Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Uptake of HCl molecules by aqueous sulfuric acid droplets as a function of acid concentration

Journal Article · · Journal of Geophysical Research; (United States)
; ;  [1]; ; ;  [2]
  1. Boston Coll., Chestnut Hill, MA (United States)
  2. Aerodyne Research, Inc., Billerica, MA (United States)
The uptake of Hci molecules by acqueous sulfuric acid droplets was measured at 283 K as a function of acid mole fraction. In the apparatus a controllable stream of monodispersed droplets is produced by a vibrating orifice jet. The droplets enter a flow system containing HCl(g). The droplets are switched on and off while the density of the species is continuously monitored by infrared absorption. From the on-off signal a coefficient for the probability of gas uptake upon collision with the liquid surface is calculated. This coefficient is 0.15 for pure water, remains constant up to 0.1 mole fraction of H{sub 2}SO{sub 4} (40 wt%) and then drops sharply to < 10{sup {minus}2} at 0.2 mole fraction (60 wt%). The results are in accord with calculations based on the decrease in the solubility of HCl with increasing H{sub 2}SO{sub 4} mole fraction. Increasing acidity reduces the dissociation of HCl into H{sup +} and Cl{sup {minus}} in solution. Results indicate that mass accommodation coefficients are large enough so that the HCl content of stratospheric aerosols will be determined entirely by this solubility.
OSTI ID:
5077982
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 95:D5; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English