MadSci Network: Astronomy |
The simple answer is gravity. Gas may flow towards a vacuum, but gravity holds it to the earth. What you see as you increase your altitude is that the air becomes steadily thinner because most of the air is held close to the earth by gravity. So it's not a question of the vacuum of space sucking the air out of the atmosphere, but more the earth's gravity holding as much of the air as close to the earth as it can. The earth does lose some air continuously, but because of heating. In the upper atmosphere, the distance between individual atoms or molecules is pretty large and the temperatures are very high. Since temperature of gas molecules is simply a measure of their average energy, this means that high-temperature gas molecules are moving at high speeds. In the upper atmosphere, they can be moving quickly enough to reach escape velocity and, with no other molecules nearby to slow them down, they can escape into outer space. Something like this helped to remove just about all the hydrogen from the earth's atmosphere early in the history of the planet. You can find more details about both of these phenomena in most introductory books about astronomy or atmospheric science. In addition, "Planet Earth" (Cesare Emiliani, Cambridge University Press, 1992) gives a good general discussion of this topic and "The Chemical Evolution of the Atmosphere and Oceans" (Heinrich Holland, Princeton University Press, 1984) gives a much more detailed and technical account. Both are excellent books, but Holland's is not for the scientifically faint of heart. Emiliani's, on the other hand, is an excellent general reference for many questions about the earth and its history.
Try the links in the MadSci Library for more information on Astronomy.