1
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Zhao B, Donahue NM, Zhang K, Mao L, Shrivastava M, Ma PL, Shen J, Wang S, Sun J, Gordon H, Tang S, Fast J, Wang M, Gao Y, Yan C, Singh B, Li Z, Huang L, Lou S, Lin G, Wang H, Jiang J, Ding A, Nie W, Qi X, Chi X, Wang L. Global variability in atmospheric new particle formation mechanisms. Nature 2024; 631:98-105. [PMID: 38867037 PMCID: PMC11222162 DOI: 10.1038/s41586-024-07547-1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/21/2023] [Accepted: 05/09/2024] [Indexed: 06/14/2024]
Abstract
A key challenge in aerosol pollution studies and climate change assessment is to understand how atmospheric aerosol particles are initially formed1,2. Although new particle formation (NPF) mechanisms have been described at specific sites3-6, in most regions, such mechanisms remain uncertain to a large extent because of the limited ability of atmospheric models to simulate critical NPF processes1,7. Here we synthesize molecular-level experiments to develop comprehensive representations of 11 NPF mechanisms and the complex chemical transformation of precursor gases in a fully coupled global climate model. Combined simulations and observations show that the dominant NPF mechanisms are distinct worldwide and vary with region and altitude. Previously neglected or underrepresented mechanisms involving organics, amines, iodine oxoacids and HNO3 probably dominate NPF in most regions with high concentrations of aerosols or large aerosol radiative forcing; such regions include oceanic and human-polluted continental boundary layers, as well as the upper troposphere over rainforests and Asian monsoon regions. These underrepresented mechanisms also play notable roles in other areas, such as the upper troposphere of the Pacific and Atlantic oceans. Accordingly, NPF accounts for different fractions (10-80%) of the nuclei on which cloud forms at 0.5% supersaturation over various regions in the lower troposphere. The comprehensive simulation of global NPF mechanisms can help improve estimation and source attribution of the climate effects of aerosols.
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Affiliation(s)
- Bin Zhao
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China.
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing, China.
- Pacific Northwest National Laboratory, Richland, WA, USA.
| | - Neil M Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Engineering and Public Policy, Carnegie Mellon University, Pittsburgh, PA, USA
| | - Kai Zhang
- Pacific Northwest National Laboratory, Richland, WA, USA
| | - Lizhuo Mao
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China
| | | | - Po-Lun Ma
- Pacific Northwest National Laboratory, Richland, WA, USA
| | - Jiewen Shen
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China
| | - Shuxiao Wang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing, China
| | - Jian Sun
- National Center for Atmospheric Research, Boulder, CO, USA
| | - Hamish Gordon
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USA
| | - Shuaiqi Tang
- Pacific Northwest National Laboratory, Richland, WA, USA
| | - Jerome Fast
- Pacific Northwest National Laboratory, Richland, WA, USA
| | - Mingyi Wang
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - Yang Gao
- Key Laboratory of Marine Environment and Ecology, Ministry of Education, Ocean University of China, Qingdao, China
| | - Chao Yan
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | | | - Zeqi Li
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China
| | - Lyuyin Huang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China
| | - Sijia Lou
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Guangxing Lin
- Pacific Northwest National Laboratory, Richland, WA, USA
- College of Ocean and Earth Sciences, Xiamen University, Xiamen, China
| | - Hailong Wang
- Pacific Northwest National Laboratory, Richland, WA, USA
| | - Jingkun Jiang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing, China
| | - Aijun Ding
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Wei Nie
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Ximeng Qi
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Xuguang Chi
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Lin Wang
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), Department of Environmental Science and Engineering, Fudan University, Shanghai, China
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2
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Brean J, Rowell A, Beddows DC, Weinhold K, Mettke P, Merkel M, Tuch T, Rissanen M, Maso MD, Kumar A, Barua S, Iyer S, Karppinen A, Wiedensohler A, Shi Z, Harrison RM. Road Traffic Emissions Lead to Much Enhanced New Particle Formation through Increased Growth Rates. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2024; 58:10664-10674. [PMID: 38850427 PMCID: PMC11191591 DOI: 10.1021/acs.est.3c10526] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/13/2023] [Revised: 05/23/2024] [Accepted: 05/24/2024] [Indexed: 06/10/2024]
Abstract
New particle formation (NPF) is a major source of atmospheric aerosol particles, including cloud condensation nuclei (CCN), by number globally. Previous research has highlighted that NPF is less frequent but more intense at roadsides compared to urban background. Here, we closely examine NPF at both background and roadside sites in urban Central Europe. We show that the concentration of oxygenated organic molecules (OOMs) is greater at the roadside, and the condensation of OOMs along with sulfuric acid onto new particles is sufficient to explain the growth at both sites. We identify a hitherto unreported traffic-related OOM source contributing 29% and 16% to total OOMs at the roadside and background, respectively. Critically, this hitherto undiscovered OOM source is an essential component of urban NPF. Without their contribution to growth rates and the subsequent enhancements to particle survival, the number of >50 nm particles produced by NPF would be reduced by a factor of 21 at the roadside site. Reductions to hydrocarbon emissions from road traffic may thereby reduce particle numbers and CCN counts.
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Affiliation(s)
- James Brean
- Division
of Environmental Health and Risk Management, School of Geography,
Earth and Environmental Sciences, University
of Birmingham, Birmingham B15 2TT, United Kingdom
| | - Alex Rowell
- Division
of Environmental Health and Risk Management, School of Geography,
Earth and Environmental Sciences, University
of Birmingham, Birmingham B15 2TT, United Kingdom
| | - David C.S. Beddows
- Division
of Environmental Health and Risk Management, School of Geography,
Earth and Environmental Sciences, University
of Birmingham, Birmingham B15 2TT, United Kingdom
| | - Kay Weinhold
- Leibniz
Institute for Tropospheric Research, Leipzig 04318, Germany
| | - Peter Mettke
- Leibniz
Institute for Tropospheric Research, Leipzig 04318, Germany
| | - Maik Merkel
- Leibniz
Institute for Tropospheric Research, Leipzig 04318, Germany
| | - Thomas Tuch
- Leibniz
Institute for Tropospheric Research, Leipzig 04318, Germany
| | - Matti Rissanen
- Aerosol
Physics laboratory, Tampere University, Tampere 33720, Finland
| | - Miikka Dal Maso
- Aerosol
Physics laboratory, Tampere University, Tampere 33720, Finland
| | - Avinash Kumar
- Aerosol
Physics laboratory, Tampere University, Tampere 33720, Finland
| | - Shawon Barua
- Aerosol
Physics laboratory, Tampere University, Tampere 33720, Finland
| | - Siddharth Iyer
- Aerosol
Physics laboratory, Tampere University, Tampere 33720, Finland
| | | | | | - Zongbo Shi
- Division
of Environmental Health and Risk Management, School of Geography,
Earth and Environmental Sciences, University
of Birmingham, Birmingham B15 2TT, United Kingdom
| | - Roy M. Harrison
- Division
of Environmental Health and Risk Management, School of Geography,
Earth and Environmental Sciences, University
of Birmingham, Birmingham B15 2TT, United Kingdom
- Department
of Environmental Sciences, Faculty of Meteorology, Environment and
Arid Land Agriculture, King Abdulaziz University, Jeddah 21589, Saudi Arabia
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3
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Cai R, Mikkilä J, Bengs A, Koirala M, Mikkilä J, Holm S, Juuti P, Meder M, Partovi F, Shcherbinin A, Worsnop D, Ehn M, Kangasluoma J. Extending the Range of Detectable Trace Species with the Fast Polarity Switching of Chemical Ionization Orbitrap Mass Spectrometry. Anal Chem 2024; 96:8604-8612. [PMID: 38691094 DOI: 10.1021/acs.analchem.4c00650] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 05/03/2024]
Abstract
Chemical ionization (CI) atmospheric pressure interface mass spectrometry is a unique analytical technique for its low detection limits, softness to preserve molecular information, and selectivity for particular classes of species. Here, we present a fast polarity switching approach for highly sensitive online analysis of a wide range of trace species in complex samples using selective CI chemistries and high-resolution mass spectrometry. It is achieved by successfully coupling a multischeme chemical ionization inlet (MION) and an Orbitrap Fourier transform mass spectrometer. The capability to flexibly combine ionization chemistries from both polarities effectively extends the detectability compared to using only one ionization chemistry, as commonly used positive and negative reagent ions tend to be sensitive to different classes of species. We tested the performance of the MION-Orbitrap using reactive gaseous organic species generated by α-pinene ozonolysis in an environmental chamber and a standard mixture of 71 pesticides. Diethylammonium and nitrate are used as reagent ions in positive and negative polarities. We show that with a mass resolving power of 280,000, the MION-Orbitrap can switch and measure both polarities within 1 min, which is sufficiently fast and stable to follow the temporal evolution of reactive organic species and the thermal desorption profile of pesticides. We detected 23 of the 71 pesticides in the mixture using only nitrate as the reagent ion. Facilitated by polarity switching, we also detected 47 pesticides using diethylammonium, improving the total number of detected species to 59. For reactive organic species generated by α-pinene ozonolysis, we show that combining diethylammonium and nitrate addresses the need to measure oxygenated molecules in atmospheric environments with a wide range of oxidation states. These results indicate that the polarity switching MION-Orbitrap can promisingly serve as a versatile tool for the nontargeted chemical analysis of trace species in various applications.
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Affiliation(s)
- Runlong Cai
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), Department of Environmental Science & Engineering, Fudan University, 200438 Shanghai, China
| | - Joona Mikkilä
- Karsa Ltd., A. I. Virtasen aukio 1, 00560 Helsinki, Finland
| | - Anna Bengs
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Mrisha Koirala
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Jyri Mikkilä
- Karsa Ltd., A. I. Virtasen aukio 1, 00560 Helsinki, Finland
| | - Sebastian Holm
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Paxton Juuti
- Karsa Ltd., A. I. Virtasen aukio 1, 00560 Helsinki, Finland
| | - Melissa Meder
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Fariba Partovi
- Karsa Ltd., A. I. Virtasen aukio 1, 00560 Helsinki, Finland
- Faculty of Engineering and Natural Sciences, Tampere University, 33720 Tampere, Finland
| | | | - Douglas Worsnop
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, United States
| | - Mikael Ehn
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Juha Kangasluoma
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Karsa Ltd., A. I. Virtasen aukio 1, 00560 Helsinki, Finland
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4
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Huang W, Junninen H, Garmash O, Lehtipalo K, Stolzenburg D, Lampilahti JLP, Ezhova E, Schallhart S, Rantala P, Aliaga D, Ahonen L, Sulo J, Quéléver LLJ, Cai R, Alekseychik P, Mazon SB, Yao L, Blichner SM, Zha Q, Mammarella I, Kirkby J, Kerminen VM, Worsnop DR, Kulmala M, Bianchi F. Potential pre-industrial-like new particle formation induced by pure biogenic organic vapors in Finnish peatland. SCIENCE ADVANCES 2024; 10:eadm9191. [PMID: 38569045 PMCID: PMC10990286 DOI: 10.1126/sciadv.adm9191] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/14/2023] [Accepted: 02/28/2024] [Indexed: 04/05/2024]
Abstract
Pure biogenic new particle formation (NPF) induced by highly oxygenated organic molecules (HOMs) could be an important mechanism for pre-industrial aerosol formation. However, it has not been unambiguously confirmed in the ambient due to the scarcity of truly pristine continental locations in the present-day atmosphere or the lack of chemical characterization of NPF precursors. Here, we report ambient observations of pure biogenic HOM-driven NPF over a peatland in southern Finland. Meteorological decoupling processes formed an "air pocket" (i.e., a very shallow surface layer) at night and favored NPF initiated entirely by biogenic HOM from this peatland, whose atmospheric environment closely resembles that of the pre-industrial era. Our study sheds light on pre-industrial aerosol formation, which represents the baseline for estimating the impact of present and future aerosol on climate, as well as on future NPF, the features of which may revert toward pre-industrial-like conditions due to air pollution mitigation.
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Affiliation(s)
- Wei Huang
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Heikki Junninen
- Institute of Physics, University of Tartu, Tartu 50411, Estonia
| | - Olga Garmash
- Aerosol Physics Laboratory, Physics Unit, Tampere University, Tampere 33720, Finland
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
- Atmospheric Composition Unit, Finnish Meteorological Institute, Helsinki 00101, Finland
| | | | - Janne L. P. Lampilahti
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Ekaterina Ezhova
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Simon Schallhart
- Atmospheric Composition Unit, Finnish Meteorological Institute, Helsinki 00101, Finland
| | - Pekka Rantala
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Diego Aliaga
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Lauri Ahonen
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Juha Sulo
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Lauriane L. J. Quéléver
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Runlong Cai
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Pavel Alekseychik
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
- Bioeconomy and Environment, Natural Resources Institute Finland, Helsinki 00790, Finland
| | - Stephany B. Mazon
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Lei Yao
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), Department of Environmental Science & Engineering, Fudan University, Shanghai 200438, China
| | - Sara M. Blichner
- Department of Environmental Science, Stockholm University, Stockholm 11418, Sweden
- Bolin Centre for Climate Research, Stockholm University, Stockholm 11418, Sweden
| | - Qiaozhi Zha
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
| | - Ivan Mammarella
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Jasper Kirkby
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
- CERN, the European Organization for Nuclear Research, CH-1211 Geneve 23, Switzerland
| | - Veli-Matti Kerminen
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Douglas R. Worsnop
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
- Aerodyne Research Inc., Billerica, MA 01821, USA
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
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5
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Zhang H, Wang J, Dong B, Xu F, Liu H, Zhang Q, Zong W, Shi X. New mechanism for the participation of aromatic oxidation products in atmospheric nucleation. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 917:170487. [PMID: 38296079 DOI: 10.1016/j.scitotenv.2024.170487] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/15/2023] [Revised: 01/03/2024] [Accepted: 01/24/2024] [Indexed: 02/03/2024]
Abstract
Oxygenated organic molecules (OOMs) are recognized as important precursors for new particle formation (NPF) in the urban atmosphere. The paper theoretically studied the formation of OOMs by styrene oxidation processes initiated by OH radicals, focusing on the OOMs nucleation mechanism. The results found that in the presence of an H2SO4 molecule, lowly oxygenated organic molecules containing a benzene ring (LOMBs) can form stable clusters and grow to the scale of a critical nucleus through pi-pi stacking and OH hydrogen bonding. In addition, LOMBs are more readily generated in a styrene-oxidized system in the presence/absence of NOx than highly oxygenated organic molecules (HOMs). The reaction of OH radicals with other aromatics containing a branched chain on the benzene ring produces LOMBs to varying degrees, with pi-pi stacking playing an essential role. This result suggests that, in the presence of H2SO4 molecules, LOMBs may play a more significant role in promoting nucleation than HOMs. Our findings serve as a pivotal foundation for future investigations into the oxidation and nucleation processes of diverse aromatics in urban environments.
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Affiliation(s)
- Huidi Zhang
- College of Geography and Environment, Shandong Normal University, Jinan 250014, PR China
| | - Juanbao Wang
- College of Geography and Environment, Shandong Normal University, Jinan 250014, PR China
| | - Biao Dong
- College of Geography and Environment, Shandong Normal University, Jinan 250014, PR China
| | - Fei Xu
- Environment Research Institute, Shandong University, Qingdao 266237, PR China
| | - Houfeng Liu
- College of Geography and Environment, Shandong Normal University, Jinan 250014, PR China
| | - Qingzhu Zhang
- Environment Research Institute, Shandong University, Qingdao 266237, PR China
| | - Wansong Zong
- College of Geography and Environment, Shandong Normal University, Jinan 250014, PR China
| | - Xiangli Shi
- College of Geography and Environment, Shandong Normal University, Jinan 250014, PR China.
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6
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Li D, Huang W, Wang D, Wang M, Thornton JA, Caudillo L, Rörup B, Marten R, Scholz W, Finkenzeller H, Marie G, Baltensperger U, Bell DM, Brasseur Z, Curtius J, Dada L, Duplissy J, Gong X, Hansel A, He XC, Hofbauer V, Junninen H, Krechmer JE, Kürten A, Lamkaddam H, Lehtipalo K, Lopez B, Ma Y, Mahfouz NGA, Manninen HE, Mentler B, Perrier S, Petäjä T, Pfeifer J, Philippov M, Schervish M, Schobesberger S, Shen J, Surdu M, Tomaz S, Volkamer R, Wang X, Weber SK, Welti A, Worsnop DR, Wu Y, Yan C, Zauner-Wieczorek M, Kulmala M, Kirkby J, Donahue NM, George C, El-Haddad I, Bianchi F, Riva M. Nitrate Radicals Suppress Biogenic New Particle Formation from Monoterpene Oxidation. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2024; 58:1601-1614. [PMID: 38185880 DOI: 10.1021/acs.est.3c07958] [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: 01/09/2024]
Abstract
Highly oxygenated organic molecules (HOMs) are a major source of new particles that affect the Earth's climate. HOM production from the oxidation of volatile organic compounds (VOCs) occurs during both the day and night and can lead to new particle formation (NPF). However, NPF involving organic vapors has been reported much more often during the daytime than during nighttime. Here, we show that the nitrate radicals (NO3), which arise predominantly at night, inhibit NPF during the oxidation of monoterpenes based on three lines of observational evidence: NPF experiments in the CLOUD (Cosmics Leaving OUtdoor Droplets) chamber at CERN (European Organization for Nuclear Research), radical chemistry experiments using an oxidation flow reactor, and field observations in a wetland that occasionally exhibits nocturnal NPF. Nitrooxy-peroxy radicals formed from NO3 chemistry suppress the production of ultralow-volatility organic compounds (ULVOCs) responsible for biogenic NPF, which are covalently bound peroxy radical (RO2) dimer association products. The ULVOC yield of α-pinene in the presence of NO3 is one-fifth of that resulting from ozone chemistry alone. Even trace amounts of NO3 radicals, at sub-parts per trillion level, suppress the NPF rate by a factor of 4. Ambient observations further confirm that when NO3 chemistry is involved, monoterpene NPF is completely turned off. Our results explain the frequent absence of nocturnal biogenic NPF in monoterpene (α-pinene)-rich environments.
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Affiliation(s)
- Dandan Li
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
| | - Wei Huang
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Dongyu Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Mingyi Wang
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Joel A Thornton
- Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - Lucía Caudillo
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
| | - Birte Rörup
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Ruby Marten
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Wiebke Scholz
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck 6020, Austria
| | - Henning Finkenzeller
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Guillaume Marie
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Zoé Brasseur
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Joachim Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
| | - Lubna Dada
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Jonathan Duplissy
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
- Helsinki Institute of Physics (HIP)/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Xianda Gong
- Leibniz Institute for Tropospheric Research, Leipzig 04318, Germany
| | - Armin Hansel
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck 6020, Austria
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Victoria Hofbauer
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Heikki Junninen
- Institute of Physics, University of Tartu, Tartu 50090, Estonia
| | - Jordan E Krechmer
- Aerodyne Research Inc., Billerica, Massachusetts 01821, United States
| | - Andreas Kürten
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
| | - Houssni Lamkaddam
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
- Finnish Meteorological Institute, Helsinki 00560, Finland
| | - Brandon Lopez
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Yingge Ma
- State Environmental Protection Key Laboratory of Formation and Prevention of Urban Air Pollution Complex, Shanghai Academy of Environment Sciences, Shanghai 200233, P. R. China
| | - Naser G A Mahfouz
- Atmospheric and Oceanic Sciences, Princeton University, Princeton, New Jersey 08540, United States
| | - Hanna E Manninen
- CERN, the European Organization for Nuclear Research, Geneve 23 CH-1211, Switzerland
| | - Bernhard Mentler
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck 6020, Austria
| | - Sebastien Perrier
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
| | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Joschka Pfeifer
- CERN, the European Organization for Nuclear Research, Geneve 23 CH-1211, Switzerland
| | - Maxim Philippov
- P.N. Lebedev Physical Institute of the Russian Academy of Sciences, Moscow 119991, Russia
| | - Meredith Schervish
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | | | - Jiali Shen
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Mihnea Surdu
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Sophie Tomaz
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
| | - Rainer Volkamer
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Xinke Wang
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
| | - Stefan K Weber
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
- CERN, the European Organization for Nuclear Research, Geneve 23 CH-1211, Switzerland
| | - André Welti
- Finnish Meteorological Institute, Helsinki 00560, Finland
| | - Douglas R Worsnop
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
- Aerodyne Research Inc., Billerica, Massachusetts 01821, United States
| | - Yusheng Wu
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Chao Yan
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Marcel Zauner-Wieczorek
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Jasper Kirkby
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany
- CERN, the European Organization for Nuclear Research, Geneve 23 CH-1211, Switzerland
| | - Neil M Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Christian George
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
| | - Imad El-Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Matthieu Riva
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
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7
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Li Z, Zhao B, Yin D, Wang S, Qiao X, Jiang J, Li Y, Shen J, He Y, Chang X, Li X, Liu Y, Li Y, Liu C, Qi X, Chen L, Chi X, Jiang Y, Li Y, Wu J, Nie W, Ding A. Modeling the Formation of Organic Compounds across Full Volatility Ranges and Their Contribution to Nanoparticle Growth in a Polluted Atmosphere. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2024; 58:1223-1235. [PMID: 38117938 DOI: 10.1021/acs.est.3c06708] [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: 12/22/2023]
Abstract
Nanoparticle growth influences atmospheric particles' climatic effects, and it is largely driven by low-volatility organic vapors. However, the magnitude and mechanism of organics' contribution to nanoparticle growth in polluted environments remain unclear because current observations and models cannot capture organics across full volatility ranges or track their formation chemistry. Here, we develop a mechanistic model that characterizes the full volatility spectrum of organic vapors and their contributions to nanoparticle growth by coupling advanced organic oxidation modeling and kinetic gas-particle partitioning. The model is applied to Nanjing, a typical polluted city, and it effectively captures the volatility distribution of low-volatility organics (with saturation vapor concentrations <0.3 μg/m3), thus accurately reproducing growth rates (GRs), with a 4.91% normalized mean bias. Simulations indicate that as particles grow from 4 to 40 nm, the relative fractions of GRs attributable to organics increase from 59 to 86%, with the remaining contribution from H2SO4 and its clusters. Aromatics contribute much to condensable organic vapors (∼37%), especially low-volatility vapors (∼61%), thus contributing the most to GRs (32-46%) as 4-40 nm particles grow. Alkanes also contribute 19-35% of GRs, while biogenic volatile organic compounds contribute minimally (<13%). Our model helps assess the climatic impacts of particles and predict future changes.
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Affiliation(s)
- Zeqi Li
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
| | - Bin Zhao
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
| | - Dejia Yin
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
| | - Shuxiao Wang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
| | - Xiaohui Qiao
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Jingkun Jiang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Yiran Li
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Jiewen Shen
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
| | - Yicong He
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
| | - Xing Chang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
- Laboratory of Transport Pollution Control and Monitoring Technology, Transport Planning and Research Institute, Ministry of Transport, Beijing 100028, China
| | - Xiaoxiao Li
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Yuliang Liu
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing 210023, Jiangsu Province, China
- Jiangsu Provincial Collaborative Innovation Center for Climate Change, Nanjing University, Nanjing 210093, China
| | - Yuanyuan Li
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing 210023, Jiangsu Province, China
| | - Chong Liu
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing 210023, Jiangsu Province, China
| | - Ximeng Qi
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing 210023, Jiangsu Province, China
- Jiangsu Provincial Collaborative Innovation Center for Climate Change, Nanjing University, Nanjing 210093, China
| | - Liangduo Chen
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- Jiangsu Provincial Collaborative Innovation Center for Climate Change, Nanjing University, Nanjing 210093, China
| | - Xuguang Chi
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing 210023, Jiangsu Province, China
- Jiangsu Provincial Collaborative Innovation Center for Climate Change, Nanjing University, Nanjing 210093, China
| | - Yueqi Jiang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
- State Environmental Protection Key Laboratory of Sources and Control of Air Pollution Complex, Beijing 100084, China
| | - Yuyang Li
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Jin Wu
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Wei Nie
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing 210023, Jiangsu Province, China
- Jiangsu Provincial Collaborative Innovation Center for Climate Change, Nanjing University, Nanjing 210093, China
| | - Aijun Ding
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing 210023, Jiangsu Province, China
- Jiangsu Provincial Collaborative Innovation Center for Climate Change, Nanjing University, Nanjing 210093, China
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8
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Ye C, Liu Y, Yuan B, Wang Z, Lin Y, Hu W, Chen W, Li T, Song W, Wang X, Lv D, Gu D, Shao M. Low-NO-like Oxidation Pathway Makes a Significant Contribution to Secondary Organic Aerosol in Polluted Urban Air. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:13912-13924. [PMID: 37669221 DOI: 10.1021/acs.est.3c01055] [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: 09/07/2023]
Abstract
Anthropogenic pollutants can greatly mediate formation pathways and chemical compositions of secondary organic aerosol (SOA) in urban atmospheres. We investigated the molecular tracers for different types of SOA in PM2.5 under varying NO/NO2 conditions in Guangzhou using source analysis of particle-phase speciated organics obtained from an iodide chemical ionization mass spectrometer with a Filter Inlet for Gases and AEROsols (FIGAERO-I-CIMS). Results show that low-NO-like pathways (when NO/NO2 < 0.2) explained ∼75% of the total measured FIGAERO-OA during regional transport periods, which was enriched in more-oxidized C4-C6 non-nitrogenous compounds over ozone accumulation. Daytime high-NO chemistry played larger roles (38%) in local pollution episodes, with organic nitrates (ONs) and nitrophenols increasing with enhanced aerosol water content and nitrate fraction. Nighttime NO3-initiated oxidation, characterized by monoterpene-derived ONs, accounted for comparable percentages (10-12%) of FIGAERO-OA for both two periods. Furthermore, the presence of organosulfates (OSs) improves the understanding of the roles of aqueous-phase processes in SOA production. Carbonyl-derived OSs exhibited a preferential formation under conditions of high aerosol acidity and/or abundant sulfate, which correlated well with low-NO-like SOA. Our results demonstrate the importance of NO/NO2 ratios in controlling SOA compositions, as well as interactions between water content, aerosol acidity, and inorganic salts in gas-to-particle partitioning of condensable organics.
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Affiliation(s)
- Chenshuo Ye
- State Key Joint Laboratory of Environmental Simulation and Pollution Control (SKL-ESPC), College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
- Guangdong Provincial Academy of Environmental Science, Guangzhou 510045, China
| | - Ying Liu
- State Key Joint Laboratory of Environmental Simulation and Pollution Control (SKL-ESPC), College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Bin Yuan
- Institute for Environmental and Climate Research, Jinan University, Guangzhou 511443, China
| | - Zelong Wang
- Institute for Environmental and Climate Research, Jinan University, Guangzhou 511443, China
| | - Yi Lin
- Institute for Environmental and Climate Research, Jinan University, Guangzhou 511443, China
| | - Weiwei Hu
- State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Wei Chen
- State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Tiange Li
- Institute for Environmental and Climate Research, Jinan University, Guangzhou 511443, China
| | - Wei Song
- State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Xinming Wang
- State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Daqi Lv
- State Key Joint Laboratory of Environmental Simulation and Pollution Control (SKL-ESPC), College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Dasa Gu
- Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, The Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong 999077, China
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong 999077, China
| | - Min Shao
- Institute for Environmental and Climate Research, Jinan University, Guangzhou 511443, China
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9
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Dada L, Stolzenburg D, Simon M, Fischer L, Heinritzi M, Wang M, Xiao M, Vogel AL, Ahonen L, Amorim A, Baalbaki R, Baccarini A, Baltensperger U, Bianchi F, Daellenbach KR, DeVivo J, Dias A, Dommen J, Duplissy J, Finkenzeller H, Hansel A, He XC, Hofbauer V, Hoyle CR, Kangasluoma J, Kim C, Kürten A, Kvashnin A, Mauldin R, Makhmutov V, Marten R, Mentler B, Nie W, Petäjä T, Quéléver LLJ, Saathoff H, Tauber C, Tome A, Molteni U, Volkamer R, Wagner R, Wagner AC, Wimmer D, Winkler PM, Yan C, Zha Q, Rissanen M, Gordon H, Curtius J, Worsnop DR, Lehtipalo K, Donahue NM, Kirkby J, El Haddad I, Kulmala M. Role of sesquiterpenes in biogenic new particle formation. SCIENCE ADVANCES 2023; 9:eadi5297. [PMID: 37682996 PMCID: PMC10491295 DOI: 10.1126/sciadv.adi5297] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/02/2023] [Accepted: 08/07/2023] [Indexed: 09/10/2023]
Abstract
Biogenic vapors form new particles in the atmosphere, affecting global climate. The contributions of monoterpenes and isoprene to new particle formation (NPF) have been extensively studied. However, sesquiterpenes have received little attention despite a potentially important role due to their high molecular weight. Via chamber experiments performed under atmospheric conditions, we report biogenic NPF resulting from the oxidation of pure mixtures of β-caryophyllene, α-pinene, and isoprene, which produces oxygenated compounds over a wide range of volatilities. We find that a class of vapors termed ultralow-volatility organic compounds (ULVOCs) are highly efficient nucleators and quantitatively determine NPF efficiency. When compared with a mixture of isoprene and monoterpene alone, adding only 2% sesquiterpene increases the ULVOC yield and doubles the formation rate. Thus, sesquiterpene emissions need to be included in assessments of global aerosol concentrations in pristine climates where biogenic NPF is expected to be a major source of cloud condensation nuclei.
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Affiliation(s)
- Lubna Dada
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Dominik Stolzenburg
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
- Universität Wien, Fakultät für Physik, 1090 Vienna, Austria
- Institute for Materials Chemistry, TU Wien, 1060 Vienna, Austria
| | - Mario Simon
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, 60438 Frankfurt am Main, Germany
| | - Lukas Fischer
- Institute for Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
| | - Martin Heinritzi
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, 60438 Frankfurt am Main, Germany
| | - Mingyi Wang
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 5000 Forbes Avenue, Pittsburgh, PA 15213, USA
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA 91125, USA
| | - Mao Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Alexander L. Vogel
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, 60438 Frankfurt am Main, Germany
| | - Lauri Ahonen
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Antonio Amorim
- CENTRA and Faculdade de Ciências da Universidade de Lisboa, Lisboa, Portugal
| | - Rima Baalbaki
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Andrea Baccarini
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Laboratory of Atmospheric Processes and their Impact, Ecole Polytechnique Federale de Lausanne, 1015 Lausanne, Switzerland
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Kaspar R. Daellenbach
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Jenna DeVivo
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 5000 Forbes Avenue, Pittsburgh, PA 15213, USA
| | - Antonio Dias
- CENTRA and Faculdade de Ciências da Universidade de Lisboa, Lisboa, Portugal
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Jonathan Duplissy
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
- Helsinki Institute of Physics (HIP)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Henning Finkenzeller
- Department of Chemistry and CIRES, University of Colorado Boulder, Boulder, CO 80309, USA
| | - Armin Hansel
- Institute for Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
- Finnish Meteorological Institute, FI-00101 Helsinki, Finland
| | - Victoria Hofbauer
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 5000 Forbes Avenue, Pittsburgh, PA 15213, USA
| | - Christopher R. Hoyle
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland
| | - Juha Kangasluoma
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Changhyuk Kim
- School of Civil and Environmental Engineering, Pusan National University, Busan 46241, Republic of Korea
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA 91125, USA
| | - Andreas Kürten
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, 60438 Frankfurt am Main, Germany
| | - Aleksander Kvashnin
- P.N. Lebedev Physical Institute of the Russian Academy of Sciences, 53, Leninskiy Prospekt, Moscow, Russian Federation
| | - Roy Mauldin
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 5000 Forbes Avenue, Pittsburgh, PA 15213, USA
- Department of Atmospheric and Oceanic Sciences, University of Colorado Boulder, Boulder, CO 80309, USA
| | - Vladimir Makhmutov
- P.N. Lebedev Physical Institute of the Russian Academy of Sciences, 53, Leninskiy Prospekt, Moscow, Russian Federation
- Moscow Institute of Physics and Technology (National Research University), 141701 Dolgoprudny, Russian Federation
| | - Ruby Marten
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Bernhard Mentler
- Institute for Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
| | - Wei Nie
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, Jiangsu Province, China
| | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Lauriane L. J. Quéléver
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Harald Saathoff
- Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Hermann-von-Helmholtz-Platz 1, 76344 Eggenstein-Leopoldshafen, Germany
| | | | - Antonio Tome
- IDL-Universidade da Beira Interior, Covilhã, Portugal
| | - Ugo Molteni
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Department of Chemistry, University of California, Irvine, Irvine, CA 92697, USA
- Forest Dynamics, Swiss Federal Institute for Forest, Snow and Landscape Research, 8903 Birmensdorf, Switzerland
| | - Rainer Volkamer
- Finnish Meteorological Institute, FI-00101 Helsinki, Finland
| | - Robert Wagner
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Andrea C. Wagner
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, 60438 Frankfurt am Main, Germany
| | - Daniela Wimmer
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | | | - Chao Yan
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Qiaozhi Zha
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
| | - Matti Rissanen
- Aerosol Physics Laboratory, Department of Physics, Tampere University, 33720 Tampere, Finland
- Chemistry Department, University of Helsinki, 00014 Helsinki, Finland
| | - Hamish Gordon
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 5000 Forbes Avenue, Pittsburgh, PA 15213, USA
| | - Joachim Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, 60438 Frankfurt am Main, Germany
| | - Douglas R. Worsnop
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
- Aerodyne Research Inc., Billerica, MA 01821, USA
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
- Finnish Meteorological Institute, FI-00101 Helsinki, Finland
| | - Neil M. Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 5000 Forbes Avenue, Pittsburgh, PA 15213, USA
| | - Jasper Kirkby
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, 60438 Frankfurt am Main, Germany
- CERN, CH-1211 Geneva 23, Switzerland
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, FI-00014 Finland
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10
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Nie W, Yan C, Yang L, Roldin P, Liu Y, Vogel AL, Molteni U, Stolzenburg D, Finkenzeller H, Amorim A, Bianchi F, Curtius J, Dada L, Draper DC, Duplissy J, Hansel A, He XC, Hofbauer V, Jokinen T, Kim C, Lehtipalo K, Nichman L, Mauldin RL, Makhmutov V, Mentler B, Mizelli-Ojdanic A, Petäjä T, Quéléver LLJ, Schallhart S, Simon M, Tauber C, Tomé A, Volkamer R, Wagner AC, Wagner R, Wang M, Ye P, Li H, Huang W, Qi X, Lou S, Liu T, Chi X, Dommen J, Baltensperger U, El Haddad I, Kirkby J, Worsnop D, Kulmala M, Donahue NM, Ehn M, Ding A. NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere. Nat Commun 2023; 14:3347. [PMID: 37291087 DOI: 10.1038/s41467-023-39066-4] [Citation(s) in RCA: 4] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/14/2022] [Accepted: 05/24/2023] [Indexed: 06/10/2023] Open
Abstract
The interaction between nitrogen monoxide (NO) and organic peroxy radicals (RO2) greatly impacts the formation of highly oxygenated organic molecules (HOM), the key precursors of secondary organic aerosols. It has been thought that HOM production can be significantly suppressed by NO even at low concentrations. Here, we perform dedicated experiments focusing on HOM formation from monoterpenes at low NO concentrations (0 - 82 pptv). We demonstrate that such low NO can enhance HOM production by modulating the RO2 loss and favoring the formation of alkoxy radicals that can continue to autoxidize through isomerization. These insights suggest that HOM yields from typical boreal forest emissions can vary between 2.5%-6.5%, and HOM formation will not be completely inhibited even at high NO concentrations. Our findings challenge the notion that NO monotonically reduces HOM yields by extending the knowledge of RO2-NO interactions to the low-NO regime. This represents a major advance towards an accurate assessment of HOM budgets, especially in low-NO environments, which prevails in the pre-industrial atmosphere, pristine areas, and the upper boundary layer.
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Affiliation(s)
- Wei Nie
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China.
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing, Jiangsu Province, China.
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland.
| | - Chao Yan
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing, Jiangsu Province, China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Liwen Yang
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Pontus Roldin
- Department of Physics, Lund University, P. O. Box 118, SE-221 00, Lund, Sweden
- IVL, Swedish Environmental Research Institute, SE-211 19, Malmö, Sweden
| | - Yuliang Liu
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Alexander L Vogel
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, 60438, Germany
| | - Ugo Molteni
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, Villigen PSI, Switzerland
- Department of Chemistry, University of California, Irvine, CA, 92697, USA
- Forest Dynamics, Swiss Federal Institute for Forest, Snow and Landscape Research, 8903, Birmensdorf, Switzerland
| | - Dominik Stolzenburg
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
- Faculty of Physics, University of Vienna, Boltzmanngasse 5, 1090, Vienna, Austria
| | - Henning Finkenzeller
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, CO, 80309, USA
| | - Antonio Amorim
- CENTRA and FCUL, Universidade de Lisboa, Campo Grande, 1749-016, Lisboa, Portugal
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Joachim Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, 60438, Germany
| | - Lubna Dada
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, Villigen PSI, Switzerland
| | - Danielle C Draper
- Department of Chemistry, University of California, Irvine, CA, 92697, USA
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, 91125, USA
| | - Jonathan Duplissy
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
- Helsinki Institute of Physics (HIP)/Physics, Faculty of Science, University of Helsinki, 00014, Helsinki, Finland
| | - Armin Hansel
- Institute of Ion and Applied Physics, University of Innsbruck, 6020, Innsbruck, Austria
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Victoria Hofbauer
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
| | - Tuija Jokinen
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
- Climate & Atmosphere Research Centre (CARE-C), The Cyprus Institute, P.O. Box 27456, Nicosia, CY-1645, Cyprus
| | - Changhyuk Kim
- School of Civil and Environmental Engineering, Pusan National University, Busan, 46241, Republic of Korea
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, 91125, USA
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
- Finnish Meteorological Institute, Erik Palménin aukio 1, 00560, Helsinki, Finland
| | - Leonid Nichman
- Flight Research Laboratory, National Research Council Canada, Ottawa, K1A 0R6, ON, Canada
| | - Roy L Mauldin
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Atmospheric and Oceanic Sciences, University of Colorado Boulder, Boulder, CO, USA
| | - Vladimir Makhmutov
- P.N. Lebedev Physical Institute of the Russian Academy of Sciences, 53, Leninskiy Prospekt, Moscow, Russian Federation
- Moscow Institute of Physics and Technology (National Research University), 1A Kerchenskaya st., Moscow, Russian Federation
| | - Bernhard Mentler
- Ion Molecule Reactions & Environmental Physics Group Institute of Ion Physics and Applied Physics Leopold-Franzens University, Innsbruck Technikerstraße 25, A-6020, Innsbruck, Austria
| | - Andrea Mizelli-Ojdanic
- Faculty of Physics, University of Vienna, Boltzmanngasse 5, 1090, Vienna, Austria
- Faculty of Industrial Engineering, FH Technikum Wien - University of Applied Sciences, 1200, Vienna, Austria
| | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Lauriane L J Quéléver
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Simon Schallhart
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
- Finnish Meteorological Institute, Erik Palménin aukio 1, 00560, Helsinki, Finland
| | - Mario Simon
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, 60438, Germany
| | - Christian Tauber
- Faculty of Physics, University of Vienna, Boltzmanngasse 5, 1090, Vienna, Austria
| | - António Tomé
- IDL-Universidade da Beira Interior, Rua Marquês D'Ávila e, Bolama, 6201-001, Covilhã, Portugal
| | - Rainer Volkamer
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, CO, 80309, USA
| | - Andrea C Wagner
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, 60438, Germany
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, CO, 80309, USA
| | - Robert Wagner
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Mingyi Wang
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, 91125, USA
| | - Penglin Ye
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), Department of Environmental Science and Engineering, Fudan University, Shanghai, 200438, China
| | - Haiyan Li
- School of Civil and Environmental Engineering, Harbin Institute of Technology, Shenzhen, 518055, China
| | - Wei Huang
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Ximeng Qi
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing, Jiangsu Province, China
| | - Sijia Lou
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
| | - Tengyu Liu
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing, Jiangsu Province, China
| | - Xuguang Chi
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing, Jiangsu Province, China
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, Villigen PSI, Switzerland
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, Villigen PSI, Switzerland
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, Villigen PSI, Switzerland
| | | | - Douglas Worsnop
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
- Aerodyne Research Inc., Billerica, MA, 01821, USA
| | - Markku Kulmala
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Neil M Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
| | - Mikael Ehn
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Aijun Ding
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing, China.
- National Observation and Research Station for Atmospheric Processes and Environmental Change in Yangtze River Delta, Nanjing, Jiangsu Province, China.
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11
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Zheng P, Chen Y, Wang Z, Liu Y, Pu W, Yu C, Xia M, Xu Y, Guo J, Guo Y, Tian L, Qiao X, Huang DD, Yan C, Nie W, Worsnop DR, Lee S, Wang T. Molecular Characterization of Oxygenated Organic Molecules and Their Dominating Roles in Particle Growth in Hong Kong. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:7764-7776. [PMID: 37155674 DOI: 10.1021/acs.est.2c09252] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/10/2023]
Abstract
Oxygenated organic molecules (OOMs) are critical intermediates linking volatile organic compound oxidation and secondary organic aerosol (SOA) formation. Yet, the understanding of OOM components, formation mechanism, and impacts are still limited, especially for urbanized regions with a cocktail of anthropogenic emissions. Herein, ambient measurements of OOMs were conducted at a regional background site in South China in 2018. The molecular characteristics of OOMs revealed dominant nitrogen-containing products, and the influences of different factors on OOM composition and oxidation state were elucidated. Positive matrix factorization analysis resolved the complex OOM species to factors featured with fingerprint species from different oxidation pathways. A new method was developed to identify the key functional groups of OOMs, which successfully classified the majority species into carbonyls (8%), hydroperoxides (7%), nitrates (17%), peroxyl nitrates (10%), dinitrates (13%), aromatic ring-retaining species (6%), and terpenes (7%). The volatility estimation of OOMs was improved based on their identified functional groups and was used to simulate the aerosol growth process contributed by the condensation of those low-volatile OOMs. The results demonstrate the predominant role of OOMs in contributing sub-100 nm particle growth and SOA formation and highlight the importance of dinitrates and anthropogenic products from multistep oxidation.
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Affiliation(s)
- Penggang Zheng
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Kowloon, Hong Kong SAR 999077, China
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Kowloon, Hong Kong SAR 999077, China
| | - Yi Chen
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Kowloon, Hong Kong SAR 999077, China
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Kowloon, Hong Kong SAR 999077, China
| | - Zhe Wang
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Kowloon, Hong Kong SAR 999077, China
| | - Yuliang Liu
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
| | - Wei Pu
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Kowloon, Hong Kong SAR 999077, China
| | - Chuan Yu
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Kowloon, Hong Kong SAR 999077, China
| | - Men Xia
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Kowloon, Hong Kong SAR 999077, China
| | - Yang Xu
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Kowloon, Hong Kong SAR 999077, China
| | - Jia Guo
- Environmental Central Facility, The Hong Kong University of Science and Technology, Kowloon, Hong Kong SAR 999077, China
| | - Yishuo Guo
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing 100084, China
| | - Linhui Tian
- Department of Civil and Environmental Engineering, Faculty of Science and Technology, University of Macau, Taipa, Macau 999078, China
| | - Xiaohui Qiao
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Dan Dan Huang
- State Environmental Protection Key Laboratory of Formation and Prevention of Urban Air Pollution Complex, Shanghai Academy of Environmental Sciences, Shanghai 200233, China
| | - Chao Yan
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Wei Nie
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
| | - Douglas R Worsnop
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
- Aerodyne Research Inc., Billerica, Massachusetts 01821, United States
| | - Shuncheng Lee
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Kowloon, Hong Kong SAR 999077, China
| | - Tao Wang
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Kowloon, Hong Kong SAR 999077, China
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12
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Brean J, Rowell A, Beddows DCS, Shi Z, Harrison RM. Estimates of Future New Particle Formation under Different Emission Scenarios in Beijing. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:4741-4750. [PMID: 36930743 PMCID: PMC10061929 DOI: 10.1021/acs.est.2c08348] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 11/08/2022] [Revised: 03/06/2023] [Accepted: 03/06/2023] [Indexed: 06/18/2023]
Abstract
New particle formation (NPF) is a leading source of particulate matter by number and a contributor to particle mass during haze events. Reductions in emissions of air pollutants, many of which are NPF precursors, are expected in the move toward carbon neutrality or net-zero. Expected changes to pollutant emissions are used to investigate future changes to NPF processes, in comparison to a simulation of current conditions. The projected changes to SO2 emissions are key in changing future NPF number, with different scenarios producing either a doubling or near total reduction in sulfuric acid-amine particle formation rates. Particle growth rates are projected to change little in all but the strictest emission control scenarios. These changes will reduce the particle mass arising by NPF substantially, thus showing a further cobenefit of net-zero policies. Major uncertainties remain in future NPF including the volatility of oxygenated organic molecules resulting from changes to NOx and amine emissions.
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Affiliation(s)
- James Brean
- School
of Geography, Earth & Environmental
Sciences University of Birmingham, Birmingham B15 2TT, United Kingdom
| | - Alex Rowell
- School
of Geography, Earth & Environmental
Sciences University of Birmingham, Birmingham B15 2TT, United Kingdom
| | - David C. S. Beddows
- School
of Geography, Earth & Environmental
Sciences University of Birmingham, Birmingham B15 2TT, United Kingdom
| | - Zongbo Shi
- School
of Geography, Earth & Environmental
Sciences University of Birmingham, Birmingham B15 2TT, United Kingdom
| | - Roy M. Harrison
- School
of Geography, Earth & Environmental
Sciences University of Birmingham, Birmingham B15 2TT, United Kingdom
- Department
of Environmental Sciences, Faculty of Meteorology, Environment and
Arid Land Agriculture, King Abdulaziz University, Jeddah 21589, Saudi Arabia
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13
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Cai R, Huang W, Meder M, Bourgain F, Aizikov K, Riva M, Bianchi F, Ehn M. Improving the Sensitivity of Fourier Transform Mass Spectrometer (Orbitrap) for Online Measurements of Atmospheric Vapors. Anal Chem 2022; 94:15746-15753. [DOI: 10.1021/acs.analchem.2c03403] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Runlong Cai
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Wei Huang
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Melissa Meder
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Frederic Bourgain
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
| | | | - Matthieu Riva
- Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
| | - Mikael Ehn
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland
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14
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Shen H, Vereecken L, Kang S, Pullinen I, Fuchs H, Zhao D, Mentel TF. Unexpected significance of a minor reaction pathway in daytime formation of biogenic highly oxygenated organic compounds. SCIENCE ADVANCES 2022; 8:eabp8702. [PMID: 36269820 PMCID: PMC9586481 DOI: 10.1126/sciadv.abp8702] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 03/08/2022] [Accepted: 09/01/2022] [Indexed: 06/16/2023]
Abstract
Secondary organic aerosol (SOA), formed by oxidation of volatile organic compounds, substantially influence air quality and climate. Highly oxygenated organic molecules (HOMs), particularly those formed from biogenic monoterpenes, contribute a large fraction of SOA. During daytime, hydroxyl radicals initiate monoterpene oxidation, mainly by hydroxyl addition to monoterpene double bonds. Naturally, related HOM formation mechanisms should be induced by that reaction route, too. However, for α-pinene, the most abundant atmospheric monoterpene, we find a previously unidentified competitive pathway under atmospherically relevant conditions: HOM formation is predominately induced via hydrogen abstraction by hydroxyl radicals, a generally minor reaction pathway. We show by observations and theoretical calculations that hydrogen abstraction followed by formation and rearrangement of alkoxy radicals is a prerequisite for fast daytime HOM formation. Our analysis provides an accurate mechanism and yield, demonstrating that minor reaction pathways can become major, here for SOA formation and growth and related impacts on air quality and climate.
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Affiliation(s)
- Hongru Shen
- Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences, Fudan University, Shanghai 200438, China
| | - Luc Vereecken
- Institute of Energy and Climate Research, IEK-8: Troposphere, Forschungszentrum Jülich GmbH, 52425 Jülich, Germany
| | - Sungah Kang
- Institute of Energy and Climate Research, IEK-8: Troposphere, Forschungszentrum Jülich GmbH, 52425 Jülich, Germany
| | - Iida Pullinen
- Institute of Energy and Climate Research, IEK-8: Troposphere, Forschungszentrum Jülich GmbH, 52425 Jülich, Germany
| | - Hendrik Fuchs
- Institute of Energy and Climate Research, IEK-8: Troposphere, Forschungszentrum Jülich GmbH, 52425 Jülich, Germany
- Physikalisches Institut, Universität zu Köln, 50932 Köln, Germany
| | - Defeng Zhao
- Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences, Fudan University, Shanghai 200438, China
- Shanghai Frontiers Science Center of Atmosphere-Ocean Interaction, Fudan University, Shanghai 200438, China
- Institute of Eco-Chongming (IEC), 20 Cuiniao Rd., Chongming, Shanghai 202162, China
- IRDR ICoE on Risk Interconnectivity and Governance on Weather/Climate Extremes Impact and Public Health, Fudan University, Shanghai 200438, China
| | - Thomas F. Mentel
- Institute of Energy and Climate Research, IEK-8: Troposphere, Forschungszentrum Jülich GmbH, 52425 Jülich, Germany
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15
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Chen T, Zhang P, Ma Q, Chu B, Liu J, Ge Y, He H. Smog Chamber Study on the Role of NO x in SOA and O 3 Formation from Aromatic Hydrocarbons. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:13654-13663. [PMID: 36136046 DOI: 10.1021/acs.est.2c04022] [Citation(s) in RCA: 7] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/16/2023]
Abstract
China is facing dual pressures to reduce both PM2.5 and O3 pollution, the crucial precursors of which are NOx and VOCs. In our study, the role of NOx in both secondary organic aerosol (SOA, the important constituent of PM2.5) and O3 formation was examined in our 30 m3 indoor smog chamber. As revealed in the present study, the NOx level can obviously affect the OH concentration and volatility distribution of gas-phase oxidation products and thus O3 and SOA formation. Reducing the NOx concentration to the NOx-sensitive regime can inhibit O3 formation (by 42%), resulting in the reduction of oxidation capacity, which suppresses the SOA formation (by 45%) by inhibiting the formation of O- and N-containing gas-phase oxidation products with low volatility. The contribution of these oxidation products to the formation of SOA was also estimated, and the results could substantially support the trend of SOA yield with NOx at different VOC levels. The atmospheric implications of NOx in the coordinated control of PM2.5 and O3 are also discussed.
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Affiliation(s)
- Tianzeng Chen
- State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| | - Peng Zhang
- State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Qingxin Ma
- State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Biwu Chu
- State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Jun Liu
- State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Yanli Ge
- State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Hong He
- State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
- University of Chinese Academy of Sciences, Beijing 100049, China
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16
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Edwards KC, Klodt AL, Galeazzo T, Schervish M, Wei J, Fang T, Donahue NM, Aumont B, Nizkorodov SA, Shiraiwa M. Effects of Nitrogen Oxides on the Production of Reactive Oxygen Species and Environmentally Persistent Free Radicals from α-Pinene and Naphthalene Secondary Organic Aerosols. J Phys Chem A 2022; 126:7361-7372. [PMID: 36194388 PMCID: PMC9574922 DOI: 10.1021/acs.jpca.2c05532] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Abstract
Reactive oxygen species (ROS) and environmentally persistent free radicals (EPFR) play an important role in chemical transformation of atmospheric aerosols and adverse aerosol health effects. This study investigated the effects of nitrogen oxides (NOx) during photooxidation of α-pinene and naphthalene on the EPFR content and ROS formation from secondary organic aerosols (SOA). Electron paramagnetic resonance (EPR) spectroscopy was applied to quantify EPFR content and ROS formation. While no EPFR were detected in α-pinene SOA, we found that naphthalene SOA contained about 0.7 pmol μg-1 of EPFR, and NOx has little influence on EPFR concentrations and oxidative potential. α-Pinene and naphthalene SOA generated under low NOx conditions form OH radicals and superoxide in the aqueous phase, which was lowered substantially by 50-80% for SOA generated under high NOx conditions. High-resolution mass spectrometry analysis showed the substantial formation of nitroaromatics and organic nitrates in a high NOx environment. The modeling results using the GECKO-A model that simulates explicit gas-phase chemistry and the radical 2D-VBS model that treats autoxidation predicted reduced formation of hydroperoxides and enhanced formation of organic nitrates under high NOx due to the reactions of peroxy radicals with NOx instead of their reactions with HO2. Consistently, the presence of NOx resulted in the decrease of peroxide contents and oxidative potential of α-pinene SOA.
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Affiliation(s)
- Kasey C Edwards
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
| | - Alexandra L Klodt
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
| | - Tommaso Galeazzo
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
| | - Meredith Schervish
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
| | - Jinlai Wei
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
| | - Ting Fang
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
| | - Neil M Donahue
- Departments of Chemistry, Chemical Engineering, Engineering and Public Policy, Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Bernard Aumont
- CNRS, LISA, Univ of Paris Est Creteil and University Paris Cité, F-94010 Créteil, France
| | - Sergey A Nizkorodov
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
| | - Manabu Shiraiwa
- Department of Chemistry, University of California, Irvine, Irvine, California 92697, United States
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17
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Li X, Li Y, Cai R, Yan C, Qiao X, Guo Y, Deng C, Yin R, Chen Y, Li Y, Yao L, Sarnela N, Zhang Y, Petäjä T, Bianchi F, Liu Y, Kulmala M, Hao J, Smith JN, Jiang J. Insufficient Condensable Organic Vapors Lead to Slow Growth of New Particles in an Urban Environment. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:9936-9946. [PMID: 35749221 DOI: 10.1021/acs.est.2c01566] [Citation(s) in RCA: 10] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/15/2023]
Abstract
Atmospheric new particle formation significantly affects global climate and air quality after newly formed particles grow above ∼50 nm. In polluted urban atmospheres with 1-3 orders of magnitude higher new particle formation rates than those in clean atmospheres, particle growth rates are comparable or even lower for reasons that were previously unclear. Here, we address the slow growth in urban Beijing with advanced measurements of the size-resolved molecular composition of nanoparticles using the thermal desorption chemical ionization mass spectrometer and the gas precursors using the nitrate CI-APi-ToF. A particle growth model combining condensational growth and particle-phase acid-base chemistry was developed to explore the growth mechanisms. The composition of 8-40 nm particles during new particle formation events in urban Beijing is dominated by organics (∼80%) and sulfate (∼13%), and the remainder is from base compounds, nitrate, and chloride. With the increase in particle sizes, the fraction of sulfate decreases, while that of the slow-desorbed organics, organic acids, and nitrate increases. The simulated size-resolved composition and growth rates are consistent with the measured results in most cases, and they both indicate that the condensational growth of organic vapors and H2SO4 is the major growth pathway and the particle-phase acid-base reactions play a minor role. In comparison to the high concentrations of gaseous sulfuric acid and amines that cause high formation rates, the concentration of condensable organic vapors is comparably lower under the high NOx levels, while those of the relatively high-volatility nitrogen-containing oxidation products are higher. The insufficient condensable organic vapors lead to slow growth, which further causes low survival of the newly formed particles in urban environments. Thus, the low growth rates, to some extent, counteract the impact of the high formation rates on air quality and global climate in urban environments.
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Affiliation(s)
- Xiaoxiao Li
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - Yuyang Li
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - Runlong Cai
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Chao Yan
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, China
| | - Xiaohui Qiao
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - Yishuo Guo
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, China
| | - Chenjuan Deng
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - Rujing Yin
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - Yijing Chen
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - Yiran Li
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - Lei Yao
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Nina Sarnela
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Yusheng Zhang
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, China
| | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, China
| | - Yongchun Liu
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, China
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, China
| | - Jiming Hao
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
| | - James N Smith
- Chemistry Department, University of California, Irvine, California 92697, United Sates
| | - Jingkun Jiang
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, China
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18
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Shang D, Tang L, Fang X, Wang L, Yang S, Wu Z, Chen S, Li X, Zeng L, Guo S, Hu M. Variations in source contributions of particle number concentration under long-term emission control in winter of urban Beijing. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2022; 304:119072. [PMID: 35301034 DOI: 10.1016/j.envpol.2022.119072] [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: 11/29/2021] [Revised: 02/20/2022] [Accepted: 02/25/2022] [Indexed: 06/14/2023]
Abstract
Many studies revealed the rapid decline of atmospheric PM2.5 in Beijing due to the emission control measures. The variation of particle number concentration (PN) which has important influences on regional climate and human health, however, was rarely reported. This study measured the particle number size distributions (PNSD) in 3-700 nm in winter of Beijing during 2013-2019. It was found that PN decreased by 58% from 2013 to 2017, but increased by 29% from 2017 to 2019. By Positive matrix factorization (PMF) analysis, five source factors of PNSD were identified as Nucleation, Fresh traffic, Aged traffic + Diesel, Coal + biomass burning and Secondary. Overall, factors associated with primary emissions were found to decrease continuously. Coal + biomass burning dominated the reduction (65%) among the three primary sources during 2013-2017, which resulted from the great efforts on emission control of coal combustion and biomass burning. Fresh traffic and Aged traffic + Diesel decreased by 43% and 66%, respectively, from 2013 to 2019, as a result of the upgrade of the vehicle emission standards in Beijing-Tianjin-Hebei area. On the other hand, the contribution from Nucleation and Secondary decreased with the reduction of gaseous precursors in 2013-2017, but due to the increased intensity of new particle formation (NPF) and secondary oxidation, they increased by 56% and 70%, respectively, from 2017 to 2019, which led to the simultaneously increase of PN and particle volume concentration. This study indicated that NPF may play an important role in urban atmosphere under continuous air quality improvement.
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Affiliation(s)
- Dongjie Shang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
| | - Lizi Tang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
| | - Xin Fang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
| | - Lifan Wang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
| | - Suding Yang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
| | - Zhijun Wu
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China; Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Nanjing University of Information Science & Technology, Nanjing, 210044, China
| | - Shiyi Chen
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
| | - Xin Li
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China; Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Nanjing University of Information Science & Technology, Nanjing, 210044, China
| | - Limin Zeng
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China; Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Nanjing University of Information Science & Technology, Nanjing, 210044, China
| | - Song Guo
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China; Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Nanjing University of Information Science & Technology, Nanjing, 210044, China
| | - Min Hu
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, International Joint Laboratory for Regional Pollution Control, Ministry of Education (IJRC), College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China; Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Nanjing University of Information Science & Technology, Nanjing, 210044, China.
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19
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Aruffo E, Wang J, Ye J, Ohno P, Qin Y, Stewart M, McKinney K, Di Carlo P, Martin ST. Partitioning of Organonitrates in the Production of Secondary Organic Aerosols from α-Pinene Photo-Oxidation. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:5421-5429. [PMID: 35413185 PMCID: PMC9069682 DOI: 10.1021/acs.est.1c08380] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/08/2023]
Abstract
The chemical pathways for the production of secondary organic aerosols (SOA) are influenced by the concentration of nitrogen oxides (NOx), including the production of organonitrates (ON). Herein, a series of experiments conducted in an environmental chamber investigated the production and partitioning of total organonitrates from α-pinene photo-oxidation from <1 to 24 ppb NOx. Gas-phase and particle-phase organonitrates (gON and pON, respectively) were measured by laser-induced fluorescence (LIF). The composition of the particle phase and the particle mass concentration were simultaneously characterized by online aerosol mass spectrometry. The LIF and MS measurements of pON concentrations had a Pearson correlation coefficient of 0.91 from 0.3 to 1.1 μg m-3. For 1-6 ppb NOx, the yield of SOA particle mass concentration increased from 0.02 to 0.044 with NOx concentration. For >6 ppb NOx, the yield steadily dropped, reaching 0.034 at 24 ppb NOx. By comparison, the yield of pON steadily increased from 0.002 to 0.022 across the range of investigated NOx concentrations. The yield of gON likewise increased from 0.005 to 0.148. The gas-to-particle partitioning ratio (pON/(pON + gON)) depended strongly on the NOx concentration, changing from 0.27 to 0.13 as the NOx increased from <1 to 24 ppb. In the atmosphere, there is typically a cross-over point between clean and polluted conditions that strongly affects SOA production, and the results herein quantitatively identify 6 ppb NOx as that point for α-pinene photo-oxidation under these study conditions, including the production and partitioning of organonitrates. The trends in SOA yield and partitioning ratio as a function of NOx occur because of the changes in pON volatility.
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Affiliation(s)
- Eleonora Aruffo
- Department
of Advanced Technologies in Medicine & Dentistry, University “G. d’Annunzio” of Chieti-Pescara, Chieti 66100, Italy
- Center
for Advanced Studies and Technology-CAST, Chieti 66100, Italy
| | - Junfeng Wang
- Jiangsu
Key Laboratory of Atmospheric Environment Monitoring and Pollution
Control, Collaborative Innovation Center of Atmospheric Environment
and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science and Technology, Nanjing 211544, China
| | - Jianhuai Ye
- School
of Environmental Science & Engineering, Southern University of Science and Technology, Shenzhen 5180551, China
| | - Paul Ohno
- School
of Engineering and Applied Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
| | - Yiming Qin
- Department
of Chemistry, University of California Irvine, Irvine, California 92697-2025, United States
| | - Matthew Stewart
- School
of Engineering and Applied Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
| | - Karena McKinney
- Department
of Chemistry, Colby College, Waterville, Maine 04901, United States
| | - Piero Di Carlo
- Department
of Advanced Technologies in Medicine & Dentistry, University “G. d’Annunzio” of Chieti-Pescara, Chieti 66100, Italy
- Center
for Advanced Studies and Technology-CAST, Chieti 66100, Italy
| | - Scot T. Martin
- School
of Engineering and Applied Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
- Department
of Earth and Planetary Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
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20
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Kontkanen J, Stolzenburg D, Olenius T, Yan C, Dada L, Ahonen L, Simon M, Lehtipalo K, Riipinen I. What controls the observed size-dependency of the growth rates of sub-10 nm atmospheric particles? ENVIRONMENTAL SCIENCE: ATMOSPHERES 2022; 2:449-468. [PMID: 35694135 PMCID: PMC9119032 DOI: 10.1039/d1ea00103e] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 12/17/2021] [Accepted: 03/12/2022] [Indexed: 11/21/2022]
Abstract
The formation and growth of atmospheric particles involving sulfuric acid and organic vapors is estimated to have significant climate effects. To accurately represent this process in large-scale models, the correct interpretation of the observations on particle growth, especially below 10 nm, is essential. Here, we disentangle the factors governing the growth of sub-10 nm particles in the presence of sulfuric acid and organic vapors, using molecular-resolution cluster population simulations and chamber experiments. We find that observed particle growth rates are determined by the combined effects of (1) the concentrations and evaporation rates of the condensing vapors, (2) particle population dynamics, and (3) stochastic fluctuations, characteristic to initial nucleation. This leads to a different size-dependency of growth rate in the presence of sulfuric acid and/or organic vapors at different concentrations. Specifically, the activation type behavior, resulting in growth rate increasing with the particle size, is observed only at certain vapor concentrations. In our model simulations, cluster–cluster collisions enhance growth rate at high vapor concentrations and their importance is dictated by the cluster evaporation rates, which demonstrates the need for accurate evaporation rate data. Finally, we show that at sizes below ∼2.5–3.5 nm, stochastic effects can importantly contribute to particle population growth. Overall, our results suggest that interpreting particle growth observations with approaches neglecting population dynamics and stochastics, such as with single particle growth models, can lead to the wrong conclusions on the properties of condensing vapors and particle growth mechanisms. A combination of cluster population simulations and chamber experiments was used to disentangle the factors governing the observed growth rates of atmospheric particles.![]()
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Affiliation(s)
- Jenni Kontkanen
- Institute for Atmospheric and Earth System Research, University of Helsinki, Helsinki, Finland
| | - Dominik Stolzenburg
- Institute for Atmospheric and Earth System Research, University of Helsinki, Helsinki, Finland
| | - Tinja Olenius
- Swedish Meteorological and Hydrological Institute, Norrköping, Sweden
| | - Chao Yan
- Institute for Atmospheric and Earth System Research, University of Helsinki, Helsinki, Finland
| | - Lubna Dada
- Institute for Atmospheric and Earth System Research, University of Helsinki, Helsinki, Finland
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Lauri Ahonen
- Institute for Atmospheric and Earth System Research, University of Helsinki, Helsinki, Finland
| | - Mario Simon
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research, University of Helsinki, Helsinki, Finland
- Finnish Meteorological Institute, Helsinki, Finland
| | - Ilona Riipinen
- Department of Environmental Science (ACES), Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
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21
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Qiao X, Yan C, Li X, Guo Y, Yin R, Deng C, Li C, Nie W, Wang M, Cai R, Huang D, Wang Z, Yao L, Worsnop DR, Bianchi F, Liu Y, Donahue NM, Kulmala M, Jiang J. Contribution of Atmospheric Oxygenated Organic Compounds to Particle Growth in an Urban Environment. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2021; 55:13646-13656. [PMID: 34585932 DOI: 10.1021/acs.est.1c02095] [Citation(s) in RCA: 9] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/13/2023]
Abstract
Gas-phase oxygenated organic molecules (OOMs) can contribute substantially to the growth of newly formed particles. However, the characteristics of OOMs and their contributions to particle growth rate are not well understood in urban areas, which have complex anthropogenic emissions and atmospheric conditions. We performed long-term measurement of gas-phase OOMs in urban Beijing during 2018-2019 using nitrate-based chemical ionization mass spectrometry. OOM concentrations showed clear seasonal variations, with the highest in the summer and the lowest in the winter. Correspondingly, calculated particle growth rates due to OOM condensation were highest in summer, followed by spring, autumn, and winter. One prominent feature of OOMs in this urban environment was a high fraction (∼75%) of nitrogen-containing OOMs. These nitrogen-containing OOMs contributed only 50-60% of the total growth rate led by OOM condensation, owing to their slightly higher volatility than non-nitrate OOMs. By comparing the calculated condensation growth rates and the observed particle growth rates, we showed that sulfuric acid and its clusters are the main contributors to the growth of sub-3 nm particles, with OOMs significantly promoting the growth of 3-25 nm particles. In wintertime Beijing, however, there are missing contributors to the growth of particles above 3 nm, which remain to be further investigated.
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Affiliation(s)
- Xiaohui Qiao
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, P. R. China
| | - Chao Yan
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, P. R. China
| | - Xiaoxiao Li
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, P. R. China
| | - YiShuo Guo
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, P. R. China
| | - Rujing Yin
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, P. R. China
| | - Chenjuan Deng
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, P. R. China
| | - Chang Li
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, P. R. China
| | - Wei Nie
- Joint International research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, P. R. China
| | - Mingyi Wang
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Runlong Cai
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, P. R. China
| | - Dandan Huang
- State Environmental Protection Key Laboratory of Formation and Prevention of Urban Air Pollution Complex, Shanghai Academy of Environmental Sciences, Shanghai 200233, P. R. China
| | - Zhe Wang
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Hong Kong SAR 999077, P. R. China
| | - Lei Yao
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Douglas R Worsnop
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerodyne Research Incoporated, Billerica, Massachusetts 01821, United States
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, P. R. China
| | - Yongchun Liu
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, P. R. China
| | - Neil M Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, P. R. China
| | - Jingkun Jiang
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, 100084 Beijing, P. R. China
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22
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Surdu M, Pospisilova V, Xiao M, Wang M, Mentler B, Simon M, Stolzenburg D, Hoyle CR, Bell DM, Lee CP, Lamkaddam H, Lopez-Hilfiker F, Ahonen LR, Amorim A, Baccarini A, Chen D, Dada L, Duplissy J, Finkenzeller H, He XC, Hofbauer V, Kim C, Kürten A, Kvashnin A, Lehtipalo K, Makhmutov V, Molteni U, Nie W, Onnela A, Petäjä T, Quéléver LLJ, Tauber C, Tomé A, Wagner R, Yan C, Prevot ASH, Dommen J, Donahue NM, Hansel A, Curtius J, Winkler PM, Kulmala M, Volkamer R, Flagan RC, Kirkby J, Worsnop DR, Slowik JG, Wang DS, Baltensperger U, El Haddad I. Molecular characterization of ultrafine particles using extractive electrospray time-of-flight mass spectrometry. ACTA ACUST UNITED AC 2021; 1:434-448. [PMID: 34604755 PMCID: PMC8459645 DOI: 10.1039/d1ea00050k] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/26/2021] [Accepted: 08/10/2021] [Indexed: 12/12/2022]
Abstract
Aerosol particles negatively affect human health while also having climatic relevance due to, for example, their ability to act as cloud condensation nuclei. Ultrafine particles (diameter Dp < 100 nm) typically comprise the largest fraction of the total number concentration, however, their chemical characterization is difficult because of their low mass. Using an extractive electrospray time-of-flight mass spectrometer (EESI-TOF), we characterize the molecular composition of freshly nucleated particles from naphthalene and β-caryophyllene oxidation products at the CLOUD chamber at CERN. We perform a detailed intercomparison of the organic aerosol chemical composition measured by the EESI-TOF and an iodide adduct chemical ionization mass spectrometer equipped with a filter inlet for gases and aerosols (FIGAERO-I-CIMS). We also use an aerosol growth model based on the condensation of organic vapors to show that the chemical composition measured by the EESI-TOF is consistent with the expected condensed oxidation products. This agreement could be further improved by constraining the EESI-TOF compound-specific sensitivity or considering condensed-phase processes. Our results show that the EESI-TOF can obtain the chemical composition of particles as small as 20 nm in diameter with mass loadings as low as hundreds of ng m−3 in real time. This was until now difficult to achieve, as other online instruments are often limited by size cutoffs, ionization/thermal fragmentation and/or semi-continuous sampling. Using real-time simultaneous gas- and particle-phase data, we discuss the condensation of naphthalene oxidation products on a molecular level. Using real-time simultaneous gas- and particle-phase data, the condensation of naphthalene and β-caryophyllene oxidation products on a molecular level is discussed.![]()
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Affiliation(s)
- Mihnea Surdu
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Veronika Pospisilova
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Mao Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Mingyi Wang
- Center for Atmospheric Particle Studies, Carnegie Mellon University 15213 Pittsburgh PA USA
| | - Bernhard Mentler
- Institute of Ion Physics and Applied Physics, University of Innsbruck 6020 Innsbruck Austria
| | - Mario Simon
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Dominik Stolzenburg
- Faculty of Physics, University of Vienna 1090 Vienna Austria.,Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Christopher R Hoyle
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland .,Institute for Atmospheric and Climate Science, ETH Zurich 8006 Zurich Switzerland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Chuan Ping Lee
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Houssni Lamkaddam
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Felipe Lopez-Hilfiker
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Lauri R Ahonen
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Antonio Amorim
- CENTRA, FCUL, University of Lisbon 1749-016 Lisbon Portugal
| | - Andrea Baccarini
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland .,School of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne 1015 Lausanne Switzerland
| | - Dexian Chen
- Center for Atmospheric Particle Studies, Carnegie Mellon University 15213 Pittsburgh PA USA
| | - Lubna Dada
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland .,Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Jonathan Duplissy
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland.,Helsinki Institute of Physics, University of Helsinki 00014 Helsinki Finland
| | - Henning Finkenzeller
- Department of Chemistry, CIRES, University of Colorado Boulder 80309 Boulder CO USA
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Victoria Hofbauer
- Center for Atmospheric Particle Studies, Carnegie Mellon University 15213 Pittsburgh PA USA
| | - Changhyuk Kim
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41 Pasadena CA 91125 USA.,School of Civil and Environmental Engineering, Pusan National University Busan 46241 Republic of Korea
| | - Andreas Kürten
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Aleksandr Kvashnin
- P. N. Lebedev Physical Institute of the Russian Academy of Sciences, Laboratory of Solar and Cosmic Ray Physics 119991 Moscow Russia
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland.,Finnish Meteorological Institute 00560 Helsinki Finland
| | - Vladimir Makhmutov
- P. N. Lebedev Physical Institute of the Russian Academy of Sciences, Laboratory of Solar and Cosmic Ray Physics 119991 Moscow Russia
| | - Ugo Molteni
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Wei Nie
- Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences, Nanjing University Nanjing China
| | | | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Lauriane L J Quéléver
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | | | - António Tomé
- IDL-Universidade da Beira Interior 6201-001 Covilhã Portugal
| | - Robert Wagner
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Chao Yan
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Andre S H Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Neil M Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University 15213 Pittsburgh PA USA
| | - Armin Hansel
- Institute of Ion Physics and Applied Physics, University of Innsbruck 6020 Innsbruck Austria
| | - Joachim Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Paul M Winkler
- Faculty of Physics, University of Vienna 1090 Vienna Austria
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland.,Helsinki Institute of Physics, University of Helsinki 00014 Helsinki Finland
| | - Rainer Volkamer
- Department of Chemistry, CIRES, University of Colorado Boulder 80309 Boulder CO USA
| | - Richard C Flagan
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41 Pasadena CA 91125 USA
| | - Jasper Kirkby
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany.,CERN 1211 Geneva Switzerland
| | - Douglas R Worsnop
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland.,Aerodyne Research 01821 Billerica MA USA
| | - Jay G Slowik
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Dongyu S Wang
- 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
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23
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Eleftheriadis K, Gini MI, Diapouli E, Vratolis S, Vasilatou V, Fetfatzis P, Manousakas MI. Aerosol microphysics and chemistry reveal the COVID19 lockdown impact on urban air quality. Sci Rep 2021; 11:14477. [PMID: 34262082 PMCID: PMC8280149 DOI: 10.1038/s41598-021-93650-6] [Citation(s) in RCA: 6] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/07/2020] [Accepted: 06/24/2021] [Indexed: 11/09/2022] Open
Abstract
Air quality in urban areas and megacities is dependent on emissions, physicochemical process and atmospheric conditions in a complex manner. The impact on air quality metrics of the COVID-19 lockdown measures was evaluated during two periods in Athens, Greece. The first period involved stoppage of educational and recreational activities and the second severe restrictions to all but necessary transport and workplace activities. Fresh traffic emissions and their aerosol products in terms of ultrafine nuclei particles and nitrates showed the most significant reduction especially during the 2nd period (40–50%). Carbonaceous aerosol both from fossil fuel emissions and biomass burning, as well as aging ultrafine and accumulation mode particles showed an increase of 10–20% of average before showing a decline (5 to 30%). It is found that removal of small nuclei and Aitken modes increased growth rates and migration of condensable species to larger particles maintaining aerosol volume.
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Affiliation(s)
| | - Maria I Gini
- Environmental Research Laboratory, INRASTES, NCSR Demokritos, 15310 Ag. Paraskevi, Athens, Greece
| | - Evangelia Diapouli
- Environmental Research Laboratory, INRASTES, NCSR Demokritos, 15310 Ag. Paraskevi, Athens, Greece
| | - Stergios Vratolis
- Environmental Research Laboratory, INRASTES, NCSR Demokritos, 15310 Ag. Paraskevi, Athens, Greece
| | - Vasiliki Vasilatou
- Environmental Research Laboratory, INRASTES, NCSR Demokritos, 15310 Ag. Paraskevi, Athens, Greece
| | - Prodromos Fetfatzis
- Environmental Research Laboratory, INRASTES, NCSR Demokritos, 15310 Ag. Paraskevi, Athens, Greece
| | - Manousos I Manousakas
- Environmental Research Laboratory, INRASTES, NCSR Demokritos, 15310 Ag. Paraskevi, Athens, Greece.,LAC, Paul Scherrer Institute, Villigen PSI, Switzerland
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24
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Shen J, Bigi A, Marinoni A, Lampilahti J, Kontkanen J, Ciarelli G, Putaud JP, Nieminen T, Kulmala M, Lehtipalo K, Bianchi F. Emerging Investigator Series: COVID-19 lockdown effects on aerosol particle size distributions in northern Italy. ACTA ACUST UNITED AC 2021; 1:214-227. [PMID: 34355190 PMCID: PMC8296575 DOI: 10.1039/d1ea00016k] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/09/2021] [Accepted: 06/07/2021] [Indexed: 11/28/2022]
Abstract
The lockdown measures implemented to curb the COVID-19 epidemic in Italy reduced human mobility dramatically, which resulted in a marked decline in traffic intensity. In this study, we present the effect of lockdown measures on several air pollutants, particle number size distribution as well as on regional new particle formation (NPF) frequency in the Po Valley (northern Italy). The results show that during the lockdown period, concentrations of nitrogen dioxide (NO2), nitric oxide (NO), benzene (C6H6), and toluene (C7H8) decreased, while ozone (O3) concentrations mildly increased as compared to the corresponding period in 2016–2019. Unlike gaseous pollutants, particulate matter mass concentrations (PM2.5 and PM10) showed no significant changes. The impact of lockdown measures on particle number size distributions were also quite limited. During the lockdown period, the number concentrations of 10–25 and 25–50 nm primary particles were reduced by 66% and 34%, respectively, at the regional background site (Ispra) but surprisingly there was no difference during and after lockdown at the urban background site (Modena). Conversely, the NPF frequency was exceptionally high, 70%, in Modena during the lockdown as compared to values (22–26%) observed for the same period in 2006 and 2009, while NPF frequency in Ispra only slightly increased compared to the same period in 2016–2019. The particle growth rates, however, were slightly lower during the lockdown at both sites compared to other periods. The study shows that a drastic decrease in traffic had little influence on particulate pollution levels in the Po Valley, suggesting that other sources and processes also have a prominent impact on particle number and particulate matter mass concentration in this region. Impact of lockdown measures on the air pollutants and particle number size distribution.![]()
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Affiliation(s)
- Jiali Shen
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland
| | - Alessandro Bigi
- Department of Engineering "Enzo Ferrari", Università di Modena e Reggio Emilia Modena Italy
| | - Angela Marinoni
- Institute of Atmospheric Sciences and Climate, National Research Council of Italy Bologna Italy
| | - Janne Lampilahti
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland
| | - Jenni Kontkanen
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland
| | - Giancarlo Ciarelli
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland
| | - Jean P Putaud
- European Commission, Joint Research Centre (JRC) Ispra Italy
| | - Tuomo Nieminen
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland .,Institute for Atmospheric and Earth System Research/Forest Sciences, Faculty of Agriculture and Forestry, University of Helsinki Finland
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland .,Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology Beijing China.,Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University Nanjing China
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland .,Finnish Meteorological Institute Helsinki Finland
| | - Federico Bianchi
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Finland
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25
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Tang L, Shang D, Fang X, Wu Z, Qiu Y, Chen S, Li X, Zeng L, Guo S, Hu M. More Significant Impacts From New Particle Formation on Haze Formation During COVID-19 Lockdown. GEOPHYSICAL RESEARCH LETTERS 2021; 48:e2020GL091591. [PMID: 34149114 PMCID: PMC8206662 DOI: 10.1029/2020gl091591] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/06/2020] [Revised: 02/02/2021] [Accepted: 02/18/2021] [Indexed: 05/09/2023]
Abstract
During the COVID-19 lockdown in 2020, large-scale industrial and transportation emissions were reduced, but high PM2.5 concentration still occurred. This study investigated the variation of particle number size distribution during the lockdown, and analyzed the characteristics of new particle formation (NPF) events and its potential impact on haze formation. Through measurement conducted in urban Beijing during the first 3 months of 2020, and comparison with year-over-year data, the decrease of primary Aitken-mode particles was observed. However, frequencies, formation rates and growth rates of NPF events remained stable between 2020 and 2019 in the same period. As a result, >25 nm particles produced by NPF events, would play a more important role in serving as the haze formation "seeds" compared to those produced by primary emissions. This finding emphasizes the significance on the understanding of NPF mechanisms when making pollution mitigation policy in the future.
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Affiliation(s)
- Lizi Tang
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
| | - Dongjie Shang
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
| | - Xin Fang
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
| | - Zhijun Wu
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
- Collaborative Innovation Center of Atmospheric Environment and Equipment TechnologyNanjing University of Information Science & TechnologyNanjingChina
| | - Yanting Qiu
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
| | - Shiyi Chen
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
| | - Xin Li
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
- Collaborative Innovation Center of Atmospheric Environment and Equipment TechnologyNanjing University of Information Science & TechnologyNanjingChina
| | - Limin Zeng
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
- Collaborative Innovation Center of Atmospheric Environment and Equipment TechnologyNanjing University of Information Science & TechnologyNanjingChina
| | - Song Guo
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
- Collaborative Innovation Center of Atmospheric Environment and Equipment TechnologyNanjing University of Information Science & TechnologyNanjingChina
| | - Min Hu
- State Key Joint Laboratory of Environmental Simulation and Pollution ControlInternational Joint Laboratory for Regional Pollution ControlMinistry of Education (IJRC)College of Environmental Sciences and EngineeringPeking UniversityBeijingChina
- Collaborative Innovation Center of Atmospheric Environment and Equipment TechnologyNanjing University of Information Science & TechnologyNanjingChina
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26
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Wang M, Chen D, Xiao M, Ye Q, Stolzenburg D, Hofbauer V, Ye P, Vogel AL, Mauldin RL, Amorim A, Baccarini A, Baumgartner B, Brilke S, Dada L, Dias A, Duplissy J, Finkenzeller H, Garmash O, He XC, Hoyle CR, Kim C, Kvashnin A, Lehtipalo K, Fischer L, Molteni U, Petäjä T, Pospisilova V, Quéléver LLJ, Rissanen M, Simon M, Tauber C, Tomé A, Wagner AC, Weitz L, Volkamer R, Winkler PM, Kirkby J, Worsnop DR, Kulmala M, Baltensperger U, Dommen J, El-Haddad I, Donahue NM. Photo-oxidation of Aromatic Hydrocarbons Produces Low-Volatility Organic Compounds. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2020; 54:7911-7921. [PMID: 32515954 DOI: 10.1021/acs.est.0c02100] [Citation(s) in RCA: 26] [Impact Index Per Article: 6.5] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/11/2023]
Abstract
To better understand the role of aromatic hydrocarbons in new-particle formation, we measured the particle-phase abundance and volatility of oxidation products following the reaction of aromatic hydrocarbons with OH radicals. For this we used thermal desorption in an iodide-adduct Time-of-Flight Chemical-Ionization Mass Spectrometer equipped with a Filter Inlet for Gases and AEROsols (FIGAERO-ToF-CIMS). The particle-phase volatility measurements confirm that oxidation products of toluene and naphthalene can contribute to the initial growth of newly formed particles. Toluene-derived (C7) oxidation products have a similar volatility distribution to that of α-pinene-derived (C10) oxidation products, while naphthalene-derived (C10) oxidation products are much less volatile than those from toluene or α-pinene; they are thus stronger contributors to growth. Rapid progression through multiple generations of oxidation is more pronounced in toluene and naphthalene than in α-pinene, resulting in more oxidation but also favoring functional groups with much lower volatility per added oxygen atom, such as hydroxyl and carboxylic groups instead of hydroperoxide groups. Under conditions typical of polluted urban settings, naphthalene may well contribute to nucleation and the growth of the smallest particles, whereas the more abundant alkyl benzenes may overtake naphthalene once the particles have grown beyond the point where the Kelvin effect strongly influences the condensation driving force.
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Affiliation(s)
- Mingyi Wang
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Dexian Chen
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Mao Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Qing Ye
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | | | - Victoria Hofbauer
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Penglin Ye
- Aerodyne Research, Incorporated, Billerica, Massachusetts 01821, United States
| | - Alexander L Vogel
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany
| | - Roy L Mauldin
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Oceanic and Atmospheric Science, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Antonio Amorim
- CENTRA and FCUL, University of Lisbon, 1749-016 Lisbon, Portugal
| | - Andrea Baccarini
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | | | - Sophia Brilke
- Faculty of Physics, University of Vienna, 1090 Vienna, Austria
| | - Lubna Dada
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
| | - António Dias
- CENTRA and FCUL, University of Lisbon, 1749-016 Lisbon, Portugal
| | - Jonathan Duplissy
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
- Helsinki Institute of Physics, University of Helsinki, 00014 Helsinki, Finland
| | - Henning Finkenzeller
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Olga Garmash
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
| | - Christopher R Hoyle
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland
| | - Changhyuk Kim
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, California 91125, United States
- Department of Environmental Engineering, Pusan National University, Busan, 46241, Republic of Korea
| | | | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
- Finnish meteorological Institute, Erik Palménin aukio 1, 00560 Helsinki, Finland
| | - Lukas Fischer
- Institute for Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
| | - Ugo Molteni
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
| | - Veronika Pospisilova
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Lauriane L J Quéléver
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
| | - Matti Rissanen
- Aerosol Physics Laboratory, Physics Unit, Tampere University, P.O. Box 1001, Tampere 33100, Finland
| | - Mario Simon
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany
| | | | - António Tomé
- IDL-University of Beira Interior, Covilhã 6201-001, Portugal
| | - Andrea C Wagner
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Lena Weitz
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany
| | - Rainer Volkamer
- Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Paul M Winkler
- Faculty of Physics, University of Vienna, 1090 Vienna, Austria
| | - Jasper Kirkby
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany
- CERN, 1211 Geneva, Switzerland
| | - Douglas R Worsnop
- Aerodyne Research, Incorporated, Billerica, Massachusetts 01821, United States
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland
- Helsinki Institute of Physics, University of Helsinki, 00014 Helsinki, Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, Nanjing University, Nanjing 210044, P. R. China
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing 100029, P. R. China
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Imad El-Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Neil M Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
- Department of Engineering and Public Policy, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
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