Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Path: utzoo!linus!security!genrad!grkermit!masscomp!clyde!floyd!harpo!seismo!hao!hplabs!sri-unix!KFL@MIT-MC From: KFL%MIT-MC@sri-unix.UUCP Newsgroups: net.physics Subject: none Message-ID: <15746@sri-arpa.UUCP> Date: Thu, 19-Jan-84 22:11:00 EST Article-I.D.: sri-arpa.15746 Posted: Thu Jan 19 22:11:00 1984 Date-Received: Sat, 21-Jan-84 07:17:30 EST Lines: 33 From: Keith F. Lynch Water does not 'dissolve' in air. This is a common misconception, that water vapor is in the air because the air has some 'carrying capacity' for water, and that the relative humidity is the proportion of that capacity that the water vapor is currently filling. Water (like all substances) has a 'vapor pressure'. Water's vapor pressure varies greatly with temperature. Water boils when it becomes hot enough that its vapor pressure exceeds the pressure of the air (or whatever) that is around it. This explains why water boils at a lower temperature at high altitudes, and will boil at any temperature in a vacuum. Thus the 'carrying capacity of the air' depends strongly on temerature but not at all on the pressure or on the composition of the air (excluding gasses which chemically react with water, such as chlorine) and would be excatly the same even if there was no air! Temp (C) Vapor pressure (mm of Mercury) -20 0.8 0 4.6 20 17.5 40 55.3 60 149.3 80 355.1 100 760.0 (1 atmosphere) 120 1489.1 140 2710.9 Note how rapidly the vapor pressure changes. Also note that the vapor pressure of ice is NOT zero (i.e. ice can and does evaporate (slowly)). ...Keith