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Condensation
In the natural world, we are used to seeing substances like water exist in
three different forms: solid (ice); liquid (water); gas (steam). The gaseous
state generally exists at high temperature,above the boiling point of the liquid,
but there are circumstances under
which a gas exists at a temperature lower than the boiling point, such as in this experiment. So
the atmosphere often contains water vapour, even though the temperature is less
than 100 degrees Celsius. In this condition, water molecules may spontaneously
collect together and form droplets, e.g. fog, rain, or even, under extreme
conditions, ice crystals or snowflakes. Changes of state, such as between liquids and gases, are accurately
described by the science of thermodynamics. The attractive forces between
molecules contribute to a property known as enthalpy, and the tendency of
molecules to fly apart is described by a property known as entropy.
The difference between enthalpy and entropy (multiplied by temperature)
is called free energy. If we calculate the free energy difference between a
liquid and a gas as a function of temperature, we find that when the free energy
difference is exactly zero, then a change of state will occur. Just above this
critical temperature the system is a gas, just below it it is a liquid.
The existence of the different phases is the result of a competition between
the attractive forces between molecules and their kinetic energy. The first of
these pulls the molecules together and the second encourages them to fly
apart. A change of state from a liquid to a gas is called evaporation,
and from a gas to a liquid it is called condensation.