Yee, Lindsay D. and Isaacman-VanWertz, Gabriel and Wernis, Rebecca A. and Meng, Meng and Rivera, Ventura and Kreisberg, Nathan M. and Hering, Susanne V. and Bering, Mads S. and Glasius, Marianne and Upshur, Mary Alice and Be, Ariana Gray and Thomson, Regan J. and Geiger, Franz M. and Offenberg, John H. and Lewandowski, Michael and Kourtchev, Ivan and Kalberer, Markus and de Sa, Suzane and Martin, Scot T. and Alexander, M. Lizabeth and Palm, Brett B. and Hu, Weiwei and Campuzano-Jost, Pedro and Day, Douglas A. and Jimenez, Jose L. and Liu, Yingjun and McKinney, Karena A. and Artaxo, Paulo and Viegas, Juarez and Manzi, Antonio and Oliveira, Maria B. and de Souza, Rodrigo and Machado, Luiz A. T. and Longo, Karla and Goldstein, Allen H..
(2018)
Observations of sesquiterpenes and their oxidation products in central Amazonia during the wet and dry seasons.
ATMOSPHERIC CHEMISTRY AND PHYSICS, 18 (14).
pp. 10433-10457.
Full text not available from this repository.
Official URL: https://edoc.unibas.ch/74519/
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Abstract
Biogenic volatile organic compounds (BVOCs) from the Amazon forest region represent the largest source of organic carbon emissions to the atmosphere globally. These BVOC emissions dominantly consist of volatile and intermediate-volatility terpenoid compounds that undergo chemical transformations in the atmosphere to form oxygenated condensable gases and secondary organic aerosol (SOA). We collected quartz filter samples with 12 h time resolution and performed hourly in situ measurements with a semi-volatile thermal desorption aerosol gas chromatograph (SV-TAG) at a rural site ("T3") located to the west of the urban center of Manaus, Brazil as part of the Green Ocean Amazon (GoAmazon2014/5) field campaign to measure intermediate-volatility and semi-volatile BVOCs and their oxidation products during the wet and dry seasons. We speciated and quantified 30 sesquiterpenes and 4 diterpenes with mean concentrations in the range 0.01-6.04 ng m(-3) (1670 ppq(v)). We estimate that sesquiterpenes contribute approximately 14 and 12% to the total reactive loss of O-3 via reaction with isoprene or terpenes during the wet and dry seasons, respectively. This is reduced from similar to 50-70% for within-canopy reactive O-3 loss attributed to the ozonolysis of highly reactive sesquiterpenes (e.g., beta-caryophyllene) that are reacted away before reaching our measurement site. We further identify a suite of their oxidation products in the gas and particle phases and explore their role in biogenic SOA formation in the central Amazon region. Synthesized authentic standards were also used to quantify gas-and particle-phase oxidation products derived from beta-caryophyllene. Using tracer-based scaling methods for these products, we roughly estimate that sesquiterpene oxidation contributes at least 0.4-5% (median 1 %) of total submicron OA mass. However, this is likely a low-end estimate, as evidence for additional unaccounted sesquiterpenes and their oxidation products clearly exists. By comparing our field data to laboratory-based sesquiterpene oxidation experiments we confirm that more than 40 additional observed compounds produced through sesquiterpene oxidation are present in Amazonian SOA, warranting further efforts towards more complete quantification.
Faculties and Departments: | 05 Faculty of Science > Departement Umweltwissenschaften > Geowissenschaften > Atmospheric Sciences (Kalberer) |
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UniBasel Contributors: | Kalberer, Markus |
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Item Type: | Article, refereed |
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Article Subtype: | Research Article |
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Publisher: | COPERNICUS GESELLSCHAFT MBH |
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ISSN: | 1680-7316 |
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Note: | Publication type according to Uni Basel Research Database: Journal article |
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Identification Number: | |
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Last Modified: | 03 Apr 2020 13:51 |
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Deposited On: | 03 Apr 2020 13:51 |
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