Diffusive Separation of the Lower Atmosphere
Yosuke Adachi,*
Kenji Kawamura,
Laurence Armi,
Ralph F. Keeling
The separation of atmospheric constituents by gravity has been
proposed theoretically for almost two centuries. However, turbulent
mixing has prevented the detection of this phenomenon in the
lower atmosphere. By using precise measurements of the Ar/N2
ratio of air samples taken under strong nocturnal inversions,
we have detected such separation in near-surface layers. The
effect is shown to be consistent with combined influence of
thermal and gravimetric separation, with the thermal contribution
being more important.
Scripps Institution of Oceanography, 9500 Gilman Drive, La Jolla, CA 920930244, USA.
* Present address: Department of Applied Chemistry, Keio University, Yokohama 223-8522, Japan.
To whom correspondence should be addressed. E-mail: rkeeling{at}ucsd.edu