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Título: | Ambient Gas-Particle Partitioning of Tracers for Biogenic Oxidation |
Autor: | Isaacman-VanWertz, Gabriel A. Yee, Lindsay D. Kreisberg, Nathan M. Wernis, Rebecca A. Moss, Joshua A. Hering, Susanne V. Sá, Suzane S. de Martin, Scot T. Alexander, Michael Lizabeth Palm, Brett B. Hu, Weiwei Campuzano-Jost, Pedro Day, Douglas A. Ji?enez, José Luis Riva, Matthieu Surratt, Jason D. Viegas, Juarez Manzi, Antônio Ocimar Edgerton, Eric S. Baumann, Karsten Souza, Rodrigo Augusto Ferreira de Artaxo, Paulo Goldstein, Allen H. |
Palavras-chave: | Atmospheric Chemistry Chemical Bonds Organic Compounds Environmental Factors Equilibrium Partitioning Model Gas-particle Partitioning Gas-phase Concentration Measurement Sites Oxidation Products Particle Fraction Simultaneous Measurement Oxidation Ambient Air Atmospheric Chemistry Carbon Dioxide Concentration (composition) Environmental Factor Oxidation Particle Size Vapor Pressure Amazonia United States Aerosol Organic Compound Aerosol Chemistry Oxidation Reduction Reaction Vapor Pressure Volatilization Aerosols Organic Chemicals Oxidation-reduction Vapor Pressure Volatilization |
Data do documento: | 2016 |
Revista: | Environmental Science and Technology |
É parte de: | Volume 50, Número 18, Pags. 9952-9962 |
Abstract: | Exchange of atmospheric organic compounds between gas and particle phases is important in the production and chemistry of particle-phase mass but is poorly understood due to a lack of simultaneous measurements in both phases of individual compounds. Measurements of particle- and gas-phase organic compounds are reported here for the southeastern United States and central Amazonia. Polyols formed from isoprene oxidation contribute 8% and 15% on average to particle-phase organic mass at these sites but are also observed to have substantial gas-phase concentrations contrary to many models that treat these compounds as nonvolatile. The results of the present study show that the gas-particle partitioning of approximately 100 known and newly observed oxidation products is not well explained by environmental factors (e.g., temperature). Compounds having high vapor pressures have higher particle fractions than expected from absorptive equilibrium partitioning models. These observations support the conclusion that many commonly measured biogenic oxidation products may be bound in low-volatility mass (e.g., accretion products, inorganic-organic adducts) that decomposes to individual compounds on analysis. However, the nature and extent of any such bonding remains uncertain. Similar conclusions are reach for both study locations, and average particle fractions for a given compound are consistent within ∼25% across measurement sites. © 2016 American Chemical Society. |
DOI: | 10.1021/acs.est.6b01674 |
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