18 results on '"Aline Gratien"'
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2. Atmospheric reactivity of biogenic volatile organic compounds in a maritime pine forest during the LANDEX episode 1 field campaign
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Eric Villenave, Vincent Michoud, Nadine Locoge, Julien Kammer, Stéphane Sauvage, Mohamad Al Ajami, Sebastien Batut, Sandy Bsaibes, Aline Gratien, Thierry Léonardis, Pierre-Marie Flaud, Valérie Gros, Emilie Perraudin, Sebastien Dusanter, François Truong, Kenneth Mermet, Jean-François Doussin, Manuela Cirtog, Christophe Hecquet, Coralie Schoemaecker, Centre for Energy and Environment (CERI EE), Ecole nationale supérieure Mines-Télécom Lille Douai (IMT Lille Douai), Institut Mines-Télécom [Paris] (IMT)-Institut Mines-Télécom [Paris] (IMT), Institut Mines-Télécom [Paris] (IMT), Environnements et Paléoenvironnements OCéaniques (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP), Physicochimie des Processus de Combustion et de l’Atmosphère - UMR 8522 (PC2A), Université de Lille-Centre National de la Recherche Scientifique (CNRS), Chimie Atmosphérique Expérimentale (CAE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Centre for Energy and Environment (CERI EE - IMT Nord Europe), Ecole nationale supérieure Mines-Télécom Lille Douai (IMT Nord Europe), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), and ANR-10-LABX-0045,COTE,COntinental To coastal Ecosystems: evolution, adaptability and governance(2010)
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Environmental Engineering ,Ozone ,010504 meteorology & atmospheric sciences ,010501 environmental sciences ,01 natural sciences ,chemistry.chemical_compound ,Nitrate ,Linalool ,Environmental Chemistry ,Waste Management and Disposal ,Isoprene ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences ,biology ,15. Life on land ,biology.organism_classification ,Pollution ,Trace gas ,chemistry ,13. Climate action ,Environmental chemistry ,Myrcene ,[SDE]Environmental Sciences ,Pinus pinaster ,Camphene ,Environmental science - Abstract
Trace gas measurements were performed during the LANDEX (the LANDes EXperiment) Episode 1 field campaign in the summer 2017, in one of the largest European maritime pine forests (> 95% Pinus pinaster) located in southwestern France. Efforts have been focused on obtaining a good speciation of 20 major biogenic volatile organic compounds (BVOCs, including pinenes, carenes, terpinenes, linalool, camphene, etc.). This was made possible by the development of a new and specific chromatographic method. In order to assess the role of BVOCs in the local gas phase chemistry budget, their reactivity with the main atmospheric oxidants (hydroxyl radicals (OH), ozone (O3) and nitrate radicals (NO3)) and the corresponding consumption rates were determined. When considering the OH reactivity with BVOCs, isoprene and linalool accounted for 10-47% of the OH depletion during daytime, and monoterpenes for 50-65%, whereas monoterpenes were the main contributors during the night (70-85%). Sesquiterpenes and monoterpenes were the main contributors to the ozone reactivity, especially β-caryophyllene (30-70%), with a maximum contribution during nighttime. Nighttime nitrate reactivity was predominantly due to monoterpenes (i.e. 90-95%). Five specific groups have been proposed to classify the 19 BVOCs measured in the forest, according to their reactivity with atmospheric oxidants and their concentrations. The total amount of BVOCs consumed under and above the forest canopy was evaluated for 7 BVOCs (i.e. isoprene, α-pinene, β-pinene, myrcene, limonene + cis-ocimene and Δ3-carene). The reactivity of atmospheric oxidants and BVOCs at a local level are discussed in order to highlight the compounds (BVOCs, other VOCs), the atmospheric oxidants and the main associated reactive processes observed under the canopy of a maritime pine forest.
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- 2021
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3. Methylglyoxal Uptake Coefficients on Aqueous Aerosol Surfaces
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Alexia de Loera, Edouard Pangui, Aline Gratien, Mathieu Cazaunau, Jean-François Doussin, David O. De Haan, and Natalie G. Jimenez
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Ammonium sulfate ,Aqueous solution ,010504 meteorology & atmospheric sciences ,Methylglyoxal ,010501 environmental sciences ,01 natural sciences ,Aerosol ,chemistry.chemical_compound ,chemistry ,Glycine ,Cloud droplet ,Glyoxal ,Relative humidity ,Physical and Theoretical Chemistry ,0105 earth and related environmental sciences ,Nuclear chemistry - Abstract
In order to predict the amount of secondary organic aerosol formed by heterogeneous processing of methylglyoxal, uptake coefficients (γ) and estimates of uptake reversibility are needed. Here, uptake coefficients are extracted from chamber studies involving ammonium sulfate and glycine seed aerosol at high relative humidity (RH ≥ 72%). Methylglyoxal uptake coefficients on prereacted glycine aerosol particles had a strong dependence on RH, increasing from γ = 0.4 × 10–3 to 5.7 × 10–3 between 72 and 99% RH. Continuous methylglyoxal losses were also observed in the presence of aqueous ammonium sulfate at 95% RH (γAS,wet = 3.7 ± 0.8 × 10–3). Methylglyoxal uptake coefficients measured at ≥95% RH are larger than those reported for glyoxal on nonacidified, aqueous aerosol surfaces at 90% RH. Slight curvature in first-order uptake plots suggests that methylglyoxal uptake onto aqueous aerosol surfaces is not entirely irreversible after 20 min. Methylglyoxal uptake by cloud droplets was rapid and largely reversible...
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- 2018
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4. Atmospheric Simulation Chamber Studies of the Gas-Phase Photolysis of Pyruvic Acid
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Edouard Pangui, Jean-François Doussin, Mathieu Cazaunau, Aline Gratien, Veronica Vaida, and Allison E. Reed Harris
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010504 meteorology & atmospheric sciences ,Photodissociation ,Analytical chemistry ,chemistry.chemical_element ,Quantum yield ,Partial pressure ,010402 general chemistry ,Photochemistry ,01 natural sciences ,Nitrogen ,Oxygen ,0104 chemical sciences ,chemistry.chemical_compound ,chemistry ,Surface-area-to-volume ratio ,Pyruvic acid ,Irradiation ,Physical and Theoretical Chemistry ,0105 earth and related environmental sciences - Abstract
Pyruvic acid is an atmospherically abundant α-keto-acid that degrades efficiently from the troposphere via gas-phase photolysis. To explore conditions relevant to the environment, 2–12 ppm pyruvic acid is irradiated by a solar simulator in the environmental simulation chamber, CESAM. The combination of the long path length available in the chamber and its low surface area to volume ratio allows us to quantitatively examine the quantum yield and photochemical products of pyruvic acid. Such details are new to the literature for the low initial concentrations of pyruvic acid employed here. We determined photolysis quantum yields of ϕobsN2 = 0.84 ± 0.1 in nitrogen and ϕobsAir = 3.2 ± 0.5 in air, which are higher than those reported by previous studies that used higher partial pressures of pyruvic acid. The quantum yield greater than unity in air is due to secondary chemistry, driven by O2, that emerges under the conditions in these experiments. The low concentration of pyruvic acid and the resulting oxygen ef...
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- 2017
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5. Glyoxal's impact on dry ammonium salts: fast and reversible surface aerosol browning
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Natalie G. Jimenez, L. N. Hawkins, David O. De Haan, Hannah G. Welsh, Mathieu Cazaunau, Jean-François Doussin, Aline Gratien, Paola Formenti, Margaret A. Tolbert, Kevin Jansen, Raunak Pednekar, Edouard Pangui, Antonin Bergé, Alexia de Loera, Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP), and Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)
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Atmospheric Science ,Ammonium sulfate ,010504 meteorology & atmospheric sciences ,Analytical chemistry ,010501 environmental sciences ,Radiative forcing ,01 natural sciences ,complex mixtures ,lcsh:QC1-999 ,Aerosol ,lcsh:Chemistry ,Absorbance ,chemistry.chemical_compound ,lcsh:QD1-999 ,chemistry ,13. Climate action ,Sodium sulfate ,[SDE]Environmental Sciences ,Sulfate aerosol ,Relative humidity ,Sulfate ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,lcsh:Physics ,0105 earth and related environmental sciences - Abstract
Alpha-dicarbonyl compounds are believed to form brown carbon in the atmosphere via reactions with ammonium sulfate (AS) in cloud droplets and aqueous aerosol particles. In this work, brown carbon formation in AS and other aerosol particles was quantified as a function of relative humidity (RH) during exposure to gas-phase glyoxal (GX) in chamber experiments. Under dry conditions (RH 2 and are consistent between AS and AS–glycine aerosol. Dry methylammonium sulfate aerosol browns 4 times more than dry AS aerosol, but deliquesced AS aerosol browns much less than dry AS aerosol. Optical measurements at 405, 450, and 530 nm provide an estimated Ångstrom absorbance coefficient of -16±4. This coefficient and the empirical relationship between GX and albedo are used to estimate an upper limit to global radiative forcing by brown carbon formed by 70 ppt GX reacting with AS (+7.6×10-5 W m−2). This quantity is
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- 2020
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6. Experimental study of the formation of organosulfates from $\alpha$-Pinene oxidation. 2. Time evolution and effect of particle acidity
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Julien Kammer, Pierre-Marie Flaud, Emmanuel Geneste, Sylvie Augagneur, Houssni Lamkaddam, Geoffroy Duporté, Emilie Perraudin, Eric Villenave, Edouard Pangui, Hélène Budzinski, Aline Gratien, Jean-François Doussin, Environnements et Paléoenvironnements OCéaniques (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), CNRS-INSU is also acknowledged for supporting the CESAM chamber as a national instrument, ANR-13-BS06-0002,COGNAC,Impact de la chimie des biradicaux organiques atmosphériques sur la genèse d'aérosols(2013), European Project: 228335,EC:FP7:INFRA,FP7-INFRASTRUCTURES-2008-1,EUROCHAMP-2(2009), Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), and Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP)
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Anions ,Aerosols ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,Pinene ,Ammonium sulfate ,010304 chemical physics ,Acidity ,Inorganic chemistry ,Oxides ,010402 general chemistry ,01 natural sciences ,0104 chemical sciences ,chemistry.chemical_compound ,chemistry ,0103 physical sciences ,Particle ,Volatile organic compounds ,Physical and Theoretical Chemistry ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,Organosulfate - Abstract
International audience; The present work is an extensive laboratory study of organosulfate (OS) formation from the reaction of α-pinene oxidation products or proxies with acidified ammonium sulfate aerosols in three different acidity conditions (NH$_4$)$_2$SO$_4$ 0.06 M; (NH$_4$)$_2$SO$_4$/H$_2$SO$_4$ 0.06 M/0.005 M; (NH$_4$)$_2$SO$_4$/H$_2$SO$_4$ 0.03 M/0.05 M). The kinetics of the reactions of $\alpha$-pinene, $\alpha$-pinene oxide, isopinocampheol, pinanediol, and myrtenal with ammonium sulfate particles were studied using a quasi-static reactor. The reaction of $\alpha$-pinene oxide with the highly acidic ammonium sulfate particles was determined to be 7, 10, 21, and 24 times faster than for isopinocampheol, $\alpha$-pinene, pinanedial, and myrtenal, respectively, for an OS precursor concentration of 1 ppm and after 1 h reaction time. The effective rate coefficients for OS formation from $\alpha$-pinene oxide were determined to be 2 orders of magnitude higher in highly acidic conditions than for the two other acidity conditions. For $\alpha$-pinene oxide reactions with highly acidic ammonium sulfate particles, OS formation was observed to increase linearly with (i) the time of reaction up to 400 min ($r^2$= > 0.95) and (ii) α-pinene oxide gas-phase concentration. However, OS formation from $\alpha$-pinene oxide reactions with slightly acidic or pure ammonium sulfate particles was limited, with a plateau ([OS]max = 0.62 ± 0.03 $\mu$g) reached after around 15–20 min. Organosulfate dimers (m/z 401 and m/z 481) were detected not only with highly acidic particles but also with slightly acidic and pure ammonium sulfate particles, indicating that oligomerization processes do not require strong acidity conditions. Dehydration products of organosulfates ($m/z$ 231 and $m/z$ 383) were observed only under highly acidic conditions, indicating the key role of H$_2$SO$_4$ on the dehydration of organosulfates and the formation of olefins in the atmosphere. Finally, this kinetic study was completed with simulation chamber experiments in which the mass concentration of organosulfates was shown to depend on the available sulfate amount present in the particle phase ($r^2$ = 0.96). In conclusion, this relative comparison between five organosulfate precursors shows that epoxide was the most efficient reactant to form organosulfates via heterogeneous gas–particle reactions and illustrates how gas–particle reactions may play an important role in OS formation and hence in the atmospheric fate of organic carbon. The kinetic data presented in this work provide strong support to organosulfate formation mechanisms proposed in part 1 ( J. Phys. Chem. A 2016, 120, 7909−7923).
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- 2019
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7. High-NOx Photooxidation of n-Dodecane: Temperature Dependence of SOA Formation
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Aline Gratien, Edouard Pangui, Bénédicte Picquet-Varrault, Houssni Lamkaddam, Jean-François Doussin, and Mathieu Cazaunau
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010504 meteorology & atmospheric sciences ,Meteorology ,Concentration dependence ,Chemistry ,Analytical chemistry ,General Chemistry ,010501 environmental sciences ,01 natural sciences ,Organic vapor ,Aerosol ,N-dodecane ,Environmental Chemistry ,Seeding ,Volatility (chemistry) ,NOx ,Volume concentration ,0105 earth and related environmental sciences - Abstract
The temperature and concentration dependence of secondary organic aerosol (SOA) yields has been investigated for the first time for the photooxidation of n-dodecane (C12H26) in the presence of NOx in the CESAM chamber (French acronym for “Chamber for Atmospheric Multiphase Experimental Simulation”). Experiments were performed with and without seed aerosol between 283 and 304.5 K. In order to quantify the SOA yields, a new parametrization is proposed to account for organic vapor loss to the chamber walls. Deposition processes were found to impact the aerosol yields by a factor from 1.3 to 1.8 between the lowest and the highest value. As with other photooxidation systems, experiments performed without seed and at low concentration of oxidant showed a lower SOA yield than other seeded experiments. Temperature did not significantly influence SOA formation in this study. This unforeseen behavior indicates that the SOA is dominated by sufficiently low volatility products for which a change in their partitioning...
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- 2016
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8. Secondary organic aerosol formation from isoprene photooxidation during cloud condensation–evaporation cycles
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Mathieu Cazaunau, F. Siekmann, H. L. Dewitt, Anne Monod, Vincent Michoud, Jean-François Doussin, L. Bregonzio-Rozier, Andrea Tapparo, S. B. Morales, Edouard Pangui, Brice Temime-Roussel, Chiara Giorio, Aline Gratien, Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), Department of Chemistry [Cambridge, UK], University of Cambridge [UK] (CAM), Laboratoire Chimie de l'environnement (LCE), Aix Marseille Université (AMU)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Institut des Sciences Moléculaires (ISM), Université Montesquieu - Bordeaux 4-Université Sciences et Technologies - Bordeaux 1 (UB)-École Nationale Supérieure de Chimie et de Physique de Bordeaux (ENSCPB)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Dipartimento di Scienze Chimiche [Padova], Università degli Studi di Padova = University of Padua (Unipd), Aix Marseille Université (AMU), Université Montesquieu - Bordeaux 4-Université Sciences et Technologies - Bordeaux 1-École Nationale Supérieure de Chimie et de Physique de Bordeaux (ENSCPB)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Giorio, Chiara [0000-0001-7821-7398], Apollo - University of Cambridge Repository, Universita degli Studi di Padova, Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Aix Marseille Université (AMU)-Centre National de la Recherche Scientifique (CNRS), and Université Montesquieu - Bordeaux 4-Université Sciences et Technologies - Bordeaux 1-École Nationale Supérieure de Chimie et de Physique de Bordeaux (ENSCPB)-Centre National de la Recherche Scientifique (CNRS)
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Atmospheric Science ,010504 meteorology & atmospheric sciences ,Evaporation ,010501 environmental sciences ,Photochemistry ,complex mixtures ,behavioral disciplines and activities ,7. Clean energy ,01 natural sciences ,lcsh:Chemistry ,chemistry.chemical_compound ,Mass concentration (chemistry) ,Dissolution ,NOx ,Isoprene ,0105 earth and related environmental sciences ,[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] ,Aqueous solution ,Condensation ,37 Earth Sciences ,lcsh:QC1-999 ,Aerosol ,lcsh:QD1-999 ,chemistry ,[SDU]Sciences of the Universe [physics] ,13. Climate action ,3701 Atmospheric Sciences ,sense organs ,[CHIM.OTHE]Chemical Sciences/Other ,lcsh:Physics - Abstract
The impact of cloud events on isoprene secondary organic aerosol (SOA) formation has been studied from an isoprene/NOx/light system in an atmospheric simulation chamber. It was shown that the presence of a liquid water cloud leads to a faster and higher SOA formation than under dry conditions. When a cloud is generated early in the photooxidation reaction, before any SOA formation has occurred, a fast SOA formation is observed with mass yields ranging from 0.002 to 0.004. These yields are two and four times higher than those observed under dry conditions. When the cloud is generated at a later photooxidation stage, after isoprene SOA is stabilized at its maximum mass concentration, a rapid increase (by a factor of two or higher) of the SOA mass concentration is observed. The SOA chemical composition is influenced by cloud generation: the additional SOA formed during cloud events is composed of both organics and nitrate containing species. This SOA formation can be linked to water soluble volatile organic compounds (VOCs) dissolution in the aqueous phase and to further aqueous phase reactions. Cloud-induced SOA formation is experimentally demonstrated in this study, thus highlighting the importance of aqueous multiphase systems in atmospheric SOA formation estimations.
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- 2016
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9. Methylamine's Effects on Methylglyoxal-Containing Aerosol: Chemical, Physical, and Optical Changes
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Benjamin W. Joyce, Melanie D. Zauscher, Paola Formenti, Alexia de Loera, Jean-François Doussin, Hannah G. Welsh, Tianqu Cui, Natalie G. Jimenez, Matthieu Riva, L. N. Hawkins, Aki Pajunoja, Matthieu Cazaunau, Edouard Pangui, Alyssa D. Andretta, Aline Gratien, Jason D. Surratt, David O. De Haan, Audrey C. De Haan, IRCELYON-Catalytic and Atmospheric Reactivity for the Environment (CARE), Institut de recherches sur la catalyse et l'environnement de Lyon (IRCELYON), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL), and Université de Lyon-Université de Lyon-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS)
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Atmospheric Science ,Aqueous solution ,Methylamine ,0208 environmental biotechnology ,Methylglyoxal ,Cationic polymerization ,02 engineering and technology ,[CHIM.CATA]Chemical Sciences/Catalysis ,010501 environmental sciences ,Photochemistry ,complex mixtures ,01 natural sciences ,Oligomer ,[SDE.ES]Environmental Sciences/Environmental and Society ,020801 environmental engineering ,Aerosol ,chemistry.chemical_compound ,chemistry ,Space and Planetary Science ,Geochemistry and Petrology ,Particle ,Amine gas treating ,0105 earth and related environmental sciences - Abstract
Methylamine, a common atmospheric amine species, is found in the gas, particle, and aqueous phases. It has been shown to form light-absorbing, oligomeric species in reactions with methylglyoxal and other aldehyde species in bulk aqueous-phase experiments and when mixed into seed aerosol as a sulfate salt. Here, we explore the influence of multiphase methylamine chemistry on aerosol production, properties, and molecular composition. When methylglyoxal aerosol particles were exposed to ∼2 ppm methylamine gas in a humid chamber, rapid browning was observed, but not growth. Aerosol bounce measurements indicated that particles became slightly more viscous and hydrophobic upon methylamine exposure. Subsequent cloud processing increased both viscosity and hygroscopicity but had little effect on browning, consistent with high-resolution mass spectrometry results showing that aerosol oligomer dicarbonyl functional groups were transformed into cationic imidazole rings. Photolytic cloud processing triggered the inco...
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- 2019
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10. POLLURISK: AN INNOVATIVE EXPERIMENTAL PLATFORM TO INVESTIGATE HEALTH IMPACTS OF AIR QUALITY
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Jean-François Doussin, Laurence Thavaratnasingam, Adela Amar, Gilles Foret, Audrey Der Vatanian, Mathieu Cazaunau, Sophie Lanone, Claudia Di Biagio, Geneviève Derumeaux, Jorge Boczkowski, Margaux Mäder, Paola Formenti, Patrice Coll, Sophie Hue, Cécile Gaimoz, Isabelle Coll, Maria Pini, Edouard Pangui, Maeva Zysman, Mickaël Lacavalerie, Aline Gratien, Vincent Michoud, Frédéric Relaix, Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), Institut de Combustion, Aérothermique, Réactivité et Environnement (ICARE), Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut des Sciences de l'Ingénierie et des Systèmes (INSIS), Institut Mondor de recherche biomédicale (IMRB), Institut National de la Santé et de la Recherche Médicale (INSERM)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12), Institut Mondor de Recherche Biomédicale (IMRB), Institut National de la Santé et de la Recherche Médicale (INSERM)-IFR10-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12), Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Physiopathologie et Epidemiologie de l'Insuffisance Respiratoire, Université Paris Diderot - Paris 7 (UPD7)-Institut National de la Santé et de la Recherche Médicale (INSERM), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut des Sciences de l'Ingénierie et des Systèmes (INSIS - CNRS), Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Université de Lorraine (UL), and Université Paris-Saclay-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)
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Pollutant ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,010504 meteorology & atmospheric sciences ,Atmospheric chemistry ,Environmental engineering ,Environmental science ,010501 environmental sciences ,01 natural sciences ,Air quality index ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences - Abstract
International audience
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- 2018
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11. Nitrogen-Containing, Light-Absorbing Oligomers Produced in Aerosol Particles Exposed to Methylglyoxal, Photolysis, and Cloud Cycling
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Adam C. Smith, Jean-François Doussin, Marisol Almodovar, Alexia de Loera, David O. De Haan, Tiffany N. Stewart, Shiva Nilakantan, Mathieu Cazaunau, Edouard Pangui, Mary Caitlin Jordan, Tianqu Cui, Enrico Tapavicza, Aline Gratien, Audrey C. De Haan, Matthieu Riva, Jason D. Surratt, IRCELYON-Catalytic and Atmospheric Reactivity for the Environment (CARE), Institut de recherches sur la catalyse et l'environnement de Lyon (IRCELYON), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL), and Université de Lyon-Université de Lyon-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS)
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010504 meteorology & atmospheric sciences ,Absorption spectroscopy ,Nitrogen ,Electrospray ionization ,Mass spectrometry ,Photochemistry ,01 natural sciences ,Gas Chromatography-Mass Spectrometry ,chemistry.chemical_compound ,0103 physical sciences ,Environmental Chemistry ,Physics::Atmospheric and Oceanic Physics ,0105 earth and related environmental sciences ,Aerosols ,Aqueous solution ,Photolysis ,010304 chemical physics ,Methylamine ,Methylglyoxal ,Photodissociation ,General Chemistry ,[CHIM.CATA]Chemical Sciences/Catalysis ,Pyruvaldehyde ,[SDE.ES]Environmental Sciences/Environmental and Society ,Aerosol ,chemistry - Abstract
Aqueous methylglyoxal chemistry has often been implicated as an important source of oligomers in atmospheric aerosol. Here we report on chemical analysis of brown carbon aerosol particles collected from cloud cycling/photolysis chamber experiments, where gaseous methylglyoxal and methylamine interacted with glycine, ammonium, or methylammonium sulfate seed particles. Eighteen N-containing oligomers were identified in the particulate phase by liquid chromatography/diode array detection/electrospray ionization high-resolution quadrupole time-of-flight mass spectrometry. Chemical formulas were determined and, for 6 major oligomer products, MS2 fragmentation spectra were used to propose tentative structures and mechanisms. Electronic absorption spectra were calculated for six tentative product structures by an ab initio second order algebraic-diagrammatic-construction/density functional theory approach. For five structures, matching calculated and measured absorption spectra suggest that they are dominant lig...
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- 2018
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12. Cloud Processing of Secondary Organic Aerosol from Isoprene and Methacrolein Photooxidation
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Andrea Tapparo, Arthur T. Zielinski, Helen Langley DeWitt, Jean-François Doussin, Magda Claeys, Markus Kalberer, Mathieu Cazaunau, Didier Voisin, Lola Brégonzio-Rozier, Vincent Michoud, Aline Gratien, Reinhilde Vermeylen, Sylvain Ravier, Edouard Pangui, Brice Temime-Roussel, Chiara Giorio, Anne Monod, Department of Chemistry (Cambridge], University of Cambridge [UK] (CAM), Laboratoire Chimie de l'environnement (LCE), Aix Marseille Université (AMU)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), Dipartimento di Scienze Chimiche [Padova], Università degli Studi di Padova = University of Padua (Unipd), Department of Pharmaceutical Sciences, University of Antwerp (UA), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Department of Chemistry, University of Cambridge, Cambridge CB2 1EW, U.K, Universita degli Studi di Padova, Centre National de la Recherche Scientifique (CNRS)-Aix Marseille Université (AMU), Centre National de la Recherche Scientifique (CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS), Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS), Aix Marseille Université (AMU)-Centre National de la Recherche Scientifique (CNRS), Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), and Centre National de la Recherche Scientifique (CNRS)-Aix Marseille Université (AMU)-Institut de Chimie du CNRS (INC)
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010504 meteorology & atmospheric sciences ,Analytical chemistry ,Methacrolein ,010501 environmental sciences ,Mass spectrometry ,7. Clean energy ,01 natural sciences ,complex mixtures ,Article ,chemistry.chemical_compound ,Metastability ,Relative humidity ,Physical and Theoretical Chemistry ,Isoprene ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,Aqueous solution ,[CHIM.ORGA]Chemical Sciences/Organic chemistry ,Physics ,Energy budget ,[SDE.ES]Environmental Sciences/Environmental and Society ,Aerosol ,Chemistry ,chemistry ,13. Climate action ,Environmental chemistry ,sense organs - Abstract
Aerosol-cloud interaction contributes to the largest uncertainties in the estimation and interpretation of the Earth's changing energy budget. The present study explores experimentally the impacts of water condensation-evaporation events, mimicking processes occurring, in atmospheric clouds, on the molecular composition of secondary organic aerosol (SOA) from the photooxidation of methacrolein. A range of on and off-line mass spectrometry techniques were used to obtain a detailed chemical characterization of SOA formed in control experiments in dry conditions, in triphasic experiments simulating gas-particle-cloud droplet interactions (starting from dry conditions and from 60% relative humidity (RH)), and in bulk aqueous-phase experiments. We observed that cloud events trigger fast SOA formation accompanied by evaporative losses. These evaporative losses decreased SOA concentration in the simulation chamber by 25-32% upon RH increase, while aqueous SOA was found to be metastable and slowly evaporated after cloud dissipation. In the simulation chamber, SOA composition measured with a high-resolution time-of flight aerosol mass spectrometer, did not change during cloud events compared with high RH conditions (RH > 80%). In all experiments, off-line mass spectrometry techniques emphasize the critical role of 2-methylglyceric acid as a major product of isoprene chemistry, as an important contributor to the total SOA mass (15-20%) and as a key building block of oligomers found in the particulate phase. Interestingly, the comparison between the series of oligomers obtained from experiments performed under different conditions show a markedly different reactivity. In particular, long reaction times at high RH seem to create the conditions for aqueous-phase processing to occur in a more efficient manner than during two relatively short cloud events.
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- 2017
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13. Brown Carbon Production in Ammonium- or Amine-Containing Aerosol Particles by Reactive Uptake of Methylglyoxal and Photolytic Cloud Cycling
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Aki Pajunoja, Hannah G. Welsh, Paola Formenti, Mathieu Cazaunau, Jason R. Casar, Michael A. Symons, Elyse A. Pennington, Alexia de Loera, Raunak Pednekar, David O. De Haan, Lorenzo Caponi, Edouard Pangui, Melanie D. Zauscher, Aline Gratien, L. N. Hawkins, Natalie G. Jimenez, and Jean-François Doussin
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Aerosols ,Ammonium sulfate ,Aqueous solution ,010504 meteorology & atmospheric sciences ,Inorganic chemistry ,Methylglyoxal ,chemistry.chemical_element ,General Chemistry ,010501 environmental sciences ,Pyruvaldehyde ,complex mixtures ,01 natural sciences ,Carbon ,Aerosol ,chemistry.chemical_compound ,chemistry ,Ammonium Compounds ,Browning ,Environmental Chemistry ,Ammonium ,Sulfate ,Amines ,0105 earth and related environmental sciences - Abstract
The effects of methylglyoxal uptake on the physical and optical properties of aerosol containing amines or ammonium sulfate were determined before and after cloud processing in a temperature- and RH-controlled chamber. The formation of brown carbon was observed upon methylglyoxal addition, detected as an increase in water-soluble organic carbon mass absorption coefficients below 370 nm and as a drop in single-scattering albedo at 450 nm. The imaginary refractive index component k450 reached a maximum value of 0.03 ± 0.009 with aqueous glycine aerosol particles. Browning of solid particles occurred at rates limited by chamber mixing (
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- 2017
14. Multiphase Photochemistry of Pyruvic Acid under Atmospheric Conditions
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Allison E. Reed Harris, Jean-François Doussin, Elizabeth C. Griffith, Aline Gratien, Mathieu Cazaunau, Anne Monod, Edouard Pangui, Aki Pajunoja, Annele Virtanen, Veronica Vaida, Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), Laboratoire Chimie de l'environnement (LCE), Aix Marseille Université (AMU)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), University of Eastern Finland, Centre National de la Recherche Scientifique (CNRS)-Aix Marseille Université (AMU)-Institut de Chimie du CNRS (INC), Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), and Centre National de la Recherche Scientifique (CNRS)-Aix Marseille Université (AMU)
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Aqueous solution ,010504 meteorology & atmospheric sciences ,Photodissociation ,010402 general chemistry ,Photochemistry ,01 natural sciences ,0104 chemical sciences ,Aerosol ,chemistry.chemical_compound ,Acetic acid ,chemistry ,13. Climate action ,Phase (matter) ,Carbon dioxide ,[SDE]Environmental Sciences ,[CHIM]Chemical Sciences ,Reactivity (chemistry) ,Pyruvic acid ,Physical and Theoretical Chemistry ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences - Abstract
Aerosol and molecular processing in the atmosphere occurs in a complex and variable environment consisting of multiple phases and interfacial regions. To explore the effects of such conditions on the reactivity of chemical systems, we employ an environmental simulation chamber to investigate the multiphase photolysis of pyruvic acid, which photoreacts in the troposphere in aqueous particles and in the gas phase. Upon irradiation of nebulized pyruvic acid, acetic acid and carbon dioxide are rapidly generated, which is consistent with previous literature on the bulk phase photolysis reactions. Additionally, we identify a new C6 product, zymonic acid, a species that has not previously been reported from pyruvic acid photolysis under any conditions. Its observation here, and corresponding spectroscopic signatures, indicates it could be formed by heterogeneous reactions at the droplet surface. Prior studies of the aqueous photolysis of pyruvic acid have shown that high-molecular-weight compounds are formed via...
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- 2017
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15. Experimental Study of the Formation of Organosulfates from α-Pinene Oxidation. Part I: Product Identification, Formation Mechanisms and Effect of Relative Humidity
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Houssni Lamkaddam, Aline Gratien, Emilie Perraudin, Geoffroy Duporté, Edouard Pangui, Pierre-Marie Flaud, Jean-François Doussin, Hélène Budzinski, Eric Villenave, Emmanuel Geneste, Sylvie Augagneur, UMR CNRS 5805 EPOC – OASU, Équipe LPTC, Université de Bordeaux, 351 Cours de la libération, 33405 Talence Cedex, France, and Université de Bordeaux (UB)
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chemistry.chemical_classification ,Pinene ,Ammonium sulfate ,010504 meteorology & atmospheric sciences ,Electrospray ionization ,Inorganic chemistry ,Oxide ,010501 environmental sciences ,Mass spectrometry ,01 natural sciences ,chemistry.chemical_compound ,chemistry ,Yield (chemistry) ,[SDE]Environmental Sciences ,Organic chemistry ,[CHIM]Chemical Sciences ,Volatile organic compound ,Physical and Theoretical Chemistry ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences ,Organosulfate - Abstract
In the present study, quasi-static reactor and atmospheric simulation chamber experiments were performed to investigate the formation of α-pinene-derived organosulfates. Organosulfates (R–OSO3H) were examined for the reactions between acidified ammonium sulfate particles exposed to an individual gaseous volatile organic compound, such as α-pinene and oxidized products (α-pinene oxide, isopinocampheol, pinanediol and myrtenal). Molecular structures were elucidated by liquid chromatography interfaced to high-resolution quadrupole time-of-flight mass spectrometry equipped with electrospray ionization (LC/ESI-HR-QTOFMS). New organosulfate products were detected and identified for the first time in the present study. Reaction with α-pinene oxide was found to be a favored pathway for organosulfate formation (C10H18O5S) and to yield organosulfate dimers (C20H34O6S and C20H34O9S2) and trimers (C30H50O10S2) under dry conditions (RH < 1%) and high particle acidity and precursor concentrations (1 ppm). The role of r...
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- 2016
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16. New Laboratory Intercomparison of the Ozone Absorption Coefficients in the Mid-infrared (10 μm) and Ultraviolet (300−350 nm) Spectral Regions
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Jean-Marie Flaud, Jean-François Doussin, Aline Gratien, Johannes Orphal, and Bénédicte Picquet-Varrault
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Ozone ,010304 chemical physics ,010504 meteorology & atmospheric sciences ,Mid infrared ,medicine.disease_cause ,Atmospheric sciences ,01 natural sciences ,chemistry.chemical_compound ,chemistry ,13. Climate action ,Spectroscopy, Fourier Transform Infrared ,0103 physical sciences ,medicine ,Spectrophotometry, Ultraviolet ,HITRAN ,Physical and Theoretical Chemistry ,Laboratories ,Absorption (electromagnetic radiation) ,Atmospheric ozone ,Ultraviolet ,0105 earth and related environmental sciences - Abstract
Knowing the ozone absorption cross sections in the ultraviolet and infrared spectral range, with an accuracy of better than 1%, is of the utmost importance for atmospheric remote-sensing applications. For this reason, various ozone intensity intercomparisons and measurements have been published these last years. However, the corresponding results proved not to be consistent and thus have raised a controversial discussion in the community of atmospheric remote-sensing. This study, where great care has been taken to avoid any possible error, reports a new laboratory intercomparison of the ozone absorption coefficients in the mid-infrared (10 μm) and ultraviolet (300-350 nm) spectral regions. It gives a new piece of information to the puzzling problem concerning the ozone IR and UV cross sections and confirms that the IR and UV cross sections recommended in the literature are in disagreement of about 4%.
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- 2010
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17. Absorption cross-sections of ozone in the ultraviolet and visible spectral regions: Status report 2015
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Viktor Gorshelev, Stanley P. Sander, Dimitris Balis, Michael C. Pitts, Georg Wagner, Michel Van Roozendael, Anna Serdyuchenko, Thierry Leblanc, Michael Petersen, Christophe Lerot, Philippe Moussay, Jean-Marie Flaud, Mark Weber, Bénédicte Picquet-Varrault, Alberto Redondas, Christof Janssen, Doug Degenstein, Alkiviadis F. Bais, Marie-Renée De Backer, Pepijn Veefkind, Aline Gratien, Edward Hare, Robert Wielgosz, Erkki Kyrölä, Alain Barbe, Pawan K. Bhartia, Gordon Labow, Tom McElroy, Claus Zehner, David Flittner, Geir O. Braathen, Xiong Liu, Matthias Schneider, Irina Petropavlovskikh, R. Evans, Sophie Godin-Beekmann, Johannes Staehelin, Joële Viallon, Maud Rotger-Languereau, Kelly Chance, Johannes Orphal, Maud Pastel, Camille Viatte, Anthony Cox, Johanna Tamminen, Richard D. McPeters, Manfred Birk, Thomas von Clarmann, James W. Burkholder, Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), Finnish Meteorological Institute (FMI), World Meteorological Organization (WMO), Groupe de spectrométrie moléculaire et atmosphérique (GSMA), Université de Reims Champagne-Ardenne (URCA)-Centre National de la Recherche Scientifique (CNRS), Laboratory of Atmospheric Physics [Thessaloniki], Aristotle University of Thessaloniki, NASA Goddard Space Flight Center (GSFC), German Aerospace Center (DLR), Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado [Boulder]-National Oceanic and Atmospheric Administration (NOAA), Harvard-Smithsonian Center for Astrophysics (CfA), Harvard University [Cambridge]-Smithsonian Institution, University of Cambridge [UK] (CAM), Institute of Space and Atmospheric Studies [Saskatoon] (ISAS), Department of Physics and Engineering Physics [Saskatoon], University of Saskatchewan [Saskatoon] (U of S)-University of Saskatchewan [Saskatoon] (U of S), Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), NASA Langley Research Center [Hampton] (LaRC), STRATO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), University of Bremen, Environment and Climate Change Canada, Laboratoire d'Etude du Rayonnement et de la Matière en Astrophysique (LERMA), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université de Cergy Pontoise (UCP), Université Paris-Seine-Université Paris-Seine-Centre National de la Recherche Scientifique (CNRS), Bureau International des Poids et Mesures (BIPM), Jet Propulsion Laboratory (JPL), California Institute of Technology (CALTECH)-NASA, Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB), Agencia Estatal de Meteorología (AEMet), Royal Netherlands Meteorological Institute (KNMI), California Institute of Technology (CALTECH), Institute of Environmental Physics [Bremen] (IUP), European Space Research Institute (ESRIN), European Space Agency (ESA), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich), Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Environment Canada (Toronto), École normale supérieure - Paris (ENS Paris)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Université de Cergy Pontoise (UCP), NASA-California Institute of Technology (CALTECH), Spanish State Meteorological Agency (AEMET), Jacquinet, Nicole, Flaud, Jean-Marie, Gamache, Robert R., Predoi-Cross, Adriana, Vander Auwera, Jean, Harvard University-Smithsonian Institution, École normale supérieure - Paris (ENS-PSL), and Agence Spatiale Européenne = European Space Agency (ESA)
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Ozone ,010504 meteorology & atmospheric sciences ,010501 environmental sciences ,Atmospheric sciences ,medicine.disease_cause ,01 natural sciences ,Absorption ,Atmosphere ,chemistry.chemical_compound ,Reference data ,medicine ,Physical and Theoretical Chemistry ,Experimentelle Verfahren ,Absorption (electromagnetic radiation) ,Spectroscopy ,0105 earth and related environmental sciences ,[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,Remote sensing ,Status report ,Atomic and Molecular Physics, and Optics ,Lidar ,Cross sections ,chemistry ,13. Climate action ,Atmospheric chemistry ,Environmental science ,Ultraviolet ,Atmospheric ozone - Abstract
The activity “Absorption Cross-Sections of Ozone” (ACSO) started in 2008 as a joint initiative of the International Ozone Commission (IO3C), the World Meteorological Organization (WMO) and the IGACO (“Integrated Global Atmospheric Chemistry Observations”) O3/UV subgroup to study, evaluate, and recommend the most suitable ozone absorption cross-section laboratory data to be used in atmospheric ozone measurements. The evaluation was basically restricted to ozone absorption cross-sections in the UV range with particular focus on the Huggins band. Up until now, the data of Bass and Paur published in 1985 (BP, 1985) are still officially recommended for such measurements. During the last decade it became obvious that BP (1985) cross-section data have deficits for use in advanced space-borne ozone measurements. At the same time, it was recognized that the origin of systematic differences in ground-based measurements of ozone required further investigation, in particular whether the BP (1985) cross-section data might contribute to these differences. In ACSO, different sets of laboratory ozone absorption cross-section data (including their dependence on temperature) of the group of Reims (France) (Brion et al., 1993, 1998, 1992, 1995, abbreviated as BDM, 1995) and those of Serdyuchenko et al. (2014), and Gorshelev et al. (2014), (abbreviated as SER, 2014) were examined for use in atmospheric ozone measurements in the Huggins band. In conclusion, ACSO recommends: (a) The spectroscopic data of BP (1985) should no longer be used for retrieval of atmospheric ozone measurements. (b) For retrieval of ground-based instruments of total ozone and ozone profile measurements by the Umkehr method performed by Brewer and Dobson instruments data of SER (2014) are recommended to be used. When SER (2014) is used, the difference between total ozone measurements of Brewer and Dobson instruments are very small and the difference between Dobson measurements at AD and CD wavelength pairs are diminished. (c) For ground-based Light Detection and Ranging (LIDAR) measurements the use of BDM (1995) or SER (2014) is recommended. (d) For satellite retrieval the presently widely used data of BDM (1995) should be used because SER (2014) seems less suitable for retrievals that use wavelengths close to 300 nm due to a deficiency in the signal-to-noise ratio in the SER (2014) dataset. The work of ACSO also showed: • The need to continue laboratory cross-section measurements of ozone of highest quality. The importance of careful characterization of the uncertainties of the laboratory measurements. • The need to extend the scope of such studies to other wavelength ranges (particularly to cover not only the Huggins band but also the comparison with the mid-infrared region). • The need for regular cooperation of experts in spectral laboratory measurements and specialists in atmospheric (ozone) measurements.
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- 2016
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18. Gaseous products and secondary organic aerosol formation during long term oxidation of isoprene and methacrolein
- Author
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Andrea Tapparo, F. Siekmann, Sylvain Ravier, Chiara Giorio, Mathieu Cazaunau, Edouard Pangui, Brice Temime-Roussel, J-F Doussin, Aline Gratien, Vincent Michoud, L. Bregonzio-Rozier, S. B. Morales, Anne Monod, Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Aix Marseille Université (AMU), Department of Chemistry [Cambridge, UK], University of Cambridge [UK] (CAM), Institut des Sciences Moléculaires (ISM), Université Montesquieu - Bordeaux 4-Université Sciences et Technologies - Bordeaux 1-École Nationale Supérieure de Chimie et de Physique de Bordeaux (ENSCPB)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Laboratoire Chimie de l'environnement (LCE), Aix Marseille Université (AMU)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Dipartimento di Scienze Chimiche [Padova], Università degli Studi di Padova = University of Padua (Unipd), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP), Universita degli Studi di Padova, Université Montesquieu - Bordeaux 4-Université Sciences et Technologies - Bordeaux 1 (UB)-École Nationale Supérieure de Chimie et de Physique de Bordeaux (ENSCPB)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Université Montesquieu - Bordeaux 4-Université Sciences et Technologies - Bordeaux 1-École Nationale Supérieure de Chimie et de Physique de Bordeaux (ENSCPB)-Centre National de la Recherche Scientifique (CNRS), Aix Marseille Université (AMU)-Centre National de la Recherche Scientifique (CNRS), Institut de Combustion, Aérothermique, Réactivité et Environnement (ICARE), and Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut des Sciences de l'Ingénierie et des Systèmes (INSIS)
- Subjects
Atmospheric Science ,Atmospheric Science, aerosol, smog chamber, SOA ,010504 meteorology & atmospheric sciences ,aerosol ,Chemistry ,Radical ,smog chamber ,Methacrolein ,010501 environmental sciences ,Photochemistry ,01 natural sciences ,lcsh:QC1-999 ,Product distribution ,Aerosol ,lcsh:Chemistry ,Atmosphere ,chemistry.chemical_compound ,lcsh:QD1-999 ,Mass spectrum ,SOA ,[CHIM]Chemical Sciences ,lcsh:Physics ,NOx ,Isoprene ,0105 earth and related environmental sciences - Abstract
First- and higher order-generation products formed from the oxidation of isoprene and methacrolein with OH radicals in the presence of NOx have been studied in a simulation chamber. Significant oxidation rates have been maintained for up to 7 h, allowing the study of highly oxidized products. Gas-phase product distribution and yields were obtained, and show good agreement with previous studies. Secondary organic aerosol (SOA) formation has also been investigated. SOA mass yields from previous studies show large discrepancies. The mass yields obtained here were consistent with the lowest values found in the literature, and more specifically in agreement with studies carried out with natural light or artificial lamps with emission similar to the solar spectrum. Differences in light source are therefore proposed to explain partially the discrepancies observed between different studies in the literature for both isoprene- and methacrolein-SOA mass yields. There is a high degree of similarity between the SOA mass spectra from isoprene and methacrolein photooxidation, thus strengthening the importance of the role of methacrolein in SOA formation from isoprene photooxidation under our experimental conditions (i.e., presence of NOx and long term oxidation). According to our results, SOA mass yields from both isoprene and methacrolein in the atmosphere could be lower than suggested by most of the current chamber studies.
- Published
- 2015
- Full Text
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