No Access Submitted: 01 March 1996 Accepted: 30 July 1996 Published Online: 04 June 1998
American Journal of Physics 65, 404 (1997); https://doi.org/10.1119/1.18555
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  • Mário N. Berberan-Santos
  • Evgeny N. Bodunov
  • Lionello Pogliani
The barometric formula, relating the pressure p(z) of an isothermal, ideal gas of molecular mass m at some height z to its pressure p(0) at height z=0, is discussed. After a brief historical review, several derivations are given. Generalizations of the barometric formula for a nonuniform gravitational field and for a vertical temperature gradient are also presented.
  1. © 1996 American Association of Physics Teachers.