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Temperature dependence of the uptake coefficients of HNO sub 3 , HCl, and N sub 2 O sub 5 by water droplets

Journal Article · · Journal of Physical Chemistry; (USA)
DOI:https://doi.org/10.1021/j100371a009· OSTI ID:6899142
; ;  [1]; ; ;  [2]
  1. Boston College, MA (USA)
  2. Aerodyne Research Inc., Billerica, MA (USA)
The uptake of HNO{sub 3}, HCl, and N{sub 2}O{sub 5} by aqueous surfaces has been measured as a function of temperature over the range from 268 to 294 K. The experimental method employs a monodisperse train of droplets of 200-{mu}m diameter in a low-pressure flow reactor. The value of the uptake coefficient increases with decreasing temperature for each of these species. The similarity in the absolute values of {gamma} at all temperatures for HNO{sub 3}, HCl, and H{sub 2}O{sub 2} (previously reported) suggests that the uptake coefficient is a measure of the rate of physical solvation and is therefore identified as the mass accommodation coefficient. Therefore, the tropospheric cloud chemistry of these species will be determined by their solubility and aqueous-phase reactivity.
OSTI ID:
6899142
Journal Information:
Journal of Physical Chemistry; (USA), Journal Name: Journal of Physical Chemistry; (USA) Vol. 94:8; ISSN 0022-3654; ISSN JPCHA
Country of Publication:
United States
Language:
English