Use of cosmogenic S-35 to determine the rates of removal of atmospheric SO2

Details Use of cosmogenic S-35 to determine the rates of removal of atmospheric SO2 Use of cosmogenic S-35 to determine the rates of removal of atmospheric SO2

Jul 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991natur.352..226t&link_type=abstract

Nature (ISSN 0028-0836), vol. 352, July 18, 1991, p. 226-228. Research supported by DOE and NSF.

Computer Science

8

Air Pollution, Atmospheric Composition, Scavenging, Sulfur Dioxides, Sulfur Isotopes, Aerosols, Earth Surface, Planetary Boundary Layer, Vegetation

Scientific paper

The use of cosmogenic S-35 to determine the time constants for oxidation, in-cloud scavenging, and aerosol deposition is reported. The method involves determining S-35 levels in gaseous SO2, aerosol sulfate, and precipitation. If these seasonally and regionally variable time constants can be applied to terrestrially produced SO2, S-35 measurements could provide an independent method for studying the rate of SO2 in the atmosphere as a function of time and place.

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