voko said:
Those are interesting questions, given your previous statement: "I might add that, even for pure water vapor at pressures up to 10 atmospheres, the ideal gas law accurately describes the behavior (to within about 5%)."
1 atmosphere is certainly less than 10 atmosphere, yet now you say that "the ideal gas law doesn't apply".
Here's how it works. For a single component H2O system (pure water), if the pressure is 1 atm., water vapor (i.e., a gas phase) can be present only at temperatures greater than 100 C. Below this temperature, all the water will condense to liquid water or ice (depending on the temperature). So, if you have liquid water or ice only, you don't expect them to be able to be described by the ideal
gas law. Otherwise it would be called the
ideal liquid law or the
ideal solid law. At temperatures above 100C, if the pressure of the system is ≤ the equilibrium vapor pressure of water at that temperature and also less than 10 atm., the water will be purely in the gas phase and will satisfy the ideal gas law to a good approximation.
Now let's consider a multicomponent gaseous system like air (where H2O is not the only chemical species present). In atmospheric air, water vapor is only one component of the gas phase, and its mole fraction is everywhere less than 0.03. So its partial pressure at sea level in the gas phase is less than 0.03 atm. At locations in the atmosphere where the temperature is 200K (i.e., close to the tropopause), the equilibrium vapor pressure of water is only about 0.000002 atm, while the total air pressure at these locations is on the order of 0.1 atm. At these locations, if ice crystals are present, we expect the partial pressure of the water vapor in the air to be about 0.000002 atm, but, if ice crystals are not present in the air, the partial pressure of the water vapor can be somewhat less than 0.000002 atm. In either case, the gas phase at these locations will behave as an ideal gas, both with respect to the overall gas mixture as well as to the water vapor. In applying the ideal gas law to the water vapor in a gas mixture, however, one uses the partial pressure of the water vapor, not the total pressure.