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Organic acids in continental background aerosols
Institution:1. Department of Chemical Engineering, Indian Institute of Technology-Bombay, Mumbai -400 076 India;1. INERIS, Parc Technologique Alata, BP 2, 60550 Verneuil-en-Halatte, France;2. CNRS, EPOC, UMR 5805 CNRS, 33405 Talence, France;3. Université de Bordeaux, EPOC, UMR 5805 CNRS, 33405 Talence, France;4. Univ. Savoie Mont Blanc, LCME, 73000 Chambéry, France;5. IMT Lille Douai, SAGE, 59000 Lille, France;6. Univ. Grenoble Alpes, CNRS, IRD, IGE, F-38000 Grenoble, France;1. Department of Environment and Energy Engineering, Chonnam National University, 77 Yongbong-Ro, Buk-ku, Gwangju 61186, Republic of Korea;2. Center for Gas Analysis, Korea Research Institute of Standards and Science (KRISS), 267 Gajeong-ro, Yuseong-gu, Daejeon 34113, Republic of Korea
Abstract:With a newly developed method aerosol samples from three distinctly different continental sites were analyzed: an urban site (Vienna), a savanna site in South Africa (Nylsvley Nature Reserve, NNR) and a free tropospheric continental background site (Sonnblick Observatory, SBO). In all samples a range of monocarboxylic acids (MCAs) and dicarboxylic acids (DCAs) has been identified and quantified. The three most abundant MCAs in Vienna were the C18, C16 and C14 acids with concentrations of 66, 45 and 36 ng m-3, respectively. At the mid tropospheric background site (SBO) the three most abundant MCAs were the C18, C16 and C12 acid. For the DCAs at all three sites oxalic, malonic and succinic acid were the dominant compounds. For some individual compounds an information about the sources could be obtained. For example the determined unsaturated MCAs in South Africa appear to result from biogenic sources whereas in Vienna those acids are considered to be derived from combustion processes. Oxalic and glyoxalic acid appear to have a free tropospheric air chemical source. The relative high amounts at SBO in comparison to Vienna can only be explained by secondary formation of oxalic acid in the atmosphere.
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