Chlorine atoms as a potential tropospheric oxidant in the marine boundary layer
- 1 September 1993
- journal article
- Published by Springer Nature in Research on Chemical Intermediates
- Vol. 19 (3) , 235-249
- https://doi.org/10.1163/156856793x00091
Abstract
In the troposphere, the hydroxyl radical (OH) has been assumed to be the major oxidant for organics and CO. However, a variety of evidence from both laboraKeywords
This publication has 55 references indexed in Scilit:
- Heterogeneous reactions with NaCl in the El Chichon volcanic aerosolsGeophysical Research Letters, 1991
- The reaction of gaseous N2O5 with solid NaCl at 298 K: Estimated lower limit to the reaction probability and its potential role in tropospheric and stratospheric chemistryGeophysical Research Letters, 1991
- The geochemical cycling of reactive chlorine through the marine troposphereGlobal Biogeochemical Cycles, 1990
- Size distributions and statistical analysis of nitrate, excess sulfate, and chloride deficit in the marine boundary layer during GCE/CASE/WATOXGlobal Biogeochemical Cycles, 1990
- Estimation of night-time N2O5 concentrations from ambient NO2 and NO3 radical concentrations and the role of N2O5 in night-time chemistryAtmospheric Environment (1967), 1986
- Bromine in marine aerosols and the origin, nature and quantity of natural atmospheric bromineAtmospheric Environment (1967), 1986
- Chemical composition of fogwater collected along the California coastEnvironmental Science & Technology, 1985
- The atmospheric aerosol system: An overviewReviews of Geophysics, 1983
- Halogens in the atmosphereReviews of Geophysics, 1981
- Diurnal Variation of Aerosol Trace Element Concentrations In Livermore, California*Journal of the Air Pollution Control Association, 1971