On the evaporation of ammonium sulfate solution.
Aqueous evaporation and condensation kinetics are poorly understood, and uncertainties in their rates affect predictions of cloud behavior and therefore climate. We measured the cooling rate of 3 M ammonium sulfate droplets undergoing free evaporation via Raman thermometry. Analysis of the measurements yields a value of 0.58 +/- 0.05 for the evaporation coefficient, identical to that previously determined for pure water. These results imply that subsaturated aqueous ammonium sulfate, which is the most abundant inorganic component of atmospheric aerosol, does not affect the vapor-liquid exchange mechanism for cloud droplets, despite reducing the saturation vapor pressure of water significantly.
Departments of Chemistry and Earth and Planetary Science, University of California, Berkeley, CA 94720, USA.
Walter S
WS
Drisdell
Richard J
RJ
Saykally
Ronald C
RC
Cohen
D000336:Aerosols / Q000737:chemistry*; D000645:Ammonium Sulfate / Q000737:chemistry*; D001272:Atmosphere / Q000737:chemistry; D002980:Climate; D007700:Kinetics; D008956:Models, Chemical; D044367:Phase Transition; D013696:Temperature
D000336:Aerosols; D000645:Ammonium Sulfate