If you shift the equilibrium of an ice/water mixture in the direction of melting ice, you depress the freezing temperature -- so that you can make the ice cream. If you shift the equilibrium in the direction of freezing ice you do the opposite. You raise the freezing temperature.
QED.
Edit: Scooped by
@DrClaude but I like to think in terms of ice skates and ice cream rather than phase diagrams.