The fate of atmospheric phosgene and the stratospheric chlorine loadings of its parent compounds: CCl4, C2Cl4, C2HCl3, CH3CCl3, and CHCl3

Author:

Kindler T. P.,Chameides W. L.,Wine P. H.,Cunnold D. M.,Alyea F. N.,Franklin J. A.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference58 articles.

1. Kinetics of the gas-phase reactions of Cl atoms with chloroethenes at 298 ± 2 K and atmospheric pressure;Atkinson;Int. J. Chem. Kinet.,1987

2. Low yields of SO2 from dimethyl sulfide oxidation in the marine boundary layer;Bandy;Geophys. Res. Lett,1992

3. Behnke , W. C. Zetzsch The yield of carbon tetrachloride from the tropospheric photochemical degradation of perchloroethene Frauenhofer-Institut fuer Toxikologie und Aerosolforschung Hannover, Germany 1991

4. Chloroethylene photochemical lasers: Vibrational energy content of the HCl molecular elimination products;Berry;J. Chem. Phys.,1974

5. Kinetics of the homogeneous gas phase hydrolysis of CCl3COCl, CCl2HCOCl, CH2ClOCl and COCl2;Butler;J. Air Pollut. Control Assoc.,1979

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