1
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Hao L, Li Z, Yli-Juuti T, Ylisirniö A, Pullinen I, Miettinen P, Xu W, Lehto VP, Worsnop DR, Virtanen A. Direct mitigation of secondary organic aerosol particulate pollutants by multiphase photocatalysis. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 923:171323. [PMID: 38438031 DOI: 10.1016/j.scitotenv.2024.171323] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/30/2023] [Revised: 02/05/2024] [Accepted: 02/26/2024] [Indexed: 03/06/2024]
Abstract
Particulate matter represents one of the most severe air pollutants globally. Organic aerosol (OA) comprises 30-70 % of submicron particle mass in urban areas. An effective way to mitigate OA particulate pollutants is to reduce the formation of secondary organic aerosol (SOA). Here, we studied the effect of titanium dioxide (TiO2) photocatalytic seeds on the formation and mitigation of SOA particles from α-pinene or toluene oxidation in chamber. For the first time, we discovered that under ultraviolet (UV) irradiation, the presence of TiO2 directly removed internally mixed α-pinene SOA mass by 53.7 % within 200 mins, and also directly removed SOA matter in an externally mixed state that is not in direct contact with TiO2 surface: the mass of externally mixed α-pinene SOA was reduced by 21.9 % within 81 mins, and the toluene SOA mass was reduced by 46.6 % in 145mins. In addition, the presence of TiO2 effectively inhibited the formation of SOA particles with a SOA mass yield of zero. This study brings up an innovative concept for air pollution control - the direct photocatalytic degradation of OA with aid of TiO2-based photocatalysts. Our novel findings will potentially bring practical applications in air pollution abatement and regional, even global aerosol-climate interactions.
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Affiliation(s)
- Liqing Hao
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland.
| | - Zijun Li
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
| | - Taina Yli-Juuti
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
| | - Arttu Ylisirniö
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
| | - Iida Pullinen
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
| | - Pasi Miettinen
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
| | - Wujun Xu
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
| | - Vesa-Pekka Lehto
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
| | - Douglas R Worsnop
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland; Department of Physics, University of Helsinki, P.O. 64, Finland; Aerodyne Research, Inc., Billerica, MA 08121-3976, USA
| | - Annele Virtanen
- Department of Technical Physics, University of Eastern Finland, Kuopio, Finland
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2
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Gerritz L, Wei J, Fang T, Wong C, Klodt AL, Nizkorodov SA, Shiraiwa M. Reactive Oxygen Species Formation and Peroxide and Carbonyl Decomposition in Aqueous Photolysis of Secondary Organic Aerosols. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2024; 58:4716-4726. [PMID: 38412378 DOI: 10.1021/acs.est.3c08662] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 02/29/2024]
Abstract
The mechanism and kinetics of reactive oxygen species (ROS) formation when atmospheric secondary organic aerosol (SOA) is exposed to solar radiation are poorly understood. In this study, we combined an in situ UV-vis irradiation system with electron paramagnetic resonance (EPR) spectroscopy to characterize the photolytic formation of ROS in aqueous extracts of SOA formed by the oxidation of isoprene, α-pinene, α-terpineol, and toluene. We observed substantial formation of free radicals, including •OH, superoxide (HO2•), and organic radicals (R•/RO•) upon irradiation. Compared to dark conditions, the radical yield was enhanced by a factor of ∼30 for •OH and by a factor of 2-10 for superoxide radicals, and we observed the emergence of organic radicals. Total peroxide measurements showed substantial decreases of peroxide contents after photoirradiation, indicating that organic peroxides can be an important source of the observed radicals. A liquid chromatography interfaced with high-resolution mass spectrometry was used to detect a number of organic radicals in the form of adducts with a spin trap, BMPO. The types of detected radicals and aqueous photolysis of model compounds indicated that photolysis of carbonyls by Norrish type I mechanisms plays an important role in the organic radical formation. The photolytic ROS formation serves as the driving force for cloud and fog processing of SOA.
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Affiliation(s)
- Lena Gerritz
- Department of Chemistry, University of California, Irvine, California 92697-2025, United States
| | - Jinlai Wei
- Department of Chemistry, University of California, Irvine, California 92697-2025, United States
| | - Ting Fang
- Department of Chemistry, University of California, Irvine, California 92697-2025, United States
- Sustainable Energy and Environment Thrust, The Hong Kong University of Science and Technology (Guangzhou), Nansha, Guangzhou, Guangdong 511400, China
| | - Cynthia Wong
- Department of Chemistry, University of California, Irvine, California 92697-2025, United States
| | - Alexandra L Klodt
- Department of Chemistry, University of California, Irvine, California 92697-2025, United States
| | - Sergey A Nizkorodov
- Department of Chemistry, University of California, Irvine, California 92697-2025, United States
| | - Manabu Shiraiwa
- Department of Chemistry, University of California, Irvine, California 92697-2025, United States
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3
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Kołodziejczyk A, Wróblewska A, Pietrzak M, Pyrcz P, Błaziak K, Szmigielski R. Dissociation constants of relevant secondary organic aerosol components in the atmosphere. CHEMOSPHERE 2024; 351:141166. [PMID: 38224752 DOI: 10.1016/j.chemosphere.2024.141166] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/07/2023] [Revised: 01/07/2024] [Accepted: 01/08/2024] [Indexed: 01/17/2024]
Abstract
The presented studies focus on measuring the determination of the acidity constant (pKa) of relevant secondary organic aerosol components. For our research, we selected important oxidation products (mainly carboxylic acids) of the most abundant terpene compounds, such as α-pinene, β-pinene, β-caryophyllene, and δ-3-carene. The research covered the synthesis and determination of the acidity constant of selected compounds. We used three methods to measure the acidity constant, i.e., 1H NMR titration, pH-metric titration, Bates-Schwarzenbach spectrophotometric method. Moreover, the pKa values were calculated with Marvin 21.17.0 software to compare the experimentally derived values with those calculated from the chemical structure. pKa values measured with 1H NMR titration ranged from 3.51 ± 0.01 for terebic acid to 5.18 ± 0.06 for β-norcaryophyllonic acid. Moreover, the data determined by the 1H NMR method revealed a good correlation with the data obtained with the commonly used potentiometric and UV-spectroscopic methods (R2 = 0.92). In contrast, the comparison with in silico results exhibits a relatively low correlation (R2Marvin = 0.66). We found that most of the values calculated with the Marvin Program are lower than experimental values obtained with pH-metric titration with an average difference of 0.44 pKa units. For di- and tricarboxylic acids, we obtained two and three pKa values, respectively. A good correlation with the literature values was observed, for example, Howell and Fisher (1958) used pH-metric titration and measured pKa1 and pKa2 to be 4.48 and 5.48, while our results are 4.24 ± 0.10 and 5.40 ± 0.02, respectively.
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Affiliation(s)
- Agata Kołodziejczyk
- Institute of Physical Chemistry, Polish Academy of Sciences, ul. Kasprzaka 44/52, 01-224, Warsaw, Poland.
| | - Aleksandra Wróblewska
- Institute of Physical Chemistry, Polish Academy of Sciences, ul. Kasprzaka 44/52, 01-224, Warsaw, Poland
| | - Mariusz Pietrzak
- Institute of Physical Chemistry, Polish Academy of Sciences, ul. Kasprzaka 44/52, 01-224, Warsaw, Poland
| | - Patryk Pyrcz
- Institute of Physical Chemistry, Polish Academy of Sciences, ul. Kasprzaka 44/52, 01-224, Warsaw, Poland
| | - Kacper Błaziak
- Faculty of Chemistry, University of Warsaw, ul. Pasteura 1, 01-224, Warsaw, Poland; Biological and Chemical Research Center, University of Warsaw, ul. Żwirki i Wigury 101, 01-224, Warsaw, Poland
| | - Rafał Szmigielski
- Institute of Physical Chemistry, Polish Academy of Sciences, ul. Kasprzaka 44/52, 01-224, Warsaw, Poland
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4
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Ling Z, Wu L, Wang Y, Shao M, Wang X, Huang W. Roles of semivolatile and intermediate-volatility organic compounds in secondary organic aerosol formation and its implication: A review. J Environ Sci (China) 2022; 114:259-285. [PMID: 35459491 DOI: 10.1016/j.jes.2021.08.055] [Citation(s) in RCA: 6] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/12/2021] [Revised: 08/31/2021] [Accepted: 08/31/2021] [Indexed: 06/14/2023]
Abstract
Secondary organic aerosol (SOA) is a very important component of fine particulate matter (PM2.5) in the atmosphere. However, the simulations of SOA, which could help to elucidate the detailed mechanism of SOA formation and quantify the roles of various precursors, remains unsatisfactory, as SOA levels are frequently underestimated. It has been found that the performance of SOA formation models can be significantly improved by incorporating the emission and evolution of semivolatile and intermediate-volatility organic compounds (S/IVOCs). In order to explore the roles of S/IVOCs in SOA formation, this study reviews some simulation models which could consider S/IVOCs for SOA formation as well as the development of emission inventories of S/IVOCs and S/IVOC modules for SOA formation. In addition, the future research directions for simulations of the effect of S/IVOCs on SOA formation are suggested.
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Affiliation(s)
- Zhenhao Ling
- School of Atmospheric Sciences, Sun Yat-sen University, Key Laboratory of Tropical Atmosphere-Ocean System, Ministry of Education, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China
| | - Liqing Wu
- School of Atmospheric Sciences, Sun Yat-sen University, Key Laboratory of Tropical Atmosphere-Ocean System, Ministry of Education, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China
| | - Yonghong Wang
- Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| | - Min Shao
- Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Institute for Environmental and Climate Research, Jinan University, Guangzhou 510632, China
| | - Xuemei Wang
- Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Institute for Environmental and Climate Research, Jinan University, Guangzhou 510632, China.
| | - Weiwen Huang
- School of Atmospheric Sciences, Sun Yat-sen University, Key Laboratory of Tropical Atmosphere-Ocean System, Ministry of Education, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China
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5
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D’Ambro EL, Hyttinen N, Møller KH, Iyer S, Otkjær RV, Bell DM, Liu J, Lopez-Hilfiker FD, Schobesberger S, Shilling JE, Zelenyuk A, Kjaergaard HG, Thornton JA, Kurtén T. Pathways to Highly Oxidized Products in the Δ3-Carene + OH System. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:2213-2224. [PMID: 35119266 PMCID: PMC8956127 DOI: 10.1021/acs.est.1c06949] [Citation(s) in RCA: 7] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/08/2023]
Abstract
Oxidation of the monoterpene Δ3-carene (C10H16) is a potentially important and understudied source of atmospheric secondary organic aerosol (SOA). We present chamber-based measurements of speciated gas and particle phases during photochemical oxidation of Δ3-carene. We find evidence of highly oxidized organic molecules (HOMs) in the gas phase and relatively low-volatility SOA dominated by C7-C10 species. We then use computational methods to develop the first stages of a Δ3-carene photochemical oxidation mechanism and explain some of our measured compositions. We find that alkoxy bond scission of the cyclohexyl ring likely leads to efficient HOM formation, in line with previous studies. We also find a surprising role for the abstraction of primary hydrogens from methyl groups, which has been calculated to be rapid in the α-pinene system, and suggest more research is required to determine if this is more general to other systems and a feature of autoxidation. This work develops a more comprehensive view of Δ3-carene photochemical oxidation products via measurements and lays out a suggested mechanism of oxidation via computationally derived rate coefficients.
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Affiliation(s)
- Emma L. D’Ambro
- Department
of Chemistry, University of Washington, Seattle, Washington 98195, United States
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
| | - Noora Hyttinen
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
- Institute
for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki FI-00014, Finland
| | - Kristian H. Møller
- Department
of Chemistry, University of Copenhagen, Copenhagen DK-2100, Denmark
| | - Siddharth Iyer
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
- Institute
for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki FI-00014, Finland
| | - Rasmus V. Otkjær
- Department
of Chemistry, University of Copenhagen, Copenhagen DK-2100, Denmark
| | - David M. Bell
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | - Jiumeng Liu
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | - Felipe D. Lopez-Hilfiker
- Department
of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - Siegfried Schobesberger
- Department
of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - John E. Shilling
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | - Alla Zelenyuk
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | | | - Joel A. Thornton
- Department
of Chemistry, University of Washington, Seattle, Washington 98195, United States
- Department
of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - Theo Kurtén
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
- Institute
for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki FI-00014, Finland
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6
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Allani A, Bedjanian Y, Papanastasiou DK, Romanias MN. Reaction Rate Coefficient of OH Radicals with d 9-Butanol as a Function of Temperature. ACS OMEGA 2021; 6:18123-18134. [PMID: 34308045 PMCID: PMC8296604 DOI: 10.1021/acsomega.1c01942] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 04/12/2021] [Accepted: 06/02/2021] [Indexed: 06/13/2023]
Abstract
d 9-Butanol or 1-butan-d 9-ol (D9B) is often used as an OH radical tracer in atmospheric chemistry studies to determine OH exposure, a useful universal metric that describes the extent of OH radical oxidation chemistry. Despite its frequent application, there is only one study that reports the rate coefficient of D9B with OH radicals, k 1(295 K), which limits its usefulness as an OH tracer for studying processes at temperatures lower or higher than room temperature. In this study, two complementary experimental techniques were used to measure the rate coefficient of D9B with OH radicals, k 1(T), at temperatures between 240 and 750 K and at pressures within 2-760 Torr. A thermally regulated atmospheric simulation chamber was used to determine k 1(T) in the temperature range of 263-353 K and at atmospheric pressure using the relative rate method. A low-pressure (2-10 Torr) discharge flow tube reactor coupled with a mass spectrometer was used to measure k 1(T) at temperatures within 240-750 K, using both the absolute and relative rate methods. The agreement between the two experimental aproaches followed in this study was very good, within 6%, in the overlapping temperature range, and k 1(295 ± 3 K) was 3.42 ± 0.26 × 10-12 cm3 molecule-1 s-1, where the quoted error is the overall uncertainty of the measurements. The temperature dependence of the rate coefficient is well described by the modified Arrhenius expression, k 1 = (1.57 ± 0.88) × 10-14 × (T/293)4.60±0.4 × exp(1606 ± 164/T) cm3 molecule-1 s-1 in the range of 240-750 K, where the quoted error represents the 2σ standard deviation of the fit. The results of the current study enable an accurate estimation of OH exposure in atmospheric simulation experiments and expand the applicability of D9B as an OH radical tracer at temperatures other than room temperature.
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Affiliation(s)
- Amira Allani
- IMT
Lille Douai, Univ. Lille, SAGE, Lille F-59000, France
| | - Yuri Bedjanian
- Institut
de Combustion, Aérothermique, Réactivité et Environnement
(ICARE), CNRS, Orléans Cedex
2 45071, France
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7
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Pospisilova V, Bell DM, Lamkaddam H, Bertrand A, Wang L, Bhattu D, Zhou X, Dommen J, Prevot ASH, Baltensperger U, El Haddad I, Slowik JG. Photodegradation of α-Pinene Secondary Organic Aerosol Dominated by Moderately Oxidized Molecules. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2021; 55:6936-6943. [PMID: 33961408 DOI: 10.1021/acs.est.0c06752] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
Atmospheric secondary organic aerosol (SOA) undergoes chemical and physical changes when exposed to UV radiation, affecting the atmospheric lifetime of the involved molecules. However, these photolytic processes remain poorly constrained. Here, we present a study aimed at characterizing, at a molecular level and in real time, the chemical composition of α-pinene SOA exposed to UV-A light at 50% relative humidity in an atmospheric simulation chamber. Significant SOA mass loss is observed at high loadings (∼100 μg m-3), whereas the effect is less prevalent at lower loadings (∼20 μg m-3). For the vast majority of molecules measured by the extractive electrospray time-of-flight mass spectrometer, there is a fraction that is photoactive and decays when exposed to UV-A radiation and a fraction that appears photorecalcitrant. The molecules that are most photoactive contain between 4 and 6 oxygen atoms, while the more highly oxygenated compounds and dimers do not exhibit significant decay. Overall, photolysis results in a reduction of the volatility of SOA, which cannot be explained by simple evaporative losses but requires either a change in volatility related to changes in functional groups or a change in physical parameters (i.e., viscosity).
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Affiliation(s)
- Veronika Pospisilova
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Tofwerk, 3600 Thun, Switzerland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Houssni Lamkaddam
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Amelie Bertrand
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Liwei Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Deepika Bhattu
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Department of Civil and Infrastructure Engineering, Indian Institute of Technology Jodhpur, Karwar 342037, India
| | - Xueqin Zhou
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Andre S H Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Jay G Slowik
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
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8
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Mofikoya AO, Yli-Pirilä P, Kivimäenpää M, Blande JD, Virtanen A, Holopainen JK. Deposition of α-pinene oxidation products on plant surfaces affects plant VOC emission and herbivore feeding and oviposition. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2020; 263:114437. [PMID: 32268226 DOI: 10.1016/j.envpol.2020.114437] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/22/2019] [Revised: 02/21/2020] [Accepted: 03/21/2020] [Indexed: 06/11/2023]
Abstract
White cabbage, Brassica oleracea, plants and artificial leaves covered with B. oleracea epicuticular wax were exposed to α-pinene and α-pinene oxidation products formed through the oxidation of α-pinene by ozone (O3) and hydroxyl (OH) radicals. O3 and OH-induced oxidation of α-pinene led to the formation of oxygenated volatile organic compounds (OVOCs) and secondary organic aerosol particles (SOA), referred to together as oxidation products (OP). Exposure of cabbage plants to O3 and OH-induced α-pinene OP led to the deposition and re-emission of gas-phase OP by exposed cabbage plants. In a series of 2-choice bioassays, the specialist cruciferous herbivore, Plutella xylostella adults deposited less eggs on artificial leaves exposed to α-pinene OP than on control plants exposed to clean filtered air. P. xylostella larvae did not show a specific feeding preference when offered leaves from different exposure treatments. However, the generalist Indian stick insect, Carausius morosus, fed more on control filtered air-exposed plants than on those exposed to α-pinene OP. Taken together, our results show that exposure to α-pinene oxidation products affects VOC emissions of B. oleracea and alters P. xylostella oviposition and C. morosus feeding responses.
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Affiliation(s)
- Adedayo O Mofikoya
- Department of Environmental and Biological Sciences, University of Eastern Finland, Kuopio, Finland.
| | - Pasi Yli-Pirilä
- Department of Environmental and Biological Sciences, University of Eastern Finland, Kuopio, Finland
| | - Minna Kivimäenpää
- Department of Environmental and Biological Sciences, University of Eastern Finland, Kuopio, Finland
| | - James D Blande
- Department of Environmental and Biological Sciences, University of Eastern Finland, Kuopio, Finland
| | - Annele Virtanen
- Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
| | - Jarmo K Holopainen
- Department of Environmental and Biological Sciences, University of Eastern Finland, Kuopio, Finland
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9
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Zawadowicz MA, Lee BH, Shrivastava M, Zelenyuk A, Zaveri RA, Flynn C, Thornton JA, Shilling JE. Photolysis Controls Atmospheric Budgets of Biogenic Secondary Organic Aerosol. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2020; 54:3861-3870. [PMID: 32154714 DOI: 10.1021/acs.est.9b07051] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/10/2023]
Abstract
Secondary organic aerosol (SOA) accounts for a large fraction of the tropospheric particulate matter. Although SOA production rates and mechanisms have been extensively investigated, loss pathways remain uncertain. Most large-scale chemistry and transport models account for mechanical deposition of SOA but not chemical losses such as photolysis. There is also a paucity of laboratory measurements of SOA photolysis, which limits how well photolytic losses can be modeled. Here, we show, through a combined experimental and modeling approach, that photolytic loss of SOA mass significantly alters SOA budget predictions. Using environmental chamber experiments at variable relative humidity between 0 and 60%, we find that SOA produced from several biogenic volatile organic compounds undergoes photolysis-induced mass loss at rates between 0 and 2.2 ± 0.4% of nitrogen dioxide (NO2) photolysis, equivalent to average atmospheric lifetimes as short as 10 h. We incorporate our photolysis rates into a regional chemical transport model to test the sensitivity of predicted SOA mass concentrations to photolytic losses. The addition of photolysis causes a ∼50% reduction in biogenic SOA loadings over the Amazon, indicating that photolysis exerts a substantial control over the atmospheric SOA lifetime, with a likely dependence upon the SOA molecular composition and thus production mechanisms.
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Affiliation(s)
- Maria A Zawadowicz
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Ben H Lee
- Department of Atmospheric Science, University of Washington, Seattle, Washington 98195, United States
| | - Manish Shrivastava
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Alla Zelenyuk
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Rahul A Zaveri
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Connor Flynn
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Joel A Thornton
- Department of Atmospheric Science, University of Washington, Seattle, Washington 98195, United States
| | - John E Shilling
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
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10
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Lee BH, D’Ambro EL, Lopez-Hilfiker FD, Schobesberger S, Mohr C, Zawadowicz MA, Liu J, Shilling JE, Hu W, Palm BB, Jimenez JL, Hao L, Virtanen A, Zhang H, Goldstein AH, Pye HOT, Thornton JA. Resolving ambient organic aerosol formation and aging pathways with simultaneous molecular composition and volatility observations. ACS EARTH & SPACE CHEMISTRY 2020; 4:391-402. [PMID: 32328536 PMCID: PMC7180062 DOI: 10.1021/acsearthspacechem.9b00302] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/15/2023]
Abstract
Organic aerosol (OA) constitutes a significant fraction of atmospheric fine particle mass. However, the precursors and chemical processes responsible for a majority of OA are rarely conclusively identified. We use online observations of hundreds of simultaneously measured molecular components obtained from 15 laboratory OA formation experiments with constraints on their effective saturation vapor concentrations to attribute the VOC precursors and subsequent chemical pathways giving rise to the vast majority of OA mass measured in two forested regions. We find that precursors and chemical pathways regulating OA composition and volatility are dynamic over hours to days, with their variations driven by coupled interactions between multiple oxidants. The extent of physical and photochemical aging, and its modulation by NOx, were key to a uniquely comprehensive combined composition-volatility description of OA. Our findings thus provide some of the most complete mechanistic-level guidance to the development of OA descriptions in air quality and Earth system models.
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Affiliation(s)
- Ben H. Lee
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, U.S.A
| | - Emma L. D’Ambro
- Department of Chemistry, University of Washington, Seattle, WA, U.S.A
| | | | | | - Claudia Mohr
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, U.S.A
| | - Maria A. Zawadowicz
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, U.S.A
| | - Jiumeng Liu
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, U.S.A
| | - John E. Shilling
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, U.S.A
| | - Weiwei Hu
- Cooperative Institute for Research in Environmental Sciences and Department of Chemistry, University of Colorado, Boulder, CO, U.S.A
| | - Brett B. Palm
- Cooperative Institute for Research in Environmental Sciences and Department of Chemistry, University of Colorado, Boulder, CO, U.S.A
| | - Jose L. Jimenez
- Cooperative Institute for Research in Environmental Sciences and Department of Chemistry, University of Colorado, Boulder, CO, U.S.A
| | - Liqing Hao
- Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
| | - Annele Virtanen
- Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
| | - Haofei Zhang
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, CA, U.S.A
| | - Allen H. Goldstein
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, CA, U.S.A
| | - Havala O. T. Pye
- Office of Research and Development, Environmental Protection Agency, Research Triangle, NC, U.S.A
| | - Joel A. Thornton
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, U.S.A
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11
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O'Brien RE, Kroll JH. Photolytic Aging of Secondary Organic Aerosol: Evidence for a Substantial Photo-Recalcitrant Fraction. J Phys Chem Lett 2019; 10:4003-4009. [PMID: 31264874 DOI: 10.1021/acs.jpclett.9b01417] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 06/09/2023]
Abstract
Photolytic aging has been proposed as a major mass loss mechanism for atmospheric secondary organic aerosol (SOA). However, estimated mass loss rates vary by orders of magnitude, and their impacts on modeled SOA loadings and properties are highly uncertain. In this study, photolysis rates and composition changes of α-pinene SOA are analyzed in situ over multiple days in an environmental chamber. After an initial exponential decay (τ ∼ 22 h), the mass loss rate slows dramatically, with more than ∼70-90% of the SOA particulate mass undergoing an essentially negligible photolytic degradation. Scaled to ambient conditions, SOA undergoes rapid photolysis over only its first day in the atmosphere; beyond this, the remaining SOA is photo-recalcitrant, and photolysis ceases to be a major sink compared to wet deposition time scales. Thus, extrapolation of the initial photolysis loss rate to the entire aerosol mass may significantly overestimate the role of photolysis in the removal of atmospheric SOA.
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Affiliation(s)
- Rachel E O'Brien
- Department of Chemistry , College of William and Mary , Williamsburg , Virginia 23185 , United States
- Department of Civil and Environmental Engineering , Massachusetts Institute of Technology , Cambridge , Massachusetts 02139 , United States
| | - Jesse H Kroll
- Department of Civil and Environmental Engineering , Massachusetts Institute of Technology , Cambridge , Massachusetts 02139 , United States
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12
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Sbai SE, Farida B. Photochemical aging and secondary organic aerosols generated from limonene in an oxidation flow reactor. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH INTERNATIONAL 2019; 26:18411-18420. [PMID: 31049860 DOI: 10.1007/s11356-019-05012-5] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/27/2018] [Accepted: 03/27/2019] [Indexed: 06/09/2023]
Abstract
Oxidation flow reactors (OFRs) are increasingly used to study the formation and evolution of secondary organic aerosols (SOA) in the atmosphere. The OH/HO2 and OH/O3 ratios in OFRs are similar to tropospheric ratios. In the present work, we investigated the production of SOA generated by OH oxydation and ozonolysis of limonene in OFR as a function of OH exposure and O3 exposure. The results are compared with those obtained from the simulation chambers. The precursor gas is exposed to OH concentrations ranging from 2.11 × 108 to 1.91 × 109 molec cm-3, with an estimated exposure time in the OFR of 137 s. In the environmental chambers, the precursor was oxidized using OH concentrations between 2.10 × 106 and 2.12 × 107 molec cm-3 over exposure times of several hours. In the overlapping OH exposure region, the highest SOA yields are obtained in the OFR, which is explained by the ozonolysis of limonene in the OFR. However, the yields decrease with the increase of OHexp in both systems.
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Affiliation(s)
- Salah Eddine Sbai
- Université Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON,2 Avenue Albert Einstein, 69100, Lyon, France.
- Department of physics, Laboratoires de physique des hauts Energies Modélisation et Simulation, Mohammed V University in Rabat, Rabat, Morocco.
| | - Bentayeb Farida
- Department of physics, Laboratoires de physique des hauts Energies Modélisation et Simulation, Mohammed V University in Rabat, Rabat, Morocco
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13
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Bianchi F, Kurtén T, Riva M, Mohr C, Rissanen MP, Roldin P, Berndt T, Crounse JD, Wennberg PO, Mentel TF, Wildt J, Junninen H, Jokinen T, Kulmala M, Worsnop DR, Thornton JA, Donahue N, Kjaergaard HG, Ehn M. Highly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol. Chem Rev 2019; 119:3472-3509. [PMID: 30799608 PMCID: PMC6439441 DOI: 10.1021/acs.chemrev.8b00395] [Citation(s) in RCA: 240] [Impact Index Per Article: 48.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/21/2023]
Abstract
![]()
Highly
oxygenated organic molecules (HOM) are formed in the atmosphere
via autoxidation involving peroxy radicals arising from volatile organic
compounds (VOC). HOM condense on pre-existing particles and can be
involved in new particle formation. HOM thus contribute to the formation
of secondary organic aerosol (SOA), a significant and ubiquitous component
of atmospheric aerosol known to affect the Earth’s radiation
balance. HOM were discovered only very recently, but the interest
in these compounds has grown rapidly. In this Review, we define HOM
and describe the currently available techniques for their identification/quantification,
followed by a summary of the current knowledge on their formation
mechanisms and physicochemical properties. A main aim is to provide
a common frame for the currently quite fragmented literature on HOM
studies. Finally, we highlight the existing gaps in our understanding
and suggest directions for future HOM research.
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Affiliation(s)
- Federico Bianchi
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland.,Aerosol and Haze Laboratory , University of Chemical Technology , Beijing 100029 , P.R. China
| | - Theo Kurtén
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland
| | - Matthieu Riva
- IRCELYON, CNRS University of Lyon , Villeurbanne 69626 , France
| | - Claudia Mohr
- Department of Environmental Science and Analytical Chemistry , Stockholm University , Stockholm 11418 , Sweden
| | - Matti P Rissanen
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland
| | - Pontus Roldin
- Division of Nuclear Physics, Department of Physics , Lund University , Lund 22100 , Sweden
| | - Torsten Berndt
- Leibniz Institute for Tropospheric Research , Leipzig 04318 , Germany
| | - John D Crounse
- Division of Geological and Planetary Sciences , California Institute of Technology , Pasadena , California 91125 , United States
| | - Paul O Wennberg
- Division of Geological and Planetary Sciences , California Institute of Technology , Pasadena , California 91125 , United States
| | - Thomas F Mentel
- Institut für Energie und Klimaforschung, IEK-8 , Forschungszentrum Jülich GmbH , Jülich 52425 , Germany
| | - Jürgen Wildt
- Institut für Energie und Klimaforschung, IEK-8 , Forschungszentrum Jülich GmbH , Jülich 52425 , Germany
| | - Heikki Junninen
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland.,Institute of Physics , University of Tartu , Tartu 50090 , Estonia
| | - Tuija Jokinen
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland.,Aerosol and Haze Laboratory , University of Chemical Technology , Beijing 100029 , P.R. China
| | - Douglas R Worsnop
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland.,Aerodyne Research Inc. , Billerica , Massachusetts 01821 , United States
| | - Joel A Thornton
- Department of Atmospheric Sciences , University of Washington , Seattle , Washington 98195 , United States
| | - Neil Donahue
- Center for Atmospheric Particle Studies , Carnegie Mellon University , Pittsburgh , Pennsylvania 15213 , United States
| | - Henrik G Kjaergaard
- Department of Chemistry , University of Cøpenhagen , Cøpenhagen 2100 , Denmark
| | - Mikael Ehn
- Institute for Atmospheric and Earth System Research, Faculty of Science , University of Helsinki , Helsinki 00014 , Finland
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14
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Arroyo PC, Malecha KT, Ammann M, Nizkorodov SA. Influence of humidity and iron(iii) on photodegradation of atmospheric secondary organic aerosol particles. Phys Chem Chem Phys 2018; 20:30021-30031. [PMID: 30480278 DOI: 10.1039/c8cp03981j] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
The absorption of solar actinic radiation by atmospheric secondary organic aerosol (SOA) particles drives condensed-phase photochemical processes, which lead to particle mass loss by the production of CO, CO2, hydrocarbons, and various oxygenated volatile organic compounds (OVOCs). We examined the influence of relative humidity (RH) and Fe(iii) content on the OVOC release and subsequent mass loss from secondary organic aerosol material (SOM) during UV irradiation. The samples were generated in a flow tube reactor from the oxidation of d-limonene by ozone. The SOM was collected with a Micro Orifice Uniform Deposit Impactor (MOUDI) on CaF2 windows. To selected samples, a variable amount of FeCl3 was added before irradiation. The resulting SOM samples, with or without added FeCl3, were irradiated with a 305 nm light-emitting diode and the release of several OVOCs, including acetic acid, acetone, formic acid and acetaldehyde, was measured with a Proton Transfer Reaction Time-of-Flight Mass Spectrometer (PTR-ToF-MS). The release of OVOCs from photodegradation of SOM at typical ambient mid-values of RH (30-70%) was 2-4 times higher than under dry conditions. The release of OVOCs was slightly enhanced in the presence of low concentrations of iron (0.04 Fe molar ratio) but it was suppressed at higher concentrations (0.50 Fe molar ratio) of iron indicating the existence of a complicated radical chemistry driving the photodegradation of SOM. Our findings suggest that the presence of iron in atmospheric aerosol particles will either increase or decrease release of OVOCs due to the photodegradation of SOM depending on whether the relative iron concentration is low or high, respectively. At atmospherically relevant RH conditions, the expected fractional mass loss induced by these photochemical processes from limonene SOA particles would be between 2 and 4% of particle mass per hour. Therefore, photodegradation is an important aging mechanism for this type of SOA.
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Affiliation(s)
- Pablo Corral Arroyo
- Paul Scherrer Institute, Laboratory of Environmental Chemistry, 5232 Villigen PSI, Switzerland
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15
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Leong YJ, Sanchez NP, Wallace HW, Karakurt Cevik B, Hernandez CS, Han Y, Flynn JH, Massoli P, Floerchinger C, Fortner EC, Herndon S, Bean JK, Hildebrandt Ruiz L, Jeon W, Choi Y, Lefer B, Griffin RJ. Overview of surface measurements and spatial characterization of submicrometer particulate matter during the DISCOVER-AQ 2013 campaign in Houston, TX. JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION (1995) 2017; 67:854-872. [PMID: 28278029 DOI: 10.1080/10962247.2017.1296502] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/25/2016] [Accepted: 01/18/2017] [Indexed: 06/06/2023]
Abstract
UNLABELLED The sources of submicrometer particulate matter (PM1) remain poorly characterized in the industrialized city of Houston, TX. A mobile sampling approach was used to characterize PM1 composition and concentration across Houston based on high-time-resolution measurements of nonrefractory PM1 and trace gases during the DISCOVER-AQ Texas 2013 campaign. Two pollution zones with marked differences in PM1 levels, character, and dynamics were established based on cluster analysis of organic aerosol mass loadings sampled at 16 sites. The highest PM1 mass concentrations (average 11.6 ± 5.7 µg/m3) were observed to the northwest of Houston (zone 1), dominated by secondary organic aerosol (SOA) mass likely driven by nighttime biogenic organonitrate formation. Zone 2, an industrial/urban area south/east of Houston, exhibited lower concentrations of PM1 (average 4.4 ± 3.3 µg/m3), significant organic aerosol (OA) aging, and evidence of primary sulfate emissions. Diurnal patterns and backward-trajectory analyses enable the classification of airmass clusters characterized by distinct PM sources: biogenic SOA, photochemical aged SOA, and primary sulfate emissions from the Houston Ship Channel. Principal component analysis (PCA) indicates that secondary biogenic organonitrates primarily related with monoterpenes are predominant in zone 1 (accounting for 34% of the variability in the data set). The relevance of photochemical processes and industrial and traffic emission sources in zone 2 also is highlighted by PCA, which identifies three factors related with these processes/sources (~50% of the aerosol/trace gas concentration variability). PCA reveals a relatively minor contribution of isoprene to SOA formation in zone 1 and the absence of isoprene-derived aerosol in zone 2. The relevance of industrial amine emissions and the likely contribution of chloride-displaced sea salt aerosol to the observed variability in pollution levels in zone 2 also are captured by PCA. IMPLICATIONS This article describes an urban-scale mobile study to characterize spatial variations in submicrometer particulate matter (PM1) in greater Houston. The data set indicates substantial spatial variations in PM1 sources/chemistry and elucidates the importance of photochemistry and nighttime oxidant chemistry in producing secondary PM1. These results emphasize the potential benefits of effective control strategies throughout the region, not only to reduce primary emissions of PM1 from automobiles and industry but also to reduce the emissions of important secondary PM1 precursors, including sulfur oxides, nitrogen oxides, ammonia, and volatile organic compounds. Such efforts also could aid in efforts to reduce mixing ratios of ozone.
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Affiliation(s)
- Y J Leong
- a Department of Civil and Environmental Engineering , Rice University , Houston , TX , USA
| | - N P Sanchez
- a Department of Civil and Environmental Engineering , Rice University , Houston , TX , USA
| | - H W Wallace
- a Department of Civil and Environmental Engineering , Rice University , Houston , TX , USA
| | - B Karakurt Cevik
- a Department of Civil and Environmental Engineering , Rice University , Houston , TX , USA
| | - C S Hernandez
- a Department of Civil and Environmental Engineering , Rice University , Houston , TX , USA
| | - Y Han
- a Department of Civil and Environmental Engineering , Rice University , Houston , TX , USA
| | - J H Flynn
- b Department of Earth and Atmospheric Sciences , University of Houston , Houston , TX , USA
| | - P Massoli
- c Aerodyne Research, Inc ., Billerica , MA , USA
| | | | - E C Fortner
- c Aerodyne Research, Inc ., Billerica , MA , USA
| | - S Herndon
- c Aerodyne Research, Inc ., Billerica , MA , USA
| | - J K Bean
- d McKetta Department of Chemical Engineering , University of Texas at Austin , Austin , TX , USA
| | - L Hildebrandt Ruiz
- d McKetta Department of Chemical Engineering , University of Texas at Austin , Austin , TX , USA
| | - W Jeon
- b Department of Earth and Atmospheric Sciences , University of Houston , Houston , TX , USA
| | - Y Choi
- b Department of Earth and Atmospheric Sciences , University of Houston , Houston , TX , USA
| | - B Lefer
- b Department of Earth and Atmospheric Sciences , University of Houston , Houston , TX , USA
| | - R J Griffin
- a Department of Civil and Environmental Engineering , Rice University , Houston , TX , USA
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16
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Malecha KT, Nizkorodov SA. Feasibility of Photosensitized Reactions with Secondary Organic Aerosol Particles in the Presence of Volatile Organic Compounds. J Phys Chem A 2017; 121:4961-4967. [PMID: 28598172 DOI: 10.1021/acs.jpca.7b04066] [Citation(s) in RCA: 15] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Abstract
The ability of a complex mixture of organic compounds found in secondary organic aerosol (SOA) to act as a photosensitizer in the oxidation of volatile organic compounds (VOCs) was investigated. Different types of SOAs were produced in a smog chamber by oxidation of various biogenic and anthropogenic VOCs. The SOA particles were collected from the chamber onto an inert substrate, and the resulting material was exposed to 365 nm radiation in an air flow containing ∼200 ppbv of limonene vapor. The mixing ratio of limonene and other VOCs in the flow was observed with a proton transfer reaction time-of-flight mass spectrometer (PTR-ToF-MS). The photosensitized uptake of limonene was observed for several SOA materials, with a lower limit for the reactive uptake coefficient on the scale of ∼10-5. The lower limit for the uptake coefficient under conditions of Los Angeles, California on the summer solstice at noon was estimated to be on the order of ∼10-6. Photoproduction of oxygenated VOCs (OVOCs) resulting from photodegradation of the SOA material also occurred in parallel with the photosensitized uptake of limonene. The estimated photosensitized limonene uptake rates by atmospheric SOA particles and vegetation surfaces appear to be too small to compete with the atmospheric oxidation of limonene by the hydroxyl radical or ozone. However, these processes could play a role in the leaf boundary layer where concentrations of oxidants are depleted and concentrations of VOCs are enhanced relative to the free atmosphere.
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Affiliation(s)
- Kurtis T Malecha
- Department of Chemistry, University of California , Irvine, California 92697-2025, United States
| | - Sergey A Nizkorodov
- Department of Chemistry, University of California , Irvine, California 92697-2025, United States
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17
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Jathar SH, Woody M, Pye HOT, Baker KR, Robinson AL. Chemical transport model simulations of organic aerosol in southern California: model evaluation and gasoline and diesel source contributions. ATMOSPHERIC CHEMISTRY AND PHYSICS 2017; 17:4305-4318. [PMID: 30079083 PMCID: PMC6070158 DOI: 10.5194/acp-17-4305-2017] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/05/2023]
Abstract
Gasoline- and diesel-fueled engines are ubiquitous sources of air pollution in urban environments. They emit both primary particulate matter and precursor gases that react to form secondary particulate matter in the atmosphere. In this work, we updated the organic aerosol module and organic emissions inventory of a three-dimensional chemical transport model, the Community Multiscale Air Quality Model (CMAQ), using recent, experimentally derived inputs and parameterizations for mobile sources. The updated model included a revised volatile organic compound (VOC) speciation for mobile sources and secondary organic aerosol (SOA) formation from unspeciated intermediate volatility organic compounds (IVOCs). The updated model was used to simulate air quality in southern California during May and June 2010, when the California Research at the Nexus of Air Quality and Climate Change (CalNex) study was conducted. Compared to the Traditional version of CMAQ, which is commonly used for regulatory applications, the updated model did not significantly alter the predicted organic aerosol (OA) mass concentrations but did substantially improve predictions of OA sources and composition (e.g., POA-SOA split), as well as ambient IVOC concentrations. The updated model, despite substantial differences in emissions and chemistry, performed similar to a recently released research version of CMAQ (Woody et al., 2016) that did not include the updated VOC and IVOC emissions and SOA data. Mobile sources were predicted to contribute 30-40 % of the OA in southern California (half of which was SOA), making mobile sources the single largest source contributor to OA in southern California. The remainder of the OA was attributed to non-mobile anthropogenic sources (e.g., cooking, biomass burning) with biogenic sources contributing to less than 5 % to the total OA. Gasoline sources were predicted to contribute about 13 times more OA than diesel sources; this difference was driven by differences in SOA production. Model predictions highlighted the need to better constrain multi-generational oxidation reactions in chemical transport models.
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Affiliation(s)
- Shantanu H. Jathar
- Mechanical Engineering, Colorado State University, Fort Collins, CO 80525, USA
| | - Matthew Woody
- US Environmental Protection Agency, Research Triangle Park, NC 27711, USA
| | - Havala O. T. Pye
- US Environmental Protection Agency, Research Triangle Park, NC 27711, USA
| | - Kirk R. Baker
- US Environmental Protection Agency, Research Triangle Park, NC 27711, USA
| | - Allen L. Robinson
- Mechanical Engineering, Carnegie Mellon University, Pittsburgh, PA 15213, USA
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18
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19
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Malecha KT, Nizkorodov SA. Photodegradation of Secondary Organic Aerosol Particles as a Source of Small, Oxygenated Volatile Organic Compounds. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2016; 50:9990-7. [PMID: 27547987 DOI: 10.1021/acs.est.6b02313] [Citation(s) in RCA: 29] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/10/2023]
Abstract
We investigated the photodegradation of secondary organic aerosol (SOA) particles by near-UV radiation and photoproduction of oxygenated volatile organic compounds (OVOCs) from various types of SOA. We used a smog chamber to generate SOA from α-pinene, guaiacol, isoprene, tetradecane, and 1,3,5-trimethylbenzene under high-NOx, low-NOx, or ozone oxidation conditions. The SOA particles were collected on a substrate, and the resulting material was exposed to several mW of near-UV radiation (λ ∼ 300 nm) from a light-emitting diode. Various OVOCs, including acetic acid, formic acid, acetaldehyde, and acetone were observed during photodegradation, and their SOA-mass-normalized fluxes were estimated with a Proton Transfer Reaction Time-of-Flight Mass Spectrometer (PTR-ToF-MS). All the SOA, with the exception of guaiacol SOA, emitted OVOCs upon irradiation. Based on the measured OVOC emission rates, we estimate that SOA particles would lose at least ∼1% of their mass over a 24 h period during summertime conditions in Los Angeles, California. This condensed-phase photochemical process may produce a few Tg/year of gaseous formic acid, the amount comparable to its primary sources. The condensed-phase SOA photodegradation processes could therefore measurably affect the budgets of both particulate and gaseous atmospheric organic compounds on a global scale.
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Affiliation(s)
- Kurtis T Malecha
- Department of Chemistry, University of California , Irvine, California 92697, United States
| | - Sergey A Nizkorodov
- Department of Chemistry, University of California , Irvine, California 92697, United States
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20
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Riva M, Budisulistiorini SH, Chen Y, Zhang Z, D'Ambro EL, Zhang X, Gold A, Turpin BJ, Thornton JA, Canagaratna MR, Surratt JD. Chemical Characterization of Secondary Organic Aerosol from Oxidation of Isoprene Hydroxyhydroperoxides. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2016; 50:9889-99. [PMID: 27466979 DOI: 10.1021/acs.est.6b02511] [Citation(s) in RCA: 45] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/03/2023]
Abstract
Atmospheric oxidation of isoprene under low-NOx conditions leads to the formation of isoprene hydroxyhydroperoxides (ISOPOOH). Subsequent oxidation of ISOPOOH largely produces isoprene epoxydiols (IEPOX), which are known secondary organic aerosol (SOA) precursors. Although SOA from IEPOX has been previously examined, systematic studies of SOA characterization through a non-IEPOX route from 1,2-ISOPOOH oxidation are lacking. In the present work, SOA formation from the oxidation of authentic 1,2-ISOPOOH under low-NOx conditions was systematically examined with varying aerosol compositions and relative humidity. High yields of highly oxidized compounds, including multifunctional organosulfates (OSs) and hydroperoxides, were chemically characterized in both laboratory-generated SOA and fine aerosol samples collected from the southeastern U.S. IEPOX-derived SOA constituents were observed in all experiments, but their concentrations were only enhanced in the presence of acidified sulfate aerosol, consistent with prior work. High-resolution aerosol mass spectrometry (HR-AMS) reveals that 1,2-ISOPOOH-derived SOA formed through non-IEPOX routes exhibits a notable mass spectrum with a characteristic fragment ion at m/z 91. This laboratory-generated mass spectrum is strongly correlated with a factor recently resolved by positive matrix factorization (PMF) of aerosol mass spectrometer data collected in areas dominated by isoprene emissions, suggesting that the non-IEPOX pathway could contribute to ambient SOA measured in the Southeastern United States.
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Affiliation(s)
- Matthieu Riva
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599 United States
| | - Sri H Budisulistiorini
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599 United States
| | - Yuzhi Chen
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599 United States
| | - Zhenfa Zhang
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599 United States
| | - Emma L D'Ambro
- Department of Atmospheric Sciences, University of Washington , Seattle, Washington 98195 United States
| | - Xuan Zhang
- Center for Aerosol and Cloud Chemistry, Aerodyne Research , Billerica, Massachusetts 01821 United States
| | - Avram Gold
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599 United States
| | - Barbara J Turpin
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599 United States
| | - Joel A Thornton
- Department of Atmospheric Sciences, University of Washington , Seattle, Washington 98195 United States
| | - Manjula R Canagaratna
- Center for Aerosol and Cloud Chemistry, Aerodyne Research , Billerica, Massachusetts 01821 United States
| | - Jason D Surratt
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599 United States
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21
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Huang M, Zhang J, Cai S, Liao Y, Zhao W, Hu C, Gu X, Fang L, Zhang W. Characterization of particulate products for aging of ethylbenzene secondary organic aerosol in the presence of ammonium sulfate seed aerosol. J Environ Sci (China) 2016; 47:219-229. [PMID: 27593289 DOI: 10.1016/j.jes.2015.11.033] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/08/2015] [Revised: 11/15/2015] [Accepted: 11/27/2015] [Indexed: 06/06/2023]
Abstract
Aging of secondary organic aerosol (SOA) particles formed from OH- initiated oxidation of ethylbenzene in the presence of high mass (100-300μg/m(3)) concentrations of (NH4)2SO4 seed aerosol was investigated in a home-made smog chamber in this study. The chemical composition of aged ethylbenzene SOA particles was measured using an aerosol laser time-of-flight mass spectrometer (ALTOFMS) coupled with a Fuzzy C-Means (FCM) clustering algorithm. Experimental results showed that nitrophenol, ethyl-nitrophenol, 2,4-dinitrophenol, methyl glyoxylic acid, 5-ethyl-6-oxo-2,4-hexadienoic acid, 2-ethyl-2,4-hexadiendioic acid, 2,3-dihydroxy-5-ethyl-6-oxo-4-hexenoic acid, 1H-imidazole, hydrated N-glyoxal substituted 1H-imidazole, hydrated glyoxal dimer substituted imidazole, 1H-imidazole-2-carbaldehyde, N-glyoxal substituted hydrated 1H-imidazole-2-carbaldehyde and high-molecular-weight (HMW) components were the predominant products in the aged particles. Compared to the previous aromatic SOA aging studies, imidazole compounds, which can absorb solar radiation effectively, were newly detected in aged ethylbenzene SOA in the presence of high concentrations of (NH4)2SO4 seed aerosol. These findings provide new information for discussing aromatic SOA aging mechanisms.
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Affiliation(s)
- Mingqiang Huang
- College of Chemistry & Environment, Minnan Normal University, Zhangzhou 363000, China; Fujian Province Key Laboratory of Modern Analytical Science and Separation Technology, Zhangzhou 363000, China; Department of Environmental Science and Engineering, Xiamen University, Tan Kah Kee College, Zhangzhou 363105, China.
| | - Jiahui Zhang
- College of Chemistry & Environment, Minnan Normal University, Zhangzhou 363000, China
| | - Shunyou Cai
- College of Chemistry & Environment, Minnan Normal University, Zhangzhou 363000, China; Fujian Province Key Laboratory of Modern Analytical Science and Separation Technology, Zhangzhou 363000, China
| | - Yingmin Liao
- Department of Environmental Science and Engineering, Xiamen University, Tan Kah Kee College, Zhangzhou 363105, China
| | - Weixiong Zhao
- Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, China
| | - Changjin Hu
- Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, China
| | - Xuejun Gu
- Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, China
| | - Li Fang
- Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, China
| | - Weijun Zhang
- Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, China.
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22
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Ye P, Ding X, Ye Q, Robinson ES, Donahue NM. Uptake of Semivolatile Secondary Organic Aerosol Formed from α-Pinene into Nonvolatile Polyethylene Glycol Probe Particles. J Phys Chem A 2016; 120:1459-67. [DOI: 10.1021/acs.jpca.5b07435] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
- Penglin Ye
- Center
for Atmospheric Particle Studies, Carnegie Mellon University, 5000
Forbes Avenue, Pittsburgh, Pennsylvania 15213, United States
| | - Xiang Ding
- Center
for Atmospheric Particle Studies, Carnegie Mellon University, 5000
Forbes Avenue, Pittsburgh, Pennsylvania 15213, United States
- State
Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Qing Ye
- Center
for Atmospheric Particle Studies, Carnegie Mellon University, 5000
Forbes Avenue, Pittsburgh, Pennsylvania 15213, United States
| | - Ellis S. Robinson
- Center
for Atmospheric Particle Studies, Carnegie Mellon University, 5000
Forbes Avenue, Pittsburgh, Pennsylvania 15213, United States
| | - Neil M. Donahue
- Center
for Atmospheric Particle Studies, Carnegie Mellon University, 5000
Forbes Avenue, Pittsburgh, Pennsylvania 15213, United States
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23
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Nah T, Sanchez J, Boyd CM, Ng NL. Photochemical Aging of α-pinene and β-pinene Secondary Organic Aerosol formed from Nitrate Radical Oxidation. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2016; 50:222-231. [PMID: 26618657 DOI: 10.1021/acs.est.5b04594] [Citation(s) in RCA: 33] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/05/2023]
Abstract
The nitrate radical (NO3) is the dominant nighttime oxidant in most urban and rural environments and reacts rapidly with biogenic volatile organic compounds to form secondary organic aerosol (SOA) and organic nitrates (ON). Here, we study the formation of SOA and ON from the NO3 oxidation of two monoterpenes (α-pinene and β-pinene) and investigate how they evolve during photochemical aging. High SOA mass loadings are produced in the NO3+β-pinene reaction, during which we detected 41 highly oxygenated gas- and particle-phase ON possessing 4 to 9 oxygen atoms. The fraction of particle-phase ON in the β-pinene SOA remains fairly constant during photochemical aging. In contrast to the NO3+β-pinene reaction, low SOA mass loadings are produced during the NO3+α-pinene reaction, during which only 5 highly oxygenated gas- and particle-phase ON are detected. The majority of the particle-phase ON evaporates from the α-pinene SOA during photochemical aging, thus exhibiting a drastically different behavior from that of β-pinene SOA. Our results indicate that nighttime ON formed by NO3+monoterpene chemistry can serve as either permanent or temporary NOx sinks depending on the monoterpene precursor.
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Affiliation(s)
- Theodora Nah
- School of Chemical and Biomolecular Engineering, Georgia Institute of Technology , Atlanta, Georgia 30332, United States
| | - Javier Sanchez
- School of Chemical and Biomolecular Engineering, Georgia Institute of Technology , Atlanta, Georgia 30332, United States
| | - Christopher M Boyd
- School of Chemical and Biomolecular Engineering, Georgia Institute of Technology , Atlanta, Georgia 30332, United States
| | - Nga Lee Ng
- School of Chemical and Biomolecular Engineering, Georgia Institute of Technology , Atlanta, Georgia 30332, United States
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology , Atlanta, Georgia 30332, United States
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24
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Daumit KE, Carrasquillo AJ, Sugrue RA, Kroll JH. Effects of Condensed-Phase Oxidants on Secondary Organic Aerosol Formation. J Phys Chem A 2015; 120:1386-94. [DOI: 10.1021/acs.jpca.5b06160] [Citation(s) in RCA: 22] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- Kelly E. Daumit
- Department
of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, 02139, United States
| | - Anthony J. Carrasquillo
- Department
of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, 02139, United States
| | - Rebecca A. Sugrue
- Department
of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, 02139, United States
| | - Jesse H. Kroll
- Department
of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, 02139, United States
- Department
of Chemical Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, 02139, United States
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25
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George C, Ammann M, D’Anna B, Donaldson DJ, Nizkorodov S. Heterogeneous photochemistry in the atmosphere. Chem Rev 2015; 115:4218-58. [PMID: 25775235 PMCID: PMC4772778 DOI: 10.1021/cr500648z] [Citation(s) in RCA: 279] [Impact Index Per Article: 31.0] [Reference Citation Analysis] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/14/2014] [Indexed: 02/06/2023]
Affiliation(s)
- Christian George
- Université
de Lyon 1, Lyon F-69626, France
- CNRS, UMR5256,
IRCELYON, Institut de Recherches sur la Catalyse et
l’Environnement de Lyon, Villeurbanne F-69626, France
| | - Markus Ammann
- Laboratory
of Radiochemistry and Environmental Chemistry, Paul Scherrer Institut, 5232 Villigen, Switzerland
| | - Barbara D’Anna
- Université
de Lyon 1, Lyon F-69626, France
- CNRS, UMR5256,
IRCELYON, Institut de Recherches sur la Catalyse et
l’Environnement de Lyon, Villeurbanne F-69626, France
| | - D. J. Donaldson
- Department
of Chemistry and Department of Physical & Environmental Sciences, University of Toronto, Toronto, Ontario M5S 3H6, Canada
| | - Sergey
A. Nizkorodov
- Department
of Chemistry, University of California, Irvine, California 92697, United States
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26
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Riva M, Robinson ES, Perraudin E, Donahue NM, Villenave E. Photochemical aging of secondary organic aerosols generated from the photooxidation of polycyclic aromatic hydrocarbons in the gas-phase. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2015; 49:5407-5416. [PMID: 25856309 DOI: 10.1021/acs.est.5b00442] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/04/2023]
Abstract
Aging processes of secondary organic aerosol (SOA) may be a source of oxygenated organic aerosols; however, the chemical processes involved remain unclear. In this study, we investigate photochemical aging of SOA produced by the gas-phase oxidation of naphthalene by hydroxyl radicals and acenaphthylene by ozone. We monitored the SOA composition using a high-resolution time-of-flight aerosol mass spectrometer. We initiated SOA aging with UV photolysis alone and with OH radicals in the presence or absence of light and at different NOx levels. For naphthalene, the organic composition of the particulate phase seems to be dominated by highly oxidized compounds such as carboxylic acids, and aging data may be consistent with diffusion limitations. For acenaphthylene, the fate of oxidized products and the moderately oxidized aerosol seem to indicate that functionalization reactions might be the main aging process were initiated by the cumulative effect of light and OH radicals.
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Affiliation(s)
- Matthieu Riva
- †University of Bordeaux, EPOC, UMR 5805, F-33405 Talence cedex, France
- ‡CNRS, EPOC, UMR 5805, F-33405 Talence cedex, France
| | - Ellis S Robinson
- §Center for Atmospheric Particles Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Emilie Perraudin
- †University of Bordeaux, EPOC, UMR 5805, F-33405 Talence cedex, France
- ‡CNRS, EPOC, UMR 5805, F-33405 Talence cedex, France
| | - Neil M Donahue
- §Center for Atmospheric Particles Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Eric Villenave
- †University of Bordeaux, EPOC, UMR 5805, F-33405 Talence cedex, France
- ‡CNRS, EPOC, UMR 5805, F-33405 Talence cedex, France
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27
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Wong JPS, Zhou S, Abbatt JPD. Changes in Secondary Organic Aerosol Composition and Mass due to Photolysis: Relative Humidity Dependence. J Phys Chem A 2014; 119:4309-16. [DOI: 10.1021/jp506898c] [Citation(s) in RCA: 56] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/14/2022]
Affiliation(s)
| | - Shouming Zhou
- Department of Chemistry, University of Toronto, Toronto, Canada
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28
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Emanuelsson EU, Mentel TF, Watne AK, Spindler C, Bohn B, Brauers T, Dorn HP, Hallquist AM, Häseler R, Kiendler-Scharr A, Müller KP, Pleijel H, Rohrer F, Rubach F, Schlosser E, Tillmann R, Hallquist M. Parameterization of thermal properties of aging secondary organic aerosol produced by photo-oxidation of selected terpene mixtures. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2014; 48:6168-6176. [PMID: 24810838 DOI: 10.1021/es405412p] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/03/2023]
Abstract
Formation and evolution of secondary organic aerosols (SOA) from biogenic VOCs influences the Earth's radiative balance. We have examined the photo-oxidation and aging of boreal terpene mixtures in the SAPHIR simulation chamber. Changes in thermal properties and chemical composition, deduced from mass spectrometric measurements, were providing information on the aging of biogenic SOA produced under ambient solar conditions. Effects of precursor mixture, concentration, and photochemical oxidation levels (OH exposure) were evaluated. OH exposure was found to be the major driver in the long term photochemical transformations, i.e., reaction times of several hours up to days, of SOA and its thermal properties, whereas the initial concentrations and terpenoid mixtures had only minor influence. The volatility distributions were parametrized using a sigmoidal function to determine TVFR0.5 (the temperature yielding a 50% particle volume fraction remaining) and the steepness of the volatility distribution. TVFR0.5 increased by 0.3±0.1% (ca. 1 K), while the steepness increased by 0.9±0.3% per hour of 1×10(6) cm(-3) OH exposure. Thus, aging reduces volatility and increases homogeneity of the vapor pressure distribution, presumably because highly volatile fractions become increasingly susceptible to gas phase oxidation, while less volatile fractions are less reactive with gas phase OH.
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Affiliation(s)
- Eva U Emanuelsson
- Atmospheric Science, Department of Chemistry and Molecular Biology, University of Gothenburg , Gothenburg S-405 30, Sweden
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29
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Donahue NM, Ortega IK, Chuang W, Riipinen I, Riccobono F, Schobesberger S, Dommen J, Baltensperger U, Kulmala M, Worsnop DR, Vehkamaki H. How do organic vapors contribute to new-particle formation? Faraday Discuss 2014; 165:91-104. [PMID: 24600998 DOI: 10.1039/c3fd00046j] [Citation(s) in RCA: 51] [Impact Index Per Article: 5.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
Highly oxidised organic vapors can effectively stabilize sulphuric acid in heteronuclear clusters and drive new-particle formation. We present quantum chemical calculations of cluster stability, showing that multifunctional species can stabilize sulphuric acid and also present additional polar functional groups for subsequent cluster growth. We also model the multi-generation oxidation of vapors associated with secondary organic aerosol formation using a two-dimensional volatility basis set. The steady-state saturation ratios and absolute concentrations of extremely low volatility products are sufficient to drive new-particle formation with sulphuric acid at atmospherically relevant rates.
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Affiliation(s)
- Neil M Donahue
- Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave., Pittsburgh, PA, USA.
| | - Ismael K Ortega
- Division of Atmospheric Science, Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland
| | - Wayne Chuang
- Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave., Pittsburgh, PA, USA
| | - Ilona Riipinen
- Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave., Pittsburgh, PA, USA
| | - Francesco Riccobono
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232 Villigen, Switzerland
| | - Siegfried Schobesberger
- Division of Atmospheric Science, Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland
| | - Josef Dommen
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232 Villigen, Switzerland
| | - Urs Baltensperger
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232 Villigen, Switzerland
| | - Markku Kulmala
- Division of Atmospheric Science, Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland
| | | | - Hanna Vehkamaki
- Division of Atmospheric Science, Department of Physics, University of Helsinki, FI-00014 Helsinki, Finland
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30
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Xu L, Kollman MS, Song C, Shilling JE, Ng NL. Effects of NOx on the volatility of secondary organic aerosol from isoprene photooxidation. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2014; 48:2253-62. [PMID: 24471688 DOI: 10.1021/es404842g] [Citation(s) in RCA: 35] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/24/2023]
Abstract
The effects of NOx on the volatility of the secondary organic aerosol (SOA) formed from isoprene photooxidation are investigated in environmental chamber experiments. Two types of experiments are performed. In HO2-dominant experiments, organic peroxy radicals (RO2) primarily react with HO2. In mixed experiments, RO2 reacts through multiple pathways, including with NO, NO2, and HO2. The volatility and oxidation state of isoprene SOA are sensitive to and exhibit a nonlinear dependence on NOx levels. Depending on the NOx levels, the SOA formed in mixed experiments can be of similar or lower volatility compared to that formed in HO2-dominant experiments. The dependence of SOA yield, volatility, and oxidation state on the NOx level likely arises from gas-phase RO2 chemistry and succeeding particle-phase oligomerization reactions. The NOx level also plays a strong role in SOA aging. While the volatility of SOA in mixed experiments does not change substantially over time, SOA becomes less volatile and more oxidized as oxidation progresses in HO2-dominant experiments.
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Affiliation(s)
- Lu Xu
- School of Chemical and Biomolecular Engineering, Georgia Institute of Technology , Atlanta, Georgia 30332, United States
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31
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Lignell H, Epstein SA, Marvin MR, Shemesh D, Gerber B, Nizkorodov S. Experimental and Theoretical Study of Aqueous cis-Pinonic Acid Photolysis. J Phys Chem A 2013; 117:12930-45. [DOI: 10.1021/jp4093018] [Citation(s) in RCA: 47] [Impact Index Per Article: 4.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- Hanna Lignell
- Department
of Chemistry, University of California, Irvine, California 92697-2025, United States
- Laboratory of Physical Chemistry, University of Helsinki, P.O. Box 55, FIN-00014 Helsinki, Finland
| | - Scott A. Epstein
- Department
of Chemistry, University of California, Irvine, California 92697-2025, United States
| | - Margaret R. Marvin
- Department
of Chemistry, University of California, Irvine, California 92697-2025, United States
| | - Dorit Shemesh
- Institute of Chemistry and The Fritz Haber Research Center, The Hebrew University, Jerusalem 91904, Israel
| | - Benny Gerber
- Department
of Chemistry, University of California, Irvine, California 92697-2025, United States
- Laboratory of Physical Chemistry, University of Helsinki, P.O. Box 55, FIN-00014 Helsinki, Finland
- Institute of Chemistry and The Fritz Haber Research Center, The Hebrew University, Jerusalem 91904, Israel
| | - Sergey Nizkorodov
- Department
of Chemistry, University of California, Irvine, California 92697-2025, United States
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32
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Qi L, Nakao S, Cocker DR. Aging of secondary organic aerosol from alpha-pinene ozonolysis: roles of hydroxyl and nitrate radicals. JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION (1995) 2012; 62:1359-1369. [PMID: 23362755 DOI: 10.1080/10962247.2012.712082] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/01/2023]
Abstract
UNLABELLED This work investigates the oxidative aging of preformed secondary organic aerosol (SOA) derived from alpha-pinene ozonolysis (-100 ppb(v) hydrocarbon [HC(x)] with excess of O3) within the University of California-Riverside Center for Environmental Research and Technology environmental chamber that occurs after introduction of additional hydroxyl (OH) and nitrate (NO3) radicals. Simultaneous measurements of SOA volume concentration, hygroscopicity, particle density, and elemental chemical composition (C:O:H) reveal increased particle wall-loss-corrected SOA formation (1.5%, 7.5%, and 15.1%), increase in oxygen-to-carbon ratio (O/C; 15.6%, 8.7%, and 8.7%), and hydrophilicity (4.2%, 7.4%, and 1.4%) after addition of NO (ultraviolet [UV] on), H2O2 (UV(on)), and N2O5 (dark), respectively. The processing observed as an increase in O/C and hydrophilicity is attributed to OH and NO3 reactions with first-generation vapor products and UV photolysis. The rate of increase in O/C appears to be only sufficient to achieve semivolatile oxygenated organic aerosol (SV-OOA) on a day time scale even at the raised chamber radical concentrations. The additional processing with UV irradiation without addition of NO, H2O2, or N2O5 is observed, adding 5.5% wall-loss-corrected volume. The photolysis-only processing is attributed to additional OH generated from photolysis of the nitrous acid (HONO) offgasing from chamber walls. This finding indicates that OH and NO3 radicals can further alter the chemical composition of SOA from alpha-pinene ozonolysis, which is proved to consist of first-generation products. IMPLICATIONS Secondary organic aerosol (SOA) may undergo aging processes once formed in the atmosphere, thereby altering the physicochemical and toxic properties of aerosol. This study discusses SOA aging of a major biogenic volatile organic compound (VOC; alpha-pinene) after it initially forms SOA. Aging of the alpha-pinene ozonolysis system by OH (through NO or H2O2 injection), NO3 (through N2O5 injection), and photolysis is observed. Although the reaction rate appears to be only sufficient to achieve semivolatile oxygenated organic aerosol (SV-OOA) level of oxygenation on a 1-day scale, it is important that SOA aging be considered in ambient air quality models. Aging in this study is attributed to further oxidation of gas-phase oxidation products of alpha-pinene ozonolysis.
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Affiliation(s)
- Li Qi
- Department of Chemical and Environmental Engineering, Bourns College of Engineering, Center for Environmental Research and Technology (CE-CERT), University of California, Riverside, California, USA.
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33
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Montenegro A, Ishibashi JSA, Lam P, Li Z. Kinetics Study of Reactions of α-Pinene and β-Pinene with Hydroxyl Radical at 1–8 Torr and 240–340 K Using the Relative Rate/Discharge Flow/Mass Spectrometry Method. J Phys Chem A 2012; 116:12096-103. [DOI: 10.1021/jp307718m] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/03/2023]
Affiliation(s)
- Anthony Montenegro
- Department of Chemistry and Biochemistry, California State University—Fullerton, Fullerton,
California 92834, United States
| | - Jacob S. A. Ishibashi
- Department of Chemistry and Biochemistry, California State University—Fullerton, Fullerton,
California 92834, United States
| | - Phuong Lam
- Department of Chemistry and Biochemistry, California State University—Fullerton, Fullerton,
California 92834, United States
| | - Zhuangjie Li
- Department of Chemistry and Biochemistry, California State University—Fullerton, Fullerton,
California 92834, United States
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34
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Henry KM, Lohaus T, Donahue NM. Organic aerosol yields from α-pinene oxidation: bridging the gap between first-generation yields and aging chemistry. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2012; 46:12347-12354. [PMID: 23088520 DOI: 10.1021/es302060y] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/01/2023]
Abstract
Secondary organic aerosol formation from volatile precursors can be thought of as a succession of generations of reaction products. Here, we constrain first-generation SOA formation from the α-pinene + OH reaction and also study SOA formation from α-pinene ozonolysis carried out without an OH scavenger. SOA yields from OH oxidation of α-pinene are significantly higher than SOA yields from ozonolysis including an OH scavenger, and the SOA mass yields for unscavenged ozonolysis generally fall within the range of mass yields for α-pinene ozonolysis under various conditions. Taken together, first-generation product yields parametrized with a volatility basis set fit provide a starting point for atmospheric models designed to simulate both the production and subsequent aging of SOA from this important terpene.
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Affiliation(s)
- Kaytlin M Henry
- Carnegie Mellon University Department of Chemical Engineering, 5000 Forbes Ave Pittsburgh, Pennsylvania 15213, USA
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35
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Chacon-Madrid HJ, Murphy BN, Pandis SN, Donahue NM. Simulations of smog-chamber experiments using the two-dimensional volatility basis set: linear oxygenated precursors. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2012; 46:11179-11186. [PMID: 22970932 DOI: 10.1021/es3017232] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/01/2023]
Abstract
We use a two-dimensional volatility basis set (2D-VBS) box model to simulate secondary organic aerosol (SOA) mass yields of linear oxygenated molecules: n-tridecanal, 2- and 7-tridecanone, 2- and 7-tridecanol, and n-pentadecane. A hybrid model with explicit, a priori treatment of the first-generation products for each precursor molecule, followed by a generic 2D-VBS mechanism for later-generation chemistry, results in excellent model-measurement agreement. This strongly confirms that the 2D-VBS mechanism is a predictive tool for SOA modeling but also suggests that certain important first-generation products for major primary SOA precursors should be treated explicitly for optimal SOA predictions.
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Affiliation(s)
- Heber J Chacon-Madrid
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA 15213, USA
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36
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Aging of biogenic secondary organic aerosol via gas-phase OH radical reactions. Proc Natl Acad Sci U S A 2012; 109:13503-8. [PMID: 22869714 DOI: 10.1073/pnas.1115186109] [Citation(s) in RCA: 92] [Impact Index Per Article: 7.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
The Multiple Chamber Aerosol Chemical Aging Study (MUCHACHAS) tested the hypothesis that hydroxyl radical (OH) aging significantly increases the concentration of first-generation biogenic secondary organic aerosol (SOA). OH is the dominant atmospheric oxidant, and MUCHACHAS employed environmental chambers of very different designs, using multiple OH sources to explore a range of chemical conditions and potential sources of systematic error. We isolated the effect of OH aging, confirming our hypothesis while observing corresponding changes in SOA properties. The mass increases are consistent with an existing gap between global SOA sources and those predicted in models, and can be described by a mechanism suitable for implementation in those models.
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