At atmospheric pressure, air has different saturated water contents at various temperatures
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In air at atmospheric pressure, different temperatures correspond to different saturated water contents; when the humidity is too high, moisture will precipitate. So, how can I determine the saturated water content at different temperatures? Thank you. Additional question: For example, if I know a space of fixed volume V, the temperature T, and the relative humidity P, how can I determine the total amount of water vapor W in that space?
I recommend going and reading \"Principles of Chemical Engineering\"; there won’t be a better answer than that.