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Measurement of methyl halides in the marine atmosphere
Institution:1. Division of Environmental Chemistry, National Institute for Environmental Studies, 16-2, Onogawa, Tsukuba, Ibaraki 305-0042, Japan;2. Research Center for Advanced Science and Technology, University of Tokyo, 4-6-1, Komaba, Meguro-ku, Tokyo 153-0041, Japan;1. Univ. Lille, CNRS, UMR 8522 - PC2A - PhysicoChimie des Processus de Combustion et de l’Atmosphère, F-59000 Lille, France;2. Department of Physical and Theoretical Chemistry, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina CH1, 84215 Bratislava, Slovakia;3. Institut de Radioprotection et de Sûreté Nucléaire (IRSN), PSN-RES, Cadarache, St Paul Lez Durance 13115, France;4. Laboratoire de Recherche Commun IRSN-CNRS-Lille1 “Cinétique Chimique, Combustion, Réactivité” (C3R), Cadarache, St Paul Lez Durance 13115, France;1. School of Material Science and Engineering and Key Lab Polymer Composite & Functional Materials, Sun Yat-Sen University, No. 135, Xingang Xi Road, Guangzhou, 510275, PR China;2. School of Materials Sciences and Engineering, Shenyang Aerospace University, Shenyang, 110136, PR China
Abstract:An analytical method for measuring atmospheric methyl halides was established based on canister sampling and capillary GC/MS. Stability tests for air samples collected in two kinds of canisters (electro-chemical buffing and fused-silica lined) with smooth inner surfaces, showed that both provided stable storage for CH3Cl, CH3Br, and CH3I. The method was applied to the measurement of methyl halides at a remote island (Okinawa, Japan) in August 1996, where nocturnal ozone depletion had been observed in summer. We found that atmospheric CH3Cl increased during stable nights and was negatively correlated with surface ozone concentration. The highest CH3Cl concentration amounted to as high as 1400 pptv and indicated that CH3Cl emitted from the surrounding coastal areas had accumulated in the boundary layer under a stable atmosphere at that time. A positive correlation was observed between CH3Br and CH3I, suggesting a common source in the area.
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