Autor/es:
M. L. ASAR, E.E. AVILA, R.A. TACCONE, S. I. LANE
Resumen:
ield experiments have shown that fogs, clouds and precipitation play a significant role in the chemical
composition of the atmosphere. The clouds redistribute trace compounds emitted at the Earth?s surface vertically
from the boundary layer to the free troposphere and, in some cases, to the stratosphere, through many processes,
such as scavenging, chemical reactions, precipitation, etc.
Laboratory experiments have been carried out to investigate the uptake of acetic acid (CH3COOH) by water
droplets under controlled temperature and liquid water content conditions. The measurements were performed
with a continuous-flow cloud chamber. A special device has been developed to collect the cloud droplets in
sufficient quantity for chemical analysis by means of gas chromatography. The scavenging ratios were determined
by measuring the concentration of CH3COOH in the cloud droplet and in air. The experiments were performed
under warm cloud conditions and the results show a linear depen