As others have said, here's the difference:
Case I: At 50 C and 1 atm, in a system that contains only pure water, all the water will be in a liquid state. That's what phase diagram (a) would show you if the axes were numbered -- you're not on a coexistence line; rather, you're squarely within the liquid region.
Case II: At 50 C and 1 atm, in a system that contains water and air, some of the water will be in the gaseous state.
The natural question is then: Why?
The answer: There's no entropy of mixing in Case I, but there is in Case II.
Specifically: Water molecules will move between phases from regions where their chemical potential is higher, to where it's lower, until the chemical potential is uniform, at which point you've reached equilibrium (with respect to the water).
At 50 C & 1 atm, the chemical potential of pure water in the liquid state is lower than that of pure water in the gas state. Thus, in Case I, where we only have the possibility of pure liquid water and pure gaseous water, all the water will stay in the liquid state.
However, let's now consider Case II. Suppose we have some water in the gaseous state. Why doesn't all that gaseous water move to the liquid state, as in Case I? The reason is that the water in the gaseous state is not pure water! It is water mixed with your inert gas. And its chemical potential is lowered (relative to that of pure water vapor) as a result of the increase in entropy associated with this mixing. If the partial pressure of the water is lower than its vapor pressure, it will move from the liquid phase to the gas phase. As this happens, the chemical potential of the water in the gas phase will increase. When the chemical potential of the water in the gas phase (which includes the entropy of mixing) reaches the chemical potential of the liquid water, you have reached equilibrium. At this point, the partial pressure of the water vapor will be equal to its vapor pressure:
Defintion of terms:
$\mu_{H_2O(g)}^{mix}(T, P_{H_2O(g)})$ is the chemical potential of water vapor in a gaseous mixture at temperature $T$ and partial pressure $P_{H_2O(g)}$
$\mu_{H_2O(g)}^o(T)$ and $\mu_{H_2O(l)}^o(T)$ are the chemical potentials of pure gaseous and liquid water, respectively, at temperature $T$ and standard pressure $P^o$ (where $P^o$ = 1 bar; 1 bar is about 1 atm).
Then:
$$\mu_{H_2O(g)}^{mix}(T, P_{H_2O(g)}) = \mu_{H_2O(g)}^o(T) + RT ln \frac{P_{H_2O(g)}}{P^o},$$
where the logarithmic term is the contribution of the entropy of mixing to the chemical potential. You can see that the lower the partial pressure of the water vapor, the lower the resulting chemical potential.
At equilibrium, the chemical potentials of the water in the pure liquid and mixed gaseous states are equal:
$$\mu_{H_2O(g)}^{mix}(T, P_{H_2O(g)}) = \mu_{H_2O(l)}^o(T)$$
and thus:
$$\mu_{H_2O(g)}^o(T) + RT ln \frac{P_{H_2O(g)}}{P^o} = \mu_{H_2O(l)}^o(T)$$
Consequently:
$$RT ln \frac{P_{H_2O(g)}}{P^o} = \mu_{H_2O(l)}^o(T) - \mu_{H_2O(g)}^o(T)$$
At 50 C and 1 atm, the chemical potential of pure liquid water is less than that of pure gaseous water. Hence the RHS is negative. Equilibrium occurs when $P_{H_2O(g)}$ is sufficiently low that the LHS is equally negative. This is the vapor pressure of water at that temperature.
N.B.: You specified that your gas didn't dissolve in liquid water. But what if it were a real gas, and did? In that case, wouldn't the presence of the real gas (say, air) also lower the chemical potential of the liquid water? The answer is yes, but the amount by which the chemical potential of the liquid water is lowered by this effect is relatively small.