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Atmospheric loss processes of 1,2-dibromo-3-chloropropane and trimethyl phosphate

The reactions of 1,2-dibromo-3-chloropropane (DBCP) and trimethyl phosphate with O sub(3) and the OH radical have been investigated at 296 plus or minus 2 K and atmospheric pressure of air by long-path Fourier transform infrared spectroscopic and gas chromatography-mass spectrometry techniques. For...

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Bibliographic Details
Published in:Environmental science & technology 1986-10, Vol.20 (10), p.1043-1046
Main Authors: Tuazon, Ernesto C, Atkinson, Roger, Aschmann, Sara M, Arey, Janet, Winer, Arthur M, Pitts, James N
Format: Article
Language:English
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Summary:The reactions of 1,2-dibromo-3-chloropropane (DBCP) and trimethyl phosphate with O sub(3) and the OH radical have been investigated at 296 plus or minus 2 K and atmospheric pressure of air by long-path Fourier transform infrared spectroscopic and gas chromatography-mass spectrometry techniques. For reaction with O sub(3), upper limits to the rate constants of < 3 x 10 super(-20) cm super(3) molecule super(-1) s super(-1) for 1,2-dibromo-3-chloropropane and < 6 x 10 super(-20) cm super(3) molecule super(-1) s super(-1) for trimethyl phosphate were determined, showing that reaction with O sub(3) is not an important atmospheric loss process for these compounds. With the use of relative rate techniques, OH radical reaction rate constants of 4.4 x 10 super(-13) cm super(3) molecule super(-1) s super(-1) for 1,2-dibromo-3-chloropropane and 7.4 x 10 super(-12) cm super(3) molecule super(-1) s super(-1) for trimethyl phosphate were obtained, leading to calculated tropospheric lifetimes of similar to 55 and similar to 3 days, respectively, for the reactions of these compounds with OH radicals. CH sub(2)BrCOCH sub(2)Cl has been tentatively identified as a product of the reaction of OH radicals with 1,2-dibromo-3-chloropropane.
ISSN:0013-936X
1520-5851
DOI:10.1021/es00152a014