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Li Y, Devenish C, Tosa MI, Luo M, Bell DM, Lesmeister DB, Greenfield P, Pichler M, Levi T, Yu DW. Combining environmental DNA and remote sensing for efficient, fine-scale mapping of arthropod biodiversity. Philos Trans R Soc Lond B Biol Sci 2024; 379:20230123. [PMID: 38705177 PMCID: PMC11070265 DOI: 10.1098/rstb.2023.0123] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/31/2023] [Accepted: 01/31/2024] [Indexed: 05/07/2024] Open
Abstract
Arthropods contribute importantly to ecosystem functioning but remain understudied. This undermines the validity of conservation decisions. Modern methods are now making arthropods easier to study, since arthropods can be mass-trapped, mass-identified, and semi-mass-quantified into 'many-row (observation), many-column (species)' datasets, with homogeneous error, high resolution, and copious environmental-covariate information. These 'novel community datasets' let us efficiently generate information on arthropod species distributions, conservation values, uncertainty, and the magnitude and direction of human impacts. We use a DNA-based method (barcode mapping) to produce an arthropod-community dataset from 121 Malaise-trap samples, and combine it with 29 remote-imagery layers using a deep neural net in a joint species distribution model. With this approach, we generate distribution maps for 76 arthropod species across a 225 km2 temperate-zone forested landscape. We combine the maps to visualize the fine-scale spatial distributions of species richness, community composition, and site irreplaceability. Old-growth forests show distinct community composition and higher species richness, and stream courses have the highest site-irreplaceability values. With this 'sideways biodiversity modelling' method, we demonstrate the feasibility of biodiversity mapping at sufficient spatial resolution to inform local management choices, while also being efficient enough to scale up to thousands of square kilometres. This article is part of the theme issue 'Towards a toolkit for global insect biodiversity monitoring'.
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Affiliation(s)
- Yuanheng Li
- Yunnan Key Laboratory of Biodiversity and Ecological Security of Gaoligong Mountain, State Key Laboratory of Genetic Resources and Evolution, Chinese Academy of Sciences, Kunming, Yunnan 650223, People’s Republic of China
- Kunming Institute of Zoology, Chinese Academy of Sciences, Kunming, Yunnan 650223, People’s Republic of China
- Faculty of Biology, University of Duisburg-Essen, Essen 45141, Germany
| | - Christian Devenish
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, Norfolk NR47TJ, UK
| | - Marie I. Tosa
- Department of Fisheries, Wildlife, and Conservation Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - Mingjie Luo
- Yunnan Key Laboratory of Biodiversity and Ecological Security of Gaoligong Mountain, State Key Laboratory of Genetic Resources and Evolution, Chinese Academy of Sciences, Kunming, Yunnan 650223, People’s Republic of China
- Kunming Institute of Zoology, Chinese Academy of Sciences, Kunming, Yunnan 650223, People’s Republic of China
- Kunming College of Life Sciences, University of Chinese Academy of Sciences, Kunming, People’s Republic of China
| | - David M. Bell
- Pacific Northwest Research Station, U.S. Department of Agriculture Forest Service, Corvallis, OR 97331, USA
| | - Damon B. Lesmeister
- Department of Fisheries, Wildlife, and Conservation Sciences, Oregon State University, Corvallis, OR 97331, USA
- Pacific Northwest Research Station, U.S. Department of Agriculture Forest Service, Corvallis, OR 97331, USA
| | - Paul Greenfield
- CSIRO Energy, Lindfield, New South Wales, Australia
- School of Biological Sciences, Macquarie University, Sydney, Australia
| | | | - Taal Levi
- Department of Fisheries, Wildlife, and Conservation Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - Douglas W. Yu
- Yunnan Key Laboratory of Biodiversity and Ecological Security of Gaoligong Mountain, State Key Laboratory of Genetic Resources and Evolution, Chinese Academy of Sciences, Kunming, Yunnan 650223, People’s Republic of China
- Kunming Institute of Zoology, Chinese Academy of Sciences, Kunming, Yunnan 650223, People’s Republic of China
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, Norfolk NR47TJ, UK
- Center for Excellence in Animal Evolution and Genetics, Chinese Academy of Sciences, Kunming Yunnan 650223, People’s Republic of China
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Li K, Zhang J, Bell DM, Wang T, Lamkaddam H, Cui T, Qi L, Surdu M, Wang D, Du L, El Haddad I, Slowik JG, Prevot ASH. Uncovering the dominant contribution of intermediate volatility compounds in secondary organic aerosol formation from biomass-burning emissions. Natl Sci Rev 2024; 11:nwae014. [PMID: 38390366 PMCID: PMC10883696 DOI: 10.1093/nsr/nwae014] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/18/2023] [Revised: 01/07/2024] [Accepted: 01/08/2024] [Indexed: 02/24/2024] Open
Abstract
Organic vapors from biomass burning are a major source of secondary organic aerosols (SOAs). Previous smog chamber studies found that the SOA contributors in biomass-burning emissions are mainly volatile organic compounds (VOCs). While intermediate volatility organic compounds (IVOCs) are efficient SOA precursors and contribute a considerable fraction of biomass-burning emissions, their contribution to SOA formation has not been directly observed. Here, by deploying a newly-developed oxidation flow reactor to study SOA formation from wood burning, we find that IVOCs can contribute ∼70% of the formed SOA, i.e. >2 times more than VOCs. This previously missing SOA fraction is interpreted to be due to the high wall losses of semi-volatile oxidation products of IVOCs in smog chambers. The finding in this study reveals that SOA production from biomass burning is much higher than previously thought, and highlights the urgent need for more research on the IVOCs from biomass burning and potentially other emission sources.
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Affiliation(s)
- Kun Li
- Environment Research Institute, Shandong University, Qingdao 266237, China
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Jun Zhang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Tiantian Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Houssni Lamkaddam
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Tianqu Cui
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Lu Qi
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Mihnea Surdu
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Dongyu Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Lin Du
- Environment Research Institute, Shandong University, Qingdao 266237, China
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Jay G Slowik
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Andre S H Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
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3
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Marten R, Xiao M, Wang M, Kong W, He XC, Stolzenburg D, Pfeifer J, Marie G, Wang DS, Elser M, Baccarini A, Lee CP, Amorim A, Baalbaki R, Bell DM, Bertozzi B, Caudillo L, Dada L, Duplissy J, Finkenzeller H, Heinritzi M, Lampimäki M, Lehtipalo K, Manninen HE, Mentler B, Onnela A, Petäjä T, Philippov M, Rörup B, Scholz W, Shen J, Tham YJ, Tomé A, Wagner AC, Weber SK, Zauner-Wieczorek M, Curtius J, Kulmala M, Volkamer R, Worsnop DR, Dommen J, Flagan RC, Kirkby J, McPherson Donahue N, Lamkaddam H, Baltensperger U, El Haddad I. Assessing the importance of nitric acid and ammonia for particle growth in the polluted boundary layer. Environ Sci Atmos 2024; 4:265-274. [PMID: 38371605 PMCID: PMC10867809 DOI: 10.1039/d3ea00001j] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/02/2023] [Accepted: 12/07/2023] [Indexed: 02/20/2024]
Abstract
Aerosols formed and grown by gas-to-particle processes are a major contributor to smog and haze in megacities, despite the competition between growth and loss rates. Rapid growth rates from ammonium nitrate formation have the potential to sustain particle number in typical urban polluted conditions. This process requires supersaturation of gas-phase ammonia and nitric acid with respect to ammonium nitrate saturation ratios. Urban environments are inhomogeneous. In the troposphere, vertical mixing is fast, and aerosols may experience rapidly changing temperatures. In areas close to sources of pollution, gas-phase concentrations can also be highly variable. In this work we present results from nucleation experiments at -10 °C and 5 °C in the CLOUD chamber at CERN. We verify, using a kinetic model, how long supersaturation is likely to be sustained under urban conditions with temperature and concentration inhomogeneities, and the impact it may have on the particle size distribution. We show that rapid and strong temperature changes of 1 °C min-1 are needed to cause rapid growth of nanoparticles through ammonium nitrate formation. Furthermore, inhomogeneous emissions of ammonia in cities may also cause rapid growth of particles.
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Affiliation(s)
- Ruby Marten
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Mao Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Mingyi Wang
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41 Pasadena CA 91125 USA
| | - Weimeng Kong
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41 Pasadena CA 91125 USA
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
- Finnish Meteorological Institute FI-00560 Helsinki Finland
| | - Dominik Stolzenburg
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
- Institute for Materials Chemistry, TU Wien 1060 Vienna Austria
| | - Joschka Pfeifer
- CERN CH-1211 Geneva Switzerland
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Guillaume Marie
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Dongyu S Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Miriam Elser
- Empa, Swiss Federal Laboratories for Materials Science and Technology Dübendorf Switzerland
| | - Andrea Baccarini
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
- Atmospheric Processes and Their Impact, École Polytechnique Fédérale de Lausanne 1015 Lausanne Switzerland
| | - Chuan Ping Lee
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Antonio Amorim
- CENTRA, FCUL, University of Lisbon 1749-016 Lisbon Portugal
| | - Rima Baalbaki
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Barbara Bertozzi
- Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology 76021 Karlsruhe Germany
| | - Lucía Caudillo
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Lubna Dada
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Jonathan Duplissy
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
- Helsinki Institute of Physics (HIP)/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Henning Finkenzeller
- Department of Chemistry, CIRES, University of Colorado Boulder 215 UCB Boulder 80309 CO USA
| | - Martin Heinritzi
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Markus Lampimäki
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
- Finnish Meteorological Institute FI-00560 Helsinki Finland
| | | | - Bernhard Mentler
- Institute of Ion Physics and Applied Physics, University of Innsbruck 6020 Innsbruck Austria
| | | | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Maxim Philippov
- Lebedev Physical Institute of the Russian Academy of Sciences 119991 Leninsky prospekt, 53 Moscow Russian Federation
| | - Birte Rörup
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Wiebke Scholz
- Institute of Ion Physics and Applied Physics, University of Innsbruck 6020 Innsbruck Austria
| | - Jiali Shen
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Yee Jun Tham
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - António Tomé
- IDL-Universidade da Beira Interior 6201-001 Covilhã 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 215 UCB Boulder 80309 CO USA
- Aerosol Physics Laboratory, Physics Unit, Tampere University FI-33014 Tampere Finland
| | - Stefan K Weber
- CERN CH-1211 Geneva Switzerland
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Marcel Zauner-Wieczorek
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Joachim Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
| | - Rainer Volkamer
- Department of Chemistry, CIRES, University of Colorado Boulder 215 UCB Boulder 80309 CO USA
| | - Douglas R Worsnop
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki 00014 Helsinki Finland
- Aerodyne Research 01821 Billerica MA USA
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute 5232 Villigen Switzerland
| | - Richard C Flagan
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41 Pasadena CA 91125 USA
| | - Jasper Kirkby
- CERN CH-1211 Geneva Switzerland
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt 60438 Frankfurt am Main Germany
| | - Neil McPherson Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University 1521 Pittsburgh PA USA
| | - Houssni Lamkaddam
- 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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4
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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. Environ Sci Technol 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] [What about the content of this article? (0)] [Affiliation(s)] [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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5
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Bell DM, Zhang J, Top J, Bogler S, Surdu M, Slowik JG, Prevot ASH, El Haddad I. Sensitivity Constraints of Extractive Electrospray for a Model System and Secondary Organic Aerosol. Anal Chem 2023; 95:13788-13795. [PMID: 37656668 PMCID: PMC10515109 DOI: 10.1021/acs.analchem.3c00441] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/30/2023] [Accepted: 08/11/2023] [Indexed: 09/03/2023]
Abstract
The quantification of an aerosol chemical composition is complicated by the uncertainty in the sensitivity of each species detected. Soft-ionization response factors can vary widely from molecule to molecule. Here, we have employed a method to separate molecules by their volatility through systematic evaporation with a thermal denuder (TD). The fraction remaining after evaporation is compared between an extractive electrospray ionization time-of-flight mass spectrometer (EESI-TOF) and a scanning mobility particle sizer (SMPS), which provides a comparison between a quantified mass loss by the SMPS and the signal loss in the EESI-TOF. The sensitivity of the EESI-TOF is determined for both a simplified complex mixture (PEG-300) and also for a complex mixture of α-pinene secondary organic aerosol (SOA). For PEG-300, separation is possible on a molecule-by-molecule level with the TD and provides insights into the molecule-dependent sensitivity of the EESI-TOF, showing a higher sensitivity toward the most volatile molecule. For α-pinene SOA, sensitivity determination for specific classes is possible because of the number of molecular formula observed by the EESI-TOF. These classes are separated by their volatility and are broken down into monomers (O3-5,6-7,8+), dimers (O4-7,8+), and higher order oligomers (e.g., trimers and tetramers). Here, we show that the EESI-TOF initially measures 60.1% monomers, 32.7% dimers, and 7.2% trimers and tetramers in α-pinene SOA, but after sensitivity correction, the distribution of SOA is 37.4% monomers, 56.1% dimers, and 6.4% trimers and tetramers. These results provide a path forward for the quantification of aerosol components with the EESI-TOF in other applications and potentially for atmospheric measurements.
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Affiliation(s)
- David M. Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Jun Zhang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Jens Top
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Sophie Bogler
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Mihnea Surdu
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Jay G. Slowik
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Andre S. H. Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
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6
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Kumar V, Slowik JG, Baltensperger U, Prevot ASH, Bell DM. Time-Resolved Molecular Characterization of Secondary Organic Aerosol Formed from OH and NO 3 Radical Initiated Oxidation of a Mixture of Aromatic Precursors. Environ Sci Technol 2023; 57:11572-11582. [PMID: 37496264 PMCID: PMC10413940 DOI: 10.1021/acs.est.3c00225] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/09/2023] [Revised: 07/06/2023] [Accepted: 07/07/2023] [Indexed: 07/28/2023]
Abstract
Aromatic hydrocarbons (ArHCs) and oxygenated aromatic hydrocarbons (ArHC-OHs) are emitted from a variety of anthropogenic activities and are important precursors of secondary organic aerosol (SOA) in urban areas. Here, we analyzed and compared the composition of SOA formed from the oxidation of a mixture of aromatic VOCs by OH and NO3 radicals. The VOC mixture was composed of toluene (C7H8), p-xylene + ethylbenzene (C8H10), 1,3,5-trimethylbenzene (C9H12), phenol (C6H6O), cresol (C7H8O), 2,6-dimethylphenol (C8H10O), and 2,4,6-trimethylphenol (C9H12O) in a proportion where the aromatic VOCs were chosen to approximate day-time traffic-related emissions in Delhi, and the aromatic alcohols make up 20% of the mixture. These VOCs are prominent in other cities as well, including those influenced by biomass combustion. In the NO3 experiments, large contributions from CxHyOzN dimers (C15-C18) were observed, corresponding to fast SOA formation within 15-20 min after the start of chemistry. Additionally, the dimers were a mixture of different combinations of the initial VOCs, highlighting the importance of exploring SOAs from mixed VOC systems. In contrast, the experiments with OH radicals yielded gradual SOA mass formation, with CxHyOz monomers (C6-C9) being the dominant constituents. The evolution of SOA composition with time was tracked and a fast degradation of dimers was observed in the NO3 experiments, with concurrent formation of monomer species. The rates of dimer decomposition in NO3 SOA were ∼2-3 times higher compared to those previously determined for α-pinene + O3 SOA, highlighting the dependence of particle-phase reactions on VOC precursors and oxidants. In contrast, the SOA produced in the OH experiments did not dramatically change over the same time frame. No measurable effects of humidity were observed on the composition and evolution of SOA.
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Affiliation(s)
| | - Jay G. Slowik
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute (PSI), Villigen 5232, Switzerland
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute (PSI), Villigen 5232, Switzerland
| | - Andre S. H. Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute (PSI), Villigen 5232, Switzerland
| | - David M. Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute (PSI), Villigen 5232, Switzerland
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7
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Surdu M, Lamkaddam H, Wang DS, Bell DM, Xiao M, Lee CP, Li D, Caudillo L, Marie G, Scholz W, Wang M, Lopez B, Piedehierro AA, Ataei F, Baalbaki R, Bertozzi B, Bogert P, Brasseur Z, Dada L, Duplissy J, Finkenzeller H, He XC, Höhler K, Korhonen K, Krechmer JE, Lehtipalo K, Mahfouz NGA, Manninen HE, Marten R, Massabò D, Mauldin R, Petäjä T, Pfeifer J, Philippov M, Rörup B, Simon M, Shen J, Umo NS, Vogel F, Weber SK, Zauner-Wieczorek M, Volkamer R, Saathoff H, Möhler O, Kirkby J, Worsnop DR, Kulmala M, Stratmann F, Hansel A, Curtius J, Welti A, Riva M, Donahue NM, Baltensperger U, El Haddad I. Molecular Understanding of the Enhancement in Organic Aerosol Mass at High Relative Humidity. Environ Sci Technol 2023; 57:2297-2309. [PMID: 36716278 PMCID: PMC9933880 DOI: 10.1021/acs.est.2c04587] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/26/2022] [Revised: 10/11/2022] [Accepted: 11/21/2022] [Indexed: 06/18/2023]
Abstract
The mechanistic pathway by which high relative humidity (RH) affects gas-particle partitioning remains poorly understood, although many studies report increased secondary organic aerosol (SOA) yields at high RH. Here, we use real-time, molecular measurements of both the gas and particle phase to provide a mechanistic understanding of the effect of RH on the partitioning of biogenic oxidized organic molecules (from α-pinene and isoprene) at low temperatures (243 and 263 K) at the CLOUD chamber at CERN. We observe increases in SOA mass of 45 and 85% with increasing RH from 10-20 to 60-80% at 243 and 263 K, respectively, and attribute it to the increased partitioning of semi-volatile compounds. At 263 K, we measure an increase of a factor 2-4 in the concentration of C10H16O2-3, while the particle-phase concentrations of low-volatility species, such as C10H16O6-8, remain almost constant. This results in a substantial shift in the chemical composition and volatility distribution toward less oxygenated and more volatile species at higher RH (e.g., at 263 K, O/C ratio = 0.55 and 0.40, at RH = 10 and 80%, respectively). By modeling particle growth using an aerosol growth model, which accounts for kinetic limitations, we can explain the enhancement in the semi-volatile fraction through the complementary effect of decreased compound activity and increased bulk-phase diffusivity. Our results highlight the importance of particle water content as a diluting agent and a plasticizer for organic aerosol growth.
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Affiliation(s)
- Mihnea Surdu
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - Houssni Lamkaddam
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - Dongyu S. Wang
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - David M. Bell
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - Mao Xiao
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - Chuan Ping Lee
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - Dandan Li
- Université
de Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, 69626 Villeurbanne, France
| | - Lucía Caudillo
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Guillaume Marie
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Wiebke Scholz
- Institute
for Ion and Applied Physics, University
of Innsbruck, 6020 Innsbruck, Austria
| | - Mingyi Wang
- Division
of Chemistry and Chemical Engineering, California
Institute of Technology, Pasadena, 91125 California, United States
- Center for
Atmospheric Particle Studies, Carnegie Mellon
University, 5000 Forbes Avenue, Pittsburgh, 15213 Pennsylvania, United States
| | - Brandon Lopez
- Center for
Atmospheric Particle Studies, Carnegie Mellon
University, 5000 Forbes Avenue, Pittsburgh, 15213 Pennsylvania, United States
| | | | - Farnoush Ataei
- Department
of Experimental Aerosol and Cloud Microphysics, Leibniz Institute for Tropospheric Research, 04318 Leipzig, Germany
| | - Rima Baalbaki
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Barbara Bertozzi
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76021 Karlsruhe, Germany
| | - Pia Bogert
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76021 Karlsruhe, Germany
| | - Zoé Brasseur
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Lubna Dada
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - 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, UCB 215, Boulder, 80309-0215 Colorado, United States
| | - Xu-Cheng He
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Kristina Höhler
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76021 Karlsruhe, Germany
| | - Kimmo Korhonen
- Department of Applied Physics, University
of Eastern Finland, P.O. Box 1627, 70211 Kuopio, Finland
| | | | - Katrianne Lehtipalo
- Finnish
Meteorological Institute, 00560 Helsinki, Finland
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Naser G. A. Mahfouz
- Atmospheric and Oceanic Sciences, Princeton
University, Princeton, 08540 New Jersey, United States
| | - Hanna E. Manninen
- CERN,
the European Organization for Nuclear Research, CH-1211 Geneva 23, Switzerland
| | - Ruby Marten
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, 5232 Villigen, Switzerland
| | - Dario Massabò
- Department of Physics, University of Genoa
& INFN, 16146 Genoa, Italy
| | - Roy Mauldin
- Department
of Chemistry, Carnegie Mellon
University, 4400 Fifth
Avenue, Pittsburgh, 15213 Pennsylvania, United States
- Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, UCB 311, Boulder, 80309 Colorado, United
States
| | - Tuukka Petäjä
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Joschka Pfeifer
- CERN,
the European Organization for Nuclear Research, CH-1211 Geneva 23, Switzerland
| | - Maxim Philippov
- P. N. Lebedev Physical Institute of the
Russian Academy of Sciences, 119991 Moscow, Russia
| | - Birte Rörup
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Mario Simon
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Jiali Shen
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Nsikanabasi Silas Umo
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76021 Karlsruhe, Germany
| | - Franziska Vogel
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76021 Karlsruhe, Germany
| | - Stefan K. Weber
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
- CERN,
the European Organization for Nuclear Research, CH-1211 Geneva 23, Switzerland
| | - Marcel Zauner-Wieczorek
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Rainer Volkamer
- Department
of Chemistry & CIRES, University
of Colorado Boulder, UCB 215, Boulder, 80309-0215 Colorado, United States
| | - Harald Saathoff
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76021 Karlsruhe, Germany
| | - Ottmar Möhler
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76021 Karlsruhe, Germany
| | - Jasper Kirkby
- CERN,
the European Organization for Nuclear Research, CH-1211 Geneva 23, Switzerland
| | - Douglas R. Worsnop
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerodyne Research, Inc., Billerica, 01821 Massachusetts, United States
| | - Markku Kulmala
- Institute
for Atmospheric and Earth System Research (INAR)/Physics, Faculty
of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Frank Stratmann
- Department
of Experimental Aerosol and Cloud Microphysics, Leibniz Institute for Tropospheric Research, 04318 Leipzig, Germany
| | - Armin Hansel
- Institute
for Ion 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
| | - André Welti
- Finnish
Meteorological Institute, 00560 Helsinki, Finland
| | - Matthieu Riva
- Université
de Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, 69626 Villeurbanne, France
- Tofwerk AG, CH-3600 Thun, Switzerland
| | - Neil M. Donahue
- Center for
Atmospheric Particle Studies, Carnegie Mellon
University, 5000 Forbes Avenue, Pittsburgh, 15213 Pennsylvania, United States
| | - 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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8
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Bell DM, Pospisilova V, Lopez-Hilfiker F, Bertrand A, Xiao M, Zhou X, Huang W, Wang DS, Lee CP, Dommen J, Baltensperger U, Prevot ASH, El Haddad I, Slowik JG. Effect of OH scavengers on the chemical composition of α-pinene secondary organic aerosol. Environ Sci Atmos 2023; 3:115-123. [PMID: 36743126 PMCID: PMC9850668 DOI: 10.1039/d2ea00105e] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 08/16/2022] [Accepted: 11/01/2022] [Indexed: 11/06/2022]
Abstract
OH scavengers are extensively used in studies of secondary organic aerosol (SOA) because they create an idealized environment where only a single oxidation pathway is occurring. Here, we present a detailed molecular characterization of SOA produced from α-pinene + O3 with a variety of OH scavengers using the extractive electrospray time-of-flight mass spectrometer in our atmospheric simulation chamber, which is complemented by characterizing the gas phase composition in flow reactor experiments. Under our experimental conditions, radical chemistry largely controls the composition of SOA. Besides playing their desired role in suppressing the reaction of α-pinene with OH, OH scavengers alter the reaction pathways of radicals produced from α-pinene + O3. This involves changing the HO2 : RO2 ratio, the identity of the RO2 radicals present, and the RO2 major sinks. As a result, the use of the OH scavengers has significant effects on the composition of SOA, including inclusions of scavenger molecules in SOA, the promotion of fragmentation reactions, and depletion of dimers formed via α-pinene RO2-RO2 reactions. To date fragmentation reactions and inclusion of OH scavenger products into secondary organic aerosol have not been reported in atmospheric simulation chamber studies. Therefore, care should be considered if and when to use an OH scavenger during experiments.
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Affiliation(s)
- David M. Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Veronika Pospisilova
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland,Tofwerk3600 ThunSwitzerland
| | - Felipe Lopez-Hilfiker
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland,Tofwerk3600 ThunSwitzerland
| | - Amelie Bertrand
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Mao Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Xueqin Zhou
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Wei Huang
- Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology76344 Eggenstein-LeopoldshafenGermany
| | - Dongyu S. Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Chuan Ping Lee
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Andre S. H. Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
| | - Jay G. Slowik
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute5232 VilligenSwitzerland
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9
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Bogler S, Daellenbach KR, Bell DM, Prévôt ASH, El Haddad I, Borduas-Dedekind N. Singlet Oxygen Seasonality in Aqueous PM 10 is Driven by Biomass Burning and Anthropogenic Secondary Organic Aerosol. Environ Sci Technol 2022; 56:15389-15397. [PMID: 36306277 DOI: 10.1021/acs.est.2c04554] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/16/2023]
Abstract
The first excited state of molecular oxygen is singlet-state oxygen (1O2), formed by indirect photochemistry of chromophoric organic matter. To determine whether 1O2 can be a competitive atmospheric oxidant, we must first quantify its production in organic aerosols (OA). Here, we report the spatiotemporal distribution of 1O2 over a 1-year dataset of PM10 extracts at two locations in Switzerland, representing a rural and suburban site. Using a chemical probe technique, we measured 1O2 steady-state concentrations with a seasonality over an order of magnitude peaking in wintertime at 4.59 ± 0.01 × 10-13 M and with a quantum yield of up to 2%. Next, we identified biomass burning and anthropogenic secondary OA (SOA) as the drivers for 1O2 formation in the PM10 aqueous extracts using source apportionment data. Importantly, the quantity, the amount of brown carbon present in PM10, and the quality, the chemical composition of the brown carbon present, influence the concentration of 1O2 sensitized in each extract. Anthropogenic SOA in the extracts were 4 times more efficient in sensitizing 1O2 than primary biomass burning aerosols. Last, we developed an empirical fit to estimate 1O2 concentrations based on PM10 components, unlocking the ability to estimate 1O2 from existing source apportionment data. Overall, 1O2 is likely a competitive photo-oxidant in PM10 since 1O2 is sensitized by ubiquitous biomass burning OA and anthropogenic SOA.
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Affiliation(s)
- Sophie Bogler
- Department of Environmental Science Systems, ETH Zurich, Zurich 8092, Switzerland
| | - Kaspar R Daellenbach
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - André S H Prévôt
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Nadine Borduas-Dedekind
- Department of Environmental Science Systems, ETH Zurich, Zurich 8092, Switzerland
- Department of Chemistry, University of British Columbia, Vancouver V6T 1Z1, Canada
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10
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Kim H, McComb BC, Frey SJK, Bell DM, Betts MG. Forest microclimate and composition mediate long-term trends of breeding bird populations. Glob Chang Biol 2022; 28:6180-6193. [PMID: 36065828 PMCID: PMC9825929 DOI: 10.1111/gcb.16353] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 03/28/2022] [Revised: 07/14/2022] [Accepted: 07/18/2022] [Indexed: 06/15/2023]
Abstract
Climate change is contributing to biodiversity redistributions and species declines. However, cooler microclimate conditions provided by old-growth forest structures compared with surrounding open or younger forests have been hypothesized to provide thermal refugia for species that are sensitive to climate warming and dampen the negative effects of warming on population trends of animals (i.e., the microclimate buffering hypothesis). In addition to thermal refugia, the compositional and structural diversity of old-growth forest vegetation itself may provide resources to species that are less available in forests with simpler structure (i.e., the insurance hypothesis). We used 8 years of breeding bird abundance data from a forested watershed, accompanied with sub-canopy temperature data, and ground- and LiDAR-based vegetation data to test these hypotheses and identify factors influencing bird population changes from 2011 to 2018. After accounting for imperfect detection, we found that for 5 of 20 bird species analyzed, abundance trends tended to be less negative or neutral at sites with cooler microclimates, which supports the microclimate buffering hypothesis. Negative effects of warming on two species were also reduced in locations with greater forest compositional diversity supporting the insurance hypothesis. We provide the first empirical evidence that complex forest structure and vegetation diversity confer microclimatic advantages to some animal populations in the face of climate change. Conservation of old-growth forests, or their characteristics in managed forests, could help slow the negative effects of climate warming on some breeding bird populations via microclimate buffering and possibly insurance effects.
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Affiliation(s)
- Hankyu Kim
- Department of Forest Ecosystems and Society, College of ForestryOregon State UniversityCorvallisOregonUSA
- Department of Forest and Wildlife Ecology, College of Agricultural and Life SciencesUniversity of Wisconsin‐MadisonMadisonWisconsinUSA
| | - Brenda C. McComb
- Department of Forest Ecosystems and Society, College of ForestryOregon State UniversityCorvallisOregonUSA
- Forest Biodiversity Research Network, College of ForestryOregon State UniversityCorvallisOregonUSA
| | - Sarah J. K. Frey
- Department of Forest Ecosystems and Society, College of ForestryOregon State UniversityCorvallisOregonUSA
- Forest Biodiversity Research Network, College of ForestryOregon State UniversityCorvallisOregonUSA
| | - David M. Bell
- Pacific Northwest Research StationUSDA Forest ServiceCorvallisOregonUSA
| | - Matthew G. Betts
- Department of Forest Ecosystems and Society, College of ForestryOregon State UniversityCorvallisOregonUSA
- Forest Biodiversity Research Network, College of ForestryOregon State UniversityCorvallisOregonUSA
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11
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Shen J, Scholz W, He XC, Zhou P, Marie G, Wang M, Marten R, Surdu M, Rörup B, Baalbaki R, Amorim A, Ataei F, Bell DM, Bertozzi B, Brasseur Z, Caudillo L, Chen D, Chu B, Dada L, Duplissy J, Finkenzeller H, Granzin M, Guida R, Heinritzi M, Hofbauer V, Iyer S, Kemppainen D, Kong W, Krechmer JE, Kürten A, Lamkaddam H, Lee CP, Lopez B, Mahfouz NGA, Manninen HE, Massabò D, Mauldin RL, Mentler B, Müller T, Pfeifer J, Philippov M, Piedehierro AA, Roldin P, Schobesberger S, Simon M, Stolzenburg D, Tham YJ, Tomé A, Umo NS, Wang D, Wang Y, Weber SK, Welti A, Wollesen de Jonge R, Wu Y, Zauner-Wieczorek M, Zust F, Baltensperger U, Curtius J, Flagan RC, Hansel A, Möhler O, Petäjä T, Volkamer R, Kulmala M, Lehtipalo K, Rissanen M, Kirkby J, El-Haddad I, Bianchi F, Sipilä M, Donahue NM, Worsnop DR. High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures. Environ Sci Technol 2022; 56:13931-13944. [PMID: 36137236 PMCID: PMC9535848 DOI: 10.1021/acs.est.2c05154] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/16/2022] [Revised: 09/01/2022] [Accepted: 09/02/2022] [Indexed: 06/16/2023]
Abstract
Dimethyl sulfide (DMS) influences climate via cloud condensation nuclei (CCN) formation resulting from its oxidation products (mainly methanesulfonic acid, MSA, and sulfuric acid, H2SO4). Despite their importance, accurate prediction of MSA and H2SO4 from DMS oxidation remains challenging. With comprehensive experiments carried out in the Cosmics Leaving Outdoor Droplets (CLOUD) chamber at CERN, we show that decreasing the temperature from +25 to -10 °C enhances the gas-phase MSA production by an order of magnitude from OH-initiated DMS oxidation, while H2SO4 production is modestly affected. This leads to a gas-phase H2SO4-to-MSA ratio (H2SO4/MSA) smaller than one at low temperatures, consistent with field observations in polar regions. With an updated DMS oxidation mechanism, we find that methanesulfinic acid, CH3S(O)OH, MSIA, forms large amounts of MSA. Overall, our results reveal that MSA yields are a factor of 2-10 higher than those predicted by the widely used Master Chemical Mechanism (MCMv3.3.1), and the NOx effect is less significant than that of temperature. Our updated mechanism explains the high MSA production rates observed in field observations, especially at low temperatures, thus, substantiating the greater importance of MSA in the natural sulfur cycle and natural CCN formation. Our mechanism will improve the interpretation of present-day and historical gas-phase H2SO4/MSA measurements.
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Affiliation(s)
- Jiali Shen
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Wiebke Scholz
- Institute
of Ion Physics 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, 00014 Helsinki, Finland
| | - Putian Zhou
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Guillaume Marie
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Mingyi Wang
- Center
for Atmospheric Particle Studies, Carnegie
Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Ruby Marten
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Mihnea Surdu
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Birte Rörup
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Rima Baalbaki
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Antonio Amorim
- CENTRA
and Faculdade de Ciências da Universidade de Lisboa, 1749-016 Campo
Grande, Lisboa, Portugal
| | - Farnoush Ataei
- Leibniz
Institute for Tropospheric Research, Permoserstrasse 15, 04318 Leipzig, Germany
| | - David M. Bell
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Barbara Bertozzi
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76344 Karlsruhe, Germany
| | - Zoé Brasseur
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Lucía Caudillo
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Dexian Chen
- Center
for Atmospheric Particle Studies, Carnegie
Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Biwu Chu
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Lubna Dada
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Jonathan Duplissy
- Institute
for Atmospheric and Earth System Research/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 and Cooperative Institute for Research in the Environmental
Sciences, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Manuel Granzin
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Roberto Guida
- CERN, the European Organization for Nuclear Research, CH-1211 Geneva
23, Switzerland
| | - Martin Heinritzi
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Victoria Hofbauer
- Center
for Atmospheric Particle Studies, Carnegie
Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - Siddharth Iyer
- Aerosol Physics
Laboratory, Physics Unit, Faculty of Engineering
and Natural Sciences, Tampere University, 33014 Tampere, Finland
| | - Deniz Kemppainen
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Weimeng Kong
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, California 91125, United States
| | | | - Andreas Kürten
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Houssni Lamkaddam
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Chuan Ping Lee
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Brandon Lopez
- Center
for Atmospheric Particle Studies, Carnegie
Mellon University, Pittsburgh, Pennsylvania 15213, United States
| | - 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, CH-1211 Geneva
23, Switzerland
| | - Dario Massabò
- Department
of Physics, University of Genoa & INFN, 16146 Genoa, Italy
| | - Roy L. Mauldin
- Department of Chemistry, Carnegie Mellon
University, Pittsburgh, Pennsylvania 15213, United States
- Department of Atmospheric and Oceanic Sciences, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Bernhard Mentler
- Institute
of Ion Physics and Applied Physics, University
of Innsbruck, 6020 Innsbruck, Austria
| | - Tatjana Müller
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Joschka Pfeifer
- CERN, the European Organization for Nuclear Research, CH-1211 Geneva
23, Switzerland
| | - Maxim Philippov
- P.N. Lebedev Physical Institute of the Russian Academy of Sciences, 119991 Moscow, Russia
| | - Ana A. Piedehierro
- Finnish Meteorological Institute, Erik Palmenin aukio 1, 00560 Helsinki, Finland
| | - Pontus Roldin
- Division of Nuclear Physics, Lund University, 22100 Lund, Sweden
| | | | - Mario Simon
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Dominik Stolzenburg
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Yee Jun Tham
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- School of Marine Sciences, Sun Yat-sen
University, 519082 Zhuhai, China
| | - António Tomé
- Institute Infante Dom Luíz, University
of Beira Interior, 6200-001 Covilhã, Portugal
| | - Nsikanabasi Silas Umo
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76344 Karlsruhe, Germany
| | - Dongyu Wang
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Yonghong Wang
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Stefan K. Weber
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
- CERN, the European Organization for Nuclear Research, CH-1211 Geneva
23, Switzerland
| | - André Welti
- Finnish Meteorological Institute, Erik Palmenin aukio 1, 00560 Helsinki, Finland
| | | | - Yusheng Wu
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Marcel Zauner-Wieczorek
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Felix Zust
- Institute
of Ion Physics and Applied Physics, University
of Innsbruck, 6020 Innsbruck, Austria
| | - Urs Baltensperger
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Joachim Curtius
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Richard C. Flagan
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, California 91125, United States
| | - Armin Hansel
- Institute
of Ion Physics and Applied Physics, University
of Innsbruck, 6020 Innsbruck, Austria
| | - Ottmar Möhler
- Institute
of Meteorology and Climate Research, Karlsruhe
Institute of Technology, 76344 Karlsruhe, Germany
| | - Tuukka Petäjä
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Rainer Volkamer
- Department
of Chemistry and Cooperative Institute for Research in the Environmental
Sciences, University of Colorado Boulder, Boulder, Colorado 80309, United States
| | - Markku Kulmala
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, 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, School of Atmospheric Sciences, Nanjing University, 210023 Nanjing, China
- Aerosol and Haze Laboratory, Beijing Advanced Innovation
Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, 100029 Beijing, China
| | - Katrianne Lehtipalo
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Finnish Meteorological Institute, Erik Palmenin aukio 1, 00560 Helsinki, Finland
| | - Matti Rissanen
- Aerosol Physics
Laboratory, Physics Unit, Faculty of Engineering
and Natural Sciences, Tampere University, 33014 Tampere, Finland
| | - Jasper Kirkby
- Institute
for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
- CERN, the European Organization for Nuclear Research, CH-1211 Geneva
23, Switzerland
| | - Imad El-Haddad
- Laboratory
of Atmospheric Chemistry, Paul Scherrer
Institute, CH-5232 Villigen, Switzerland
| | - Federico Bianchi
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Mikko Sipilä
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - 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
| | - Douglas R. Worsnop
- Institute
for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Aerodyne Research, Inc., Billerica, Massachusetts 01821, United States
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12
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Liu J, D'Ambro EL, Lee BH, Schobesberger S, Bell DM, Zaveri RA, Zelenyuk A, Thornton JA, Shilling JE. Monoterpene Photooxidation in a Continuous-Flow Chamber: SOA Yields and Impacts of Oxidants, NO x, and VOC Precursors. Environ Sci Technol 2022; 56:12066-12076. [PMID: 35976919 DOI: 10.1021/acs.est.2c02630] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/15/2023]
Abstract
Monoterpene photooxidation plays an important role in secondary organic aerosol (SOA) formation in the atmosphere. The low-volatility products can enhance new particle formation and particle growth and thus influence climate feedback. Here, we present the results of α-pinene and Δ-3-carene photooxidation experiments conducted in continuous-flow mode in an environmental chamber under several reaction conditions. The roles of oxidants, addition of NO, and VOC molecular structure in influencing SOA yield are illustrated. SOA yield from α-pinene photooxidation shows a weak dependence on H2O2 concentration, which is a proxy for HO2 concentration. The high O/C ratios observed in the α-pinene photooxidation products suggest the production of highly oxygenated organic molecules (HOM). Addition of ozone to the chamber during low-NOx photooxidation experiments leads to higher SOA yield. With the addition of NO, the production of N-containing HOMs is enhanced and the SOA yield shows a modest, nonlinear dependence on the input NO concentration. Carene photooxidation leads to higher SOA yield than α-pinene under similar reaction conditions, which agrees with the lower volatility retrieved from evaporation kinetics experiments. These results improve the understanding of SOA formation from monoterpene photooxidation and could be applied to refine the representation of biogenic SOA formation in models.
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Affiliation(s)
- Jiumeng Liu
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
- School of Environment, Harbin Institute of Technology, Harbin, Heilongjiang 150001, China
| | - Emma L D'Ambro
- Department of Chemistry, University of Washington, Seattle, Washington 98195, United States
- Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - Ben Hwan Lee
- Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - Siegfried Schobesberger
- Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - David M Bell
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Rahul A Zaveri
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Alla Zelenyuk
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Joel A Thornton
- Department of Chemistry, University of Washington, Seattle, Washington 98195, United States
| | - John E Shilling
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
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13
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Reilly MJ, Zuspan A, Halofsky JS, Raymond C, McEvoy A, Dye AW, Donato DC, Kim JB, Potter BE, Walker N, Davis RJ, Dunn CJ, Bell DM, Gregory MJ, Johnston JD, Harvey BJ, Halofsky JE, Kerns BK. Cascadia Burning: The historic, but not historically unprecedented, 2020 wildfires in the Pacific Northwest,
USA. Ecosphere 2022. [DOI: 10.1002/ecs2.4070] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022] Open
Affiliation(s)
- Matthew J. Reilly
- USDA Forest Service, Pacific Northwest Research Station Western Wildland Environmental Threat Assessment Center Corvallis Oregon USA
| | - Aaron Zuspan
- USDA Forest Service, Pacific Northwest Research Station Western Wildland Environmental Threat Assessment Center, ORISE Fellow Corvallis Oregon USA
| | - Joshua S. Halofsky
- Washington State Department of Natural Resources Olympia Washington USA
- School of Environmental and Forest Sciences University of Washington Seattle Washington USA
| | - Crystal Raymond
- School of Environmental and Forest Sciences University of Washington Seattle Washington USA
| | - Andy McEvoy
- USDA Forest Service Pacific Northwest Research Station, ORISE Fellow Corvallis Oregon USA
| | - Alex W. Dye
- College of Forestry Oregon State University Corvallis Oregon USA
| | - Daniel C. Donato
- Washington State Department of Natural Resources Olympia Washington USA
- School of Environmental and Forest Sciences University of Washington Seattle Washington USA
| | - John B. Kim
- USDA Forest Service, Pacific Northwest Research Station Western Wildland Environmental Threat Assessment Center Corvallis Oregon USA
| | - Brian E. Potter
- USDA Forest Service Pacific Northwest Research Station Seattle Washington USA
| | - Nathan Walker
- USDA Forest Service Office of Sustainability and Climate Portland Oregon USA
| | - Raymond J. Davis
- USDA Forest Service Pacific Northwest Region Corvallis Oregon USA
| | | | - David M. Bell
- USDA Forest Service Pacific Northwest Research Station Corvallis Oregon USA
| | | | | | - Brian J. Harvey
- School of Environmental and Forest Sciences University of Washington Seattle Washington USA
| | - Jessica E. Halofsky
- USDA Forest Service Pacific Northwest Research Station, Western Wildland Environmental Threat Assessment Center Olympia Washington USA
| | - Becky K. Kerns
- USDA Forest Service Pacific Northwest Research Station Corvallis Oregon USA
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14
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LaManna JA, Jones FA, Bell DM, Pabst RJ, Shaw DC. Tree species diversity increases with conspecific negative density dependence across an elevation gradient. Ecol Lett 2022; 25:1237-1249. [PMID: 35291051 DOI: 10.1111/ele.13996] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/07/2021] [Revised: 01/24/2022] [Accepted: 02/13/2022] [Indexed: 11/30/2022]
Abstract
Elevational and latitudinal gradients in species diversity may be mediated by biotic interactions that cause density-dependent effects of conspecifics on survival or growth to differ from effects of heterospecifics (i.e. conspecific density dependence), but limited evidence exists to support this. We tested the hypothesis that conspecific density dependence varies with elevation using over 40 years of data on tree survival and growth from 23 old-growth temperate forest stands across a 1,000-m elevation gradient. We found that conspecific-density-dependent effects on survival of small-to-intermediate-sized focal trees were negative in lower elevation, higher diversity forest stands typically characterised by warmer temperatures and greater relative humidity. Conspecific-density-dependent effects on survival were less negative in higher elevation stands and ridges than in lower elevation stands and valley bottoms for small-to-intermediate-sized trees, but were neutral for larger trees across elevations. Conspecific-density-dependent effects on growth were negative across all tree size classes and elevations. These findings reveal fundamental differences in biotic interactions that may contribute to relationships between species diversity, elevation and climate.
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Affiliation(s)
- Joseph A LaManna
- Department of Biological Sciences, Marquette University, Milwaukee, Wisconsin, USA
| | - F Andrew Jones
- Department of Botany & Plant Pathology, Oregon State University, Corvallis, Oregon, USA.,Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama
| | - David M Bell
- Pacific Northwest Research Station, USDA Forest Service, Corvallis, Oregon, USA
| | - Robert J Pabst
- Department of Forest Ecosystems & Society, Oregon State University, Corvallis, Oregon, USA
| | - David C Shaw
- Department of Forest Engineering, Resources, and Management, Oregon State University, Corvallis, Oregon, USA
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15
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D’Ambro EL, Hyttinen N, Møller KH, Iyer S, Otkjær RV, Bell DM, Liu J, Lopez-Hilfiker FD, Schobesberger S, Shilling JE, Zelenyuk A, Kjaergaard HG, Thornton JA, Kurtén T. Pathways to Highly Oxidized Products in the Δ3-Carene + OH System. Environ Sci Technol 2022; 56:2213-2224. [PMID: 35119266 PMCID: PMC8956127 DOI: 10.1021/acs.est.1c06949] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/08/2023]
Abstract
Oxidation of the monoterpene Δ3-carene (C10H16) is a potentially important and understudied source of atmospheric secondary organic aerosol (SOA). We present chamber-based measurements of speciated gas and particle phases during photochemical oxidation of Δ3-carene. We find evidence of highly oxidized organic molecules (HOMs) in the gas phase and relatively low-volatility SOA dominated by C7-C10 species. We then use computational methods to develop the first stages of a Δ3-carene photochemical oxidation mechanism and explain some of our measured compositions. We find that alkoxy bond scission of the cyclohexyl ring likely leads to efficient HOM formation, in line with previous studies. We also find a surprising role for the abstraction of primary hydrogens from methyl groups, which has been calculated to be rapid in the α-pinene system, and suggest more research is required to determine if this is more general to other systems and a feature of autoxidation. This work develops a more comprehensive view of Δ3-carene photochemical oxidation products via measurements and lays out a suggested mechanism of oxidation via computationally derived rate coefficients.
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Affiliation(s)
- Emma L. D’Ambro
- Department
of Chemistry, University of Washington, Seattle, Washington 98195, United States
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
| | - Noora Hyttinen
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
- Institute
for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki FI-00014, Finland
| | - Kristian H. Møller
- Department
of Chemistry, University of Copenhagen, Copenhagen DK-2100, Denmark
| | - Siddharth Iyer
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
- Institute
for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki FI-00014, Finland
| | - Rasmus V. Otkjær
- Department
of Chemistry, University of Copenhagen, Copenhagen DK-2100, Denmark
| | - David M. Bell
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | - Jiumeng Liu
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | - Felipe D. Lopez-Hilfiker
- Department
of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - Siegfried Schobesberger
- Department
of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - John E. Shilling
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | - Alla Zelenyuk
- Atmospheric
Sciences and Global Change Division, Pacific
Northwest National Laboratory, Richland, Washington 99354, United States
| | | | - Joel A. Thornton
- Department
of Chemistry, University of Washington, Seattle, Washington 98195, United States
- Department
of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States
| | - Theo Kurtén
- Department
of Chemistry, University of Helsinki, Helsinki FI-00014, Finland
- Institute
for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki FI-00014, Finland
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16
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Marten R, Xiao M, Rörup B, Wang M, Kong W, He XC, Stolzenburg D, Pfeifer J, Marie G, Wang DS, Scholz W, Baccarini A, Lee CP, Amorim A, Baalbaki R, Bell DM, Bertozzi B, Caudillo L, Chu B, Dada L, Duplissy J, Finkenzeller H, Carracedo LG, Granzin M, Hansel A, Heinritzi M, Hofbauer V, Kemppainen D, Kürten A, Lampimäki M, Lehtipalo K, Makhmutov V, Manninen HE, Mentler B, Petäjä T, Philippov M, Shen J, Simon M, Stozhkov Y, Tomé A, Wagner AC, Wang Y, Weber SK, Wu Y, Zauner-Wieczorek M, Curtius J, Kulmala M, Möhler O, Volkamer R, Winkler PM, Worsnop DR, Dommen J, Flagan RC, Kirkby J, Donahue NM, Lamkaddam H, Baltensperger U, El Haddad I. Survival of newly formed particles in haze conditions. Environ Sci : Atmos 2022; 2:491-499. [PMID: 35694134 PMCID: PMC9119030 DOI: 10.1039/d2ea00007e] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/23/2022] [Accepted: 03/24/2022] [Indexed: 11/21/2022]
Abstract
Intense new particle formation events are regularly observed under highly polluted conditions, despite the high loss rates of nucleated clusters. Higher than expected cluster survival probability implies either ineffective scavenging by pre-existing particles or missing growth mechanisms. Here we present experiments performed in the CLOUD chamber at CERN showing particle formation from a mixture of anthropogenic vapours, under condensation sinks typical of haze conditions, up to 0.1 s−1. We find that new particle formation rates substantially decrease at higher concentrations of pre-existing particles, demonstrating experimentally for the first time that molecular clusters are efficiently scavenged by larger sized particles. Additionally, we demonstrate that in the presence of supersaturated gas-phase nitric acid (HNO3) and ammonia (NH3), freshly nucleated particles can grow extremely rapidly, maintaining a high particle number concentration, even in the presence of a high condensation sink. Such high growth rates may explain the high survival probability of freshly formed particles under haze conditions. We identify under what typical urban conditions HNO3 and NH3 can be expected to contribute to particle survival during haze. Illustration of how ammonium nitrate formation can cause rapid growth of nucleating particles, increasing survival of particles in polluted conditions.![]()
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Affiliation(s)
- Ruby Marten
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Mao Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Birte Rörup
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Mingyi Wang
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 15213 Pittsburgh, PA, USA
| | - Weimeng Kong
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41, Pasadena, CA 91125, USA
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Dominik Stolzenburg
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Joschka Pfeifer
- CERN, CH-1211 Geneva, Switzerland
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Guillaume Marie
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Dongyu S. Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Wiebke Scholz
- Institute of Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
| | - Andrea Baccarini
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Extreme Environments Research Laboratory (EERL), École Polytechnique Fédérale de Lausanne, Sion, CH, Switzerland
| | - Chuan Ping Lee
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Antonio Amorim
- CENTRA, FCUL, University of Lisbon, 1749-016 Lisbon, Portugal
| | - Rima Baalbaki
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - David M. Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Barbara Bertozzi
- Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, 76021 Karlsruhe, Germany
| | - Lucía Caudillo
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Biwu Chu
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Lubna Dada
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Jonathan Duplissy
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41, Pasadena, CA 91125, USA
- Helsinki Institute of Physics (HIP)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Henning Finkenzeller
- Department of Chemistry, CIRES, University of Colorado Boulder, 215 UCB, Boulder, 80309, CO, USA
| | | | - Manuel Granzin
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Armin Hansel
- Institute of Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
| | - Martin Heinritzi
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Victoria Hofbauer
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 15213 Pittsburgh, PA, USA
| | - Deniz Kemppainen
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Andreas Kürten
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Markus Lampimäki
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
- Finnish Meteorological Institute, Helsinki, Finland
| | - Vladimir Makhmutov
- Lebedev Physical Institute of the Russian Academy of Sciences, Leninsky Prospekt, 53, Moscow, 119991, Russian Federation
| | | | - Bernhard Mentler
- Institute of Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
| | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Maxim Philippov
- Lebedev Physical Institute of the Russian Academy of Sciences, Leninsky Prospekt, 53, Moscow, 119991, Russian Federation
| | - Jiali Shen
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Mario Simon
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Yuri Stozhkov
- Lebedev Physical Institute of the Russian Academy of Sciences, Leninsky Prospekt, 53, Moscow, 119991, Russian Federation
| | - António Tomé
- IDL-Universidade da Beira Interior, 6201-001 Covilhã, Portugal
| | - Andrea C. Wagner
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Yonghong Wang
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | | | - Yusheng Wu
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Marcel Zauner-Wieczorek
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Joachim Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland
| | - Ottmar Möhler
- Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, 76021 Karlsruhe, Germany
| | - Rainer Volkamer
- Department of Chemistry, CIRES, University of Colorado Boulder, 215 UCB, Boulder, 80309, CO, USA
| | - Paul M. Winkler
- Faculty of Physics, University of Vienna, Boltzmanngasse 5, A-1090 Vienna, Austria
| | | | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Richard C. Flagan
- California Institute of Technology, Division of Chemistry and Chemical Engineering 210-41, Pasadena, CA 91125, USA
| | - Jasper Kirkby
- CERN, CH-1211 Geneva, Switzerland
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
| | - Neil M. Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, 15213 Pittsburgh, PA, USA
| | - Houssni Lamkaddam
- 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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17
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Bradford JB, Shriver RK, Robles MD, McCauley LA, Woolley TJ, Andrews CA, Crimmins M, Bell DM. Tree mortality response to drought‐density interactions suggests opportunities to enhance drought resistance. J Appl Ecol 2021. [DOI: 10.1111/1365-2664.14073] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/26/2023]
Affiliation(s)
- John. B. Bradford
- Southwest Biological Science Center U.S. Geological Survey Flagstaff AZ USA
| | - Robert K. Shriver
- Department of Natural Resources and Environmental Science University of Nevada Reno NV USA
| | - Marcos D. Robles
- Center for Science and Public Policy The Nature Conservancy Tucson AZ USA
| | - Lisa A. McCauley
- Center for Science and Public Policy The Nature Conservancy Tucson AZ USA
| | - Travis J. Woolley
- Center for Science and Public Policy The Nature Conservancy Tucson AZ USA
| | - Caitlin A. Andrews
- Southwest Biological Science Center U.S. Geological Survey Flagstaff AZ USA
| | - Michael Crimmins
- Department of Environmental Science University of Arizona Tucson AZ USA
| | - David M. Bell
- Pacific Northwest Research Station USDA Forest Service Corvallis OR USA
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18
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Yu R, Pan F, Schreine C, Wang X, Bell DM, Qiu G, Wang J. Quantitative Determination of Airborne Redox-Active Compounds Based on Heating-Induced Reduction of Gold Nanoparticles. Anal Chem 2021; 93:14859-14868. [PMID: 34705434 DOI: 10.1021/acs.analchem.1c03823] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Abstract
Airborne redox-active compounds (ARC) account for a substantial fraction of atmospheric aerosols and play a vital role in chemical processes that influence global climate and human and ecological health. With the exception of the determination of total organic carbon by the expensive total organic carbon (TOC) analyzer, there is currently no easy-to-use method to quantify ARC. Here, we designed a method to detect the concentration of ARC by using the thermal-induced reduction and colorimetric behaviors of gold nanoparticles (AuNPs), in which the humic substances (HS) was used as a standard model of ARC to calculate the HS-equivalent concentration of ARC. Distinguished from the conventional complex methods, e.g., TOC analysis, the proposed approach measured localized surface plasmon resonance absorption of AuNPs and the target ARC concentration can be either directly quantified by the absorption spectrometer or qualitatively evaluated by the naked eyes. By using the absorption spectrometer, a limit of detection of 0.005 ppm by our AuNP sensor was achieved. To validate this sensing technique, aerosol samples collected from Basel (suburban), Bern (urban), and Rigi mountain (rural and high-altitude) sites in Switzerland were further investigated through the TOC combustion method. The results thereby substantiated that our plasmonic absorption-based AuNP sensor upholds a great promise for fast, cost-efficient total ARC detection and air quality assessment.
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Affiliation(s)
- Ranxue Yu
- Key Laboratory of Textile Science and Technology of Ministry of Education, College of Textiles, Donghua University, Shanghai 201620, China.,Institute of Environmental Engineering, ETH Zurich, 8093 Zurich, Switzerland.,Advanced Analytical Technologies, Empa, Ueberlandstrasse 129, 8600 Dübendorf, Switzerland
| | - Fei Pan
- Laboratory for Biointerfaces, Empa, 9014 St. Gallen, Switzerland
| | - Claudia Schreine
- Advanced Analytical Technologies, Empa, Ueberlandstrasse 129, 8600 Dübendorf, Switzerland
| | - Xinhou Wang
- Key Laboratory of Textile Science and Technology of Ministry of Education, College of Textiles, Donghua University, Shanghai 201620, China
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Guangyu Qiu
- Institute of Environmental Engineering, ETH Zurich, 8093 Zurich, Switzerland.,Advanced Analytical Technologies, Empa, Ueberlandstrasse 129, 8600 Dübendorf, Switzerland
| | - Jing Wang
- Institute of Environmental Engineering, ETH Zurich, 8093 Zurich, Switzerland.,Advanced Analytical Technologies, Empa, Ueberlandstrasse 129, 8600 Dübendorf, Switzerland
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19
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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] [What about the content of this article? (0)] [Affiliation(s)] [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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20
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Shriver RK, Yackulic CB, Bell DM, Bradford JB. Quantifying the demographic vulnerabilities of dry woodlands to climate and competition using rangewide monitoring data. Ecology 2021; 102:e03425. [PMID: 34091890 DOI: 10.1002/ecy.3425] [Citation(s) in RCA: 9] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Submit a Manuscript] [Subscribe] [Scholar Register] [Received: 12/11/2020] [Revised: 02/08/2021] [Accepted: 03/21/2021] [Indexed: 01/25/2023]
Abstract
Climate change is expected to alter the distribution and abundance of tree species, impacting ecosystem structure and function. Yet, anticipating where this will occur is often hampered by a lack of understanding of how demographic rates, most notably recruitment, vary in response to climate and competition across a species range. Using large-scale monitoring data on two dry woodland tree species (Pinus edulis and Juniperus osteosperma), we develop an approach to infer recruitment, survival, and growth of both species across their range. In doing so, we account for ecological and statistical dependencies inherent in large-scale monitoring data. We find that drying and warming conditions generally lead to declines in recruitment and survival, but the strength of responses varied between species. These climate conditions point to geographic regions of high vulnerability for particular species, such as Pinus edulis in northern Arizona, where both survival and recruitment are low. Our approach provides a path forward for leveraging emerging large-scale monitoring and remotely sensed data to anticipate the impacts of global change on species distributions.
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Affiliation(s)
- Robert K Shriver
- Department of Natural Resources and Environmental Science, University of Nevada, Reno, Nevada, 89557, USA.,U.S. Geological Survey, Southwest Biological Science Center, Flagstaff, Arizona, 86001, USA
| | - Charles B Yackulic
- U.S. Geological Survey, Southwest Biological Science Center, Flagstaff, Arizona, 86001, USA
| | - David M Bell
- U.S. Department of Agriculture Forest Service, Pacific Northwest Research Station, Corvallis, Oregon, 97331, USA
| | - John B Bradford
- U.S. Geological Survey, Southwest Biological Science Center, Flagstaff, Arizona, 86001, USA
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21
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Pospisilova V, Bell DM, Lamkaddam H, Bertrand A, Wang L, Bhattu D, Zhou X, Dommen J, Prevot ASH, Baltensperger U, El Haddad I, Slowik JG. Photodegradation of α-Pinene Secondary Organic Aerosol Dominated by Moderately Oxidized Molecules. Environ Sci Technol 2021; 55:6936-6943. [PMID: 33961408 DOI: 10.1021/acs.est.0c06752] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
Atmospheric secondary organic aerosol (SOA) undergoes chemical and physical changes when exposed to UV radiation, affecting the atmospheric lifetime of the involved molecules. However, these photolytic processes remain poorly constrained. Here, we present a study aimed at characterizing, at a molecular level and in real time, the chemical composition of α-pinene SOA exposed to UV-A light at 50% relative humidity in an atmospheric simulation chamber. Significant SOA mass loss is observed at high loadings (∼100 μg m-3), whereas the effect is less prevalent at lower loadings (∼20 μg m-3). For the vast majority of molecules measured by the extractive electrospray time-of-flight mass spectrometer, there is a fraction that is photoactive and decays when exposed to UV-A radiation and a fraction that appears photorecalcitrant. The molecules that are most photoactive contain between 4 and 6 oxygen atoms, while the more highly oxygenated compounds and dimers do not exhibit significant decay. Overall, photolysis results in a reduction of the volatility of SOA, which cannot be explained by simple evaporative losses but requires either a change in volatility related to changes in functional groups or a change in physical parameters (i.e., viscosity).
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Affiliation(s)
- Veronika Pospisilova
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Tofwerk, 3600 Thun, Switzerland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Houssni Lamkaddam
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Amelie Bertrand
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Liwei Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Deepika Bhattu
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
- Department of Civil and Infrastructure Engineering, Indian Institute of Technology Jodhpur, Karwar 342037, India
| | - Xueqin Zhou
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Andre S H Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Imad El Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
| | - Jay G Slowik
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
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22
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Wang M, Kong W, Marten R, He XC, Chen D, Pfeifer J, Heitto A, Kontkanen J, Dada L, Kürten A, Yli-Juuti T, Manninen HE, Amanatidis S, Amorim A, Baalbaki R, Baccarini A, Bell DM, Bertozzi B, Bräkling S, Brilke S, Murillo LC, Chiu R, Chu B, De Menezes LP, Duplissy J, Finkenzeller H, Carracedo LG, Granzin M, Guida R, Hansel A, Hofbauer V, Krechmer J, Lehtipalo K, Lamkaddam H, Lampimäki M, Lee CP, Makhmutov V, Marie G, Mathot S, Mauldin RL, Mentler B, Müller T, Onnela A, Partoll E, Petäjä T, Philippov M, Pospisilova V, Ranjithkumar A, Rissanen M, Rörup B, Scholz W, Shen J, Simon M, Sipilä M, Steiner G, Stolzenburg D, Tham YJ, Tomé A, Wagner AC, Wang DS, Wang Y, Weber SK, Winkler PM, Wlasits PJ, Wu Y, Xiao M, Ye Q, Zauner-Wieczorek M, Zhou X, Volkamer R, Riipinen I, Dommen J, Curtius J, Baltensperger U, Kulmala M, Worsnop DR, Kirkby J, Seinfeld JH, El-Haddad I, Flagan RC, Donahue NM. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation. Nature 2020; 581:184-189. [PMID: 32405020 PMCID: PMC7334196 DOI: 10.1038/s41586-020-2270-4] [Citation(s) in RCA: 72] [Impact Index Per Article: 18.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/26/2019] [Accepted: 03/17/2020] [Indexed: 11/08/2022]
Abstract
A list of authors and their affiliations appears at the end of the paper New-particle formation is a major contributor to urban smog1,2, but how it occurs in cities is often puzzling3. If the growth rates of urban particles are similar to those found in cleaner environments (1-10 nanometres per hour), then existing understanding suggests that new urban particles should be rapidly scavenged by the high concentration of pre-existing particles. Here we show, through experiments performed under atmospheric conditions in the CLOUD chamber at CERN, that below about +5 degrees Celsius, nitric acid and ammonia vapours can condense onto freshly nucleated particles as small as a few nanometres in diameter. Moreover, when it is cold enough (below -15 degrees Celsius), nitric acid and ammonia can nucleate directly through an acid-base stabilization mechanism to form ammonium nitrate particles. Given that these vapours are often one thousand times more abundant than sulfuric acid, the resulting particle growth rates can be extremely high, reaching well above 100 nanometres per hour. However, these high growth rates require the gas-particle ammonium nitrate system to be out of equilibrium in order to sustain gas-phase supersaturations. In view of the strong temperature dependence that we measure for the gas-phase supersaturations, we expect such transient conditions to occur in inhomogeneous urban settings, especially in wintertime, driven by vertical mixing and by strong local sources such as traffic. Even though rapid growth from nitric acid and ammonia condensation may last for only a few minutes, it is nonetheless fast enough to shepherd freshly nucleated particles through the smallest size range where they are most vulnerable to scavenging loss, thus greatly increasing their survival probability. We also expect nitric acid and ammonia nucleation and rapid growth to be important in the relatively clean and cold upper free troposphere, where ammonia can be convected from the continental boundary layer and nitric acid is abundant from electrical storms4,5.
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Affiliation(s)
- Mingyi Wang
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, PA, USA
| | - Weimeng Kong
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - Ruby Marten
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Xu-Cheng He
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Dexian Chen
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USA
| | - Joschka Pfeifer
- CERN, the European Organization for Nuclear Research, Geneva, Switzerland
| | - Arto Heitto
- Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
| | - Jenni Kontkanen
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Lubna Dada
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Andreas Kürten
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Taina Yli-Juuti
- Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
| | - Hanna E Manninen
- CERN, the European Organization for Nuclear Research, Geneva, Switzerland
| | - Stavros Amanatidis
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - António Amorim
- CENTRA and Faculdade de Ciências da Universidade de Lisboa, Campo Grande, Lisbon, Portugal
| | - Rima Baalbaki
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Andrea Baccarini
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - David M Bell
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Barbara Bertozzi
- Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
| | | | - Sophia Brilke
- Faculty of Physics, University of Vienna, Vienna, Austria
| | - Lucía Caudillo Murillo
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Randall Chiu
- Department of Chemistry and CIRES, University of Colorado at Boulder, Boulder, CO, USA
| | - Biwu Chu
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | | | - Jonathan Duplissy
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
- Helsinki Institute of Physics, University of Helsinki, Helsinki, Finland
| | - Henning Finkenzeller
- Department of Chemistry and CIRES, University of Colorado at Boulder, Boulder, CO, USA
| | | | - Manuel Granzin
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Roberto Guida
- CERN, the European Organization for Nuclear Research, Geneva, Switzerland
| | - Armin Hansel
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
- Ionicon Analytik, Innsbruck, Austria
| | - Victoria Hofbauer
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, PA, USA
| | | | - Katrianne Lehtipalo
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
- Finnish Meteorological Institute, Helsinki, Finland
| | - Houssni Lamkaddam
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Markus Lampimäki
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Chuan Ping Lee
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Vladimir Makhmutov
- P.N. Lebedev Physical Institute of the Russian Academy of Sciences, Moscow, Russia
| | - Guillaume Marie
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Serge Mathot
- CERN, the European Organization for Nuclear Research, Geneva, Switzerland
| | - Roy L Mauldin
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, PA, USA
- Department of Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, CO, USA
| | - Bernhard Mentler
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
| | - Tatjana Müller
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Antti Onnela
- CERN, the European Organization for Nuclear Research, Geneva, Switzerland
| | - Eva Partoll
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
| | - Tuukka Petäjä
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Maxim Philippov
- P.N. Lebedev Physical Institute of the Russian Academy of Sciences, Moscow, Russia
| | - Veronika Pospisilova
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | | | - Matti Rissanen
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
- Aerosol Physics Laboratory, Physics Unit, Faculty of Engineering and Natural Sciences, Tampere University, Tampere, Finland
| | - Birte Rörup
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Wiebke Scholz
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
- Ionicon Analytik, Innsbruck, Austria
| | - Jiali Shen
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Mario Simon
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Mikko Sipilä
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Gerhard Steiner
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
- Grimm Aerosol Technik Ainring, Ainring, Germany
| | - Dominik Stolzenburg
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
- Faculty of Physics, University of Vienna, Vienna, Austria
| | - Yee Jun Tham
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - António Tomé
- Institute Infante Dom Luíz, University of Beira Interior, Covilhã, Portugal
| | - Andrea C Wagner
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
- Department of Chemistry and CIRES, University of Colorado at Boulder, Boulder, CO, USA
| | - Dongyu S Wang
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Yonghong Wang
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Stefan K Weber
- CERN, the European Organization for Nuclear Research, Geneva, Switzerland
| | - Paul M Winkler
- Faculty of Physics, University of Vienna, Vienna, Austria
| | | | - Yusheng Wu
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - Mao Xiao
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Qing Ye
- Center for Atmospheric Particle Studies, 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
| | - Marcel Zauner-Wieczorek
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Xueqin Zhou
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Rainer Volkamer
- Department of Chemistry and CIRES, University of Colorado at Boulder, Boulder, CO, USA
| | - Ilona Riipinen
- Department of Applied Environmental Science, University of Stockholm, Stockholm, Sweden
| | - Josef Dommen
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Joachim Curtius
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - Urs Baltensperger
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Markku Kulmala
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
- Helsinki Institute of Physics, University of Helsinki, Helsinki, Finland
- Joint International Research Laboratory of Atmospheric and Earth System Sciences, Nanjing University, Nanjing, China
- Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, China
| | - Douglas R Worsnop
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
- Aerodyne Research, Billerica, MA, USA
| | - Jasper Kirkby
- CERN, the European Organization for Nuclear Research, Geneva, Switzerland
- Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - John H Seinfeld
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - Imad El-Haddad
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
| | - Richard C Flagan
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
| | - Neil M Donahue
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA.
- Department of Chemistry, Carnegie Mellon University, Pittsburgh, PA, USA.
- Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USA.
- Department of Engineering and Public Policy, Carnegie Mellon University, Pittsburgh, PA, USA.
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23
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Zaveri RA, Shilling JE, Zelenyuk A, Zawadowicz MA, Suski K, China S, Bell DM, Veghte D, Laskin A. Particle-Phase Diffusion Modulates Partitioning of Semivolatile Organic Compounds to Aged Secondary Organic Aerosol. Environ Sci Technol 2020; 54:2595-2605. [PMID: 31994876 DOI: 10.1021/acs.est.9b05514] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/10/2023]
Abstract
The diffusivity of semivolatile organic compounds (SVOCs) in the bulk particle phase of a viscous atmospheric secondary organic aerosol (SOA) can have a profound impact on aerosol growth and size distribution dynamics. Here, we investigate the bulk diffusivity of SVOCs formed from photo-oxidation of isoprene as they partition to a bimodal aerosol consisting of an Aitken (potassium sulfate) and accumulation mode (aged α-pinene SOA) particles as a function of relative humidity (RH). The model analysis of the observed size distribution evolution shows that liquid-like diffusion coefficient values of Db > 10-10 cm2 s-1 fail to explain the growth of the Aitken mode. Instead, much lower values of Db between 2.5 × 10-15 cm2 s-1 at 32% RH and 8 × 10-15 cm2 s-1 at 82% RH were needed to successfully reproduce the growth of both modes. The diffusivity within the aged α-pinene SOA remains appreciably slow even at 80% RH, resulting in hindered partitioning of SVOCs to large viscous particles and allowing smaller and relatively less viscous particles to effectively absorb the available SVOCs and grow much faster than would be possible otherwise. These results have important implications for modeling SOA formation and growth in the ambient atmosphere.
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Affiliation(s)
- Rahul A Zaveri
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - John E Shilling
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Alla Zelenyuk
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Maria A Zawadowicz
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Kaitlyn Suski
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Swarup China
- William R. Wiley Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - David M Bell
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Daniel Veghte
- William R. Wiley Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Alexander Laskin
- Department of Chemistry, Purdue University, West Lafayette, Indiana 47907, United States
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24
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Bell DM, Pabst RJ, Shaw DC. Tree growth declines and mortality were associated with a parasitic plant during warm and dry climatic conditions in a temperate coniferous forest ecosystem. Glob Chang Biol 2020; 26:1714-1724. [PMID: 31507026 DOI: 10.1111/gcb.14834] [Citation(s) in RCA: 9] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/12/2019] [Revised: 07/23/2019] [Accepted: 08/13/2019] [Indexed: 05/25/2023]
Abstract
Insects and pathogens are widely recognized as contributing to increased tree vulnerability to the projected future increasing frequency of hot and dry conditions, but the role of parasitic plants is poorly understood even though they are common throughout temperate coniferous forests in the western United States. We investigated the influence of western hemlock dwarf mistletoe (Arceuthobium tsugense) on large (≥45.7 cm diameter) western hemlock (Tsuga heterophylla) growth and mortality in a 500 year old coniferous forest at the Wind River Experimental Forest, Washington State, United States. We used five repeated measurements from a long-term tree record for 1,395 T. heterophylla individuals. Data were collected across a time gradient (1991-2014) capturing temperature increases and precipitation decreases. The dwarf mistletoe rating (DMR), a measure of infection intensity, varied among individuals. Our results indicated that warmer and drier conditions amplified dwarf mistletoe effects on T. heterophylla tree growth and mortality. We found that heavy infection (i.e., high DMR) resulted in reduced growth during all four measurement intervals, but during warm and dry intervals (a) growth declined across the entire population regardless of DMR level, and (b) both moderate and heavy infections resulted in greater growth declines compared to light infection levels. Mortality rates increased from cooler-wetter to warmer-drier measurement intervals, in part reflecting increasing mortality with decreasing tree growth. Mortality rates were positively related to DMR, but only during the warm and dry measurement intervals. These results imply that parasitic plants like dwarf mistletoe can amplify the impact of climatic stressors of trees, contributing to the vulnerability of forest landscapes to climate-induced productivity losses and mortality events.
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Affiliation(s)
- David M Bell
- Pacific Northwest Research Station, USDA Forest Service, Corvallis, OR, USA
| | - Robert J Pabst
- Department of Forest Ecosystems and Society, Oregon State University, Corvallis, OR, USA
| | - David C Shaw
- Department of Forest Engineering, Resources & Management, Oregon State University, Corvallis, OR, USA
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25
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Gaiser EE, Bell DM, Castorani MCN, Childers DL, Groffman PM, Jackson CR, Kominoski JS, Peters DPC, Pickett STA, Ripplinger J, Zinnert JC. Long-Term Ecological Research and Evolving Frameworks of Disturbance Ecology. Bioscience 2020. [DOI: 10.1093/biosci/biz162] [Citation(s) in RCA: 27] [Impact Index Per Article: 6.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/31/2022] Open
Abstract
AbstractDetecting and understanding disturbance is a challenge in ecology that has grown more critical with global environmental change and the emergence of research on social–ecological systems. We identify three areas of research need: developing a flexible framework that incorporates feedback loops between social and ecological systems, anticipating whether a disturbance will change vulnerability to other environmental drivers, and incorporating changes in system sensitivity to disturbance in the face of global changes in environmental drivers. In the present article, we review how discoveries from the US Long Term Ecological Research (LTER) Network have influenced theoretical paradigms in disturbance ecology, and we refine a framework for describing social–ecological disturbance that addresses these three challenges. By operationalizing this framework for seven LTER sites spanning distinct biomes, we show how disturbance can maintain or alter ecosystem state, drive spatial patterns at landscape scales, influence social–ecological interactions, and cause divergent outcomes depending on other environmental changes.
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Affiliation(s)
- Evelyn E Gaiser
- Department of Biological Sciences, Institute of Environment, Florida International University, Miami, Florida
| | - David M Bell
- Pacific Northwest Research Station, under the US Department of Agriculture Forest Service, Corvallis, Oregon
| | - Max C N Castorani
- Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia
| | | | - Peter M Groffman
- City University of New York's Advanced Science Research Center, Graduate Center, New York, New York, and with the Cary Institute of Ecosystem Studies, Millbrook, New York
| | - C Rhett Jackson
- Warnell School of Forestry and Natural Resources, University of Georgia, Athens, Georgia
| | - John S Kominoski
- Department of Biological Sciences, Institute of Environment, Florida International University, Miami, Florida
| | - Debra P C Peters
- US Department of Agriculture Agricultural Research Service's Jornada Experimental Range and Jornada Basin LTER Program, New Mexico State University, Las Cruces, New Mexico
| | | | - Julie Ripplinger
- Department of Botany and Plant Sciences, University of California—Riverside, Riverside, California
| | - Julie C Zinnert
- Department of Biology at Virginia Commonwealth University, Richmond, Virginia
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26
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Henderson EB, Bell DM, Gregory MJ. Vegetation mapping to support greater sage‐grouse habitat monitoring and management: multi‐ or univariate approach? Ecosphere 2019. [DOI: 10.1002/ecs2.2838] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/11/2023] Open
Affiliation(s)
- Emilie B. Henderson
- Institute for Natural Resources Oregon State University Portland Oregon 97207 USA
| | - David M. Bell
- USDA Forest Service, Pacific Northwest Research Station Corvallis Oregon 97331 USA
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27
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Kramer AL, Suski KJ, Bell DM, Zelenyuk A, Massey Simonich SL. Formation of Polycyclic Aromatic Hydrocarbon Oxidation Products in α-Pinene Secondary Organic Aerosol Particles Formed through Ozonolysis. Environ Sci Technol 2019; 53:6669-6677. [PMID: 31125204 PMCID: PMC7122035 DOI: 10.1021/acs.est.9b01732] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/12/2023]
Abstract
Accurate long-range atmospheric transport (LRAT) modeling of polycyclic aromatic hydrocarbons (PAHs) and PAH oxidation products (PAH-OPs) in secondary organic aerosol (SOA) particles relies on the known chemical composition of the particles. Four PAHs, phenanthrene (PHE), dibenzothiophene (DBT), pyrene (PYR), and benz(a)anthracene (BaA), were studied individually to identify and quantify PAH-OPs produced and incorporated into SOA particles formed by ozonolysis of α-pinene in the presence of PAH vapor. SOA particles were characterized using real-time in situ instrumentation, and collected on quartz fiber filters for offline analysis of PAHs and PAH-OPs. PAH-OPs were measured in all PAH experiments at equal or greater concentrations than the individual PAHs they were produced from. The total mass of PAH and PAH-OPs, relative to the total SOA mass, varied for different experiments on individual parent PAHs: PHE and 6 quantified PHE-OPs (3.0%), DBT and dibenzothiophene sulfone (4.9%), PYR and 3 quantified PYR-OPs (3.1%), and BaA and benz(a)anthracene-7,12-dione (0.26%). Further exposure of PAH-SOA to ozone generally increased the concentration ratio of PAH-OPs to PAH, suggesting longer atmospheric lifetimes for PAH-OPs, relative to PAHs. These data indicate that PAH-OPs are formed during SOA particle formation and growth.
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Affiliation(s)
- Amber L. Kramer
- Department of Chemistry, Oregon State University, Corvallis Oregon 97331, United States
| | - Kaitlyn J. Suski
- Atmospheric Sciences and Global Change, Pacific Northwest National Laboratory, Richland Washington 99354, United States
| | - David M. Bell
- Atmospheric Sciences and Global Change, Pacific Northwest National Laboratory, Richland Washington 99354, United States
| | - Alla Zelenyuk
- Atmospheric Sciences and Global Change, Pacific Northwest National Laboratory, Richland Washington 99354, United States
| | - Staci L. Massey Simonich
- Department of Chemistry, Oregon State University, Corvallis Oregon 97331, United States
- Department of Environmental and Molecular Toxicology, Oregon State University, Corvallis Oregon 97331, United States
- Corresponding Author: Tel: (541) 737-9194. Fax: (542) 737 0497.
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28
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Affiliation(s)
- Damon B. Lesmeister
- USDA Forest Service, Pacific Northwest Research Station Corvallis Oregon 97331 USA
- Department of Fisheries and Wildlife Oregon State University Corvallis Oregon 97331 USA
| | - Stan G. Sovern
- Department of Fisheries and Wildlife Oregon State University Corvallis Oregon 97331 USA
| | - Raymond J. Davis
- USDA Forest Service, Pacific Northwest Region Corvallis Oregon 97331 USA
| | - David M. Bell
- USDA Forest Service, Pacific Northwest Research Station Corvallis Oregon 97331 USA
| | - Matthew J. Gregory
- Department of Forest Ecosystems and Society Oregon State University Corvallis Oregon 97331 USA
| | - Jody C. Vogeler
- Department of Forest Ecosystems and Society Oregon State University Corvallis Oregon 97331 USA
- Natural Resources Ecology Lab Colorado State University Fort Collins Colorado 80523 USA
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29
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Bell DM, Gregory MJ, Kane V, Kane J, Kennedy RE, Roberts HM, Yang Z. Multiscale divergence between Landsat- and lidar-based biomass mapping is related to regional variation in canopy cover and composition. Carbon Balance Manag 2018; 13:15. [PMID: 30218413 PMCID: PMC6138055 DOI: 10.1186/s13021-018-0104-6] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 05/31/2018] [Accepted: 09/07/2018] [Indexed: 06/08/2023]
Abstract
BACKGROUND Satellite-based aboveground forest biomass maps commonly form the basis of forest biomass and carbon stock mapping and monitoring, but biomass maps likely vary in performance by region and as a function of spatial scale of aggregation. Assessing such variability is not possible with spatially-sparse vegetation plot networks. In the current study, our objective was to determine whether high-resolution lidar-based and moderate-resolution Landsat-base aboveground live forest biomass maps converged on similar predictions at stand- to landscape-levels (10 s to 100 s ha) and whether such differences depended on biophysical setting. Specifically, we examined deviations between lidar- and Landsat-based biomass mapping methods across scales and ecoregions using a measure of error (normalized root mean square deviation), a measure of the unsystematic deviations, or noise (Pearson correlation coefficient), and two measures related to systematic deviations, or biases (intercept and slope of a regression between the two sets of predictions). RESULTS Compared to forest inventory data (0.81-ha aggregate-level), lidar and Landsat-based mean biomass predictions exhibited similar performance, though lidar predictions exhibited less normalized root mean square deviation than Landsat when compared with the reference plot data. Across aggregate-levels, the intercepts and slopes of regression equations describing the relationships between lidar- and Landsat-based biomass predictions stabilized (i.e., little additional change with increasing area of aggregates) at aggregate-levels between 10 and 100 ha, suggesting a consistent relationship between the two maps at landscape-scales. Differences between lidar- and Landsat-based biomass maps varied as a function of forest canopy heterogeneity and composition, with systematic deviations (regression intercepts) increasing with mean canopy cover and hardwood proportion within forests and correlations decreasing with hardwood proportion. CONCLUSIONS Deviations between lidar- and Landsat-based maps indicated that satellite-based approaches may represent general gradients in forest biomass. Ecoregion impacted deviations between lidar and Landsat biomass maps, highlighting the importance of biophysical setting in determining biomass map performance across aggregate scales. Therefore, regardless of the source of remote sensing (e.g., Landsat vs. lidar), factors affecting the measurement and prediction of forest biomass, such as species composition, need to be taken into account whether one is estimating biomass at the plot, stand, or landscape scale.
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Affiliation(s)
- David M. Bell
- Pacific Northwest Research Station, USDA Forest Service, 3200 SW Jefferson Way, Corvallis, OR 97331 USA
| | - Matthew J. Gregory
- Forest Ecosystems and Society Department, Oregon State University, Corvallis, OR USA
| | - Van Kane
- School of Environmental and Forest Sciences, University of Washington, Seattle, WA USA
| | - Jonathan Kane
- School of Environmental and Forest Sciences, University of Washington, Seattle, WA USA
| | - Robert E. Kennedy
- College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR USA
| | - Heather M. Roberts
- Forest Ecosystems and Society Department, Oregon State University, Corvallis, OR USA
| | - Zhiqiang Yang
- Forest Ecosystems and Society Department, Oregon State University, Corvallis, OR USA
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30
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Bell DM, Cohen WB, Reilly M, Yang Z. Visual interpretation and time series modeling of Landsat imagery highlight drought's role in forest canopy declines. Ecosphere 2018. [DOI: 10.1002/ecs2.2195] [Citation(s) in RCA: 14] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/24/2022] Open
Affiliation(s)
- David M. Bell
- United States Department of Agriculture, Forest Service; Pacific Northwest Research Station; Corvallis Oregon 97331 USA
| | - Warren B. Cohen
- United States Department of Agriculture, Forest Service; Pacific Northwest Research Station; Corvallis Oregon 97331 USA
| | - Matthew Reilly
- Department of Forest Ecosystems and Society; College of Forestry; Oregon State University; Corvallis Oregon 97331 USA
- Department of Biological Sciences; College of Natural Resources and Sciences; Humboldt State University; Arcata California 95521 USA
| | - Zhiqiang Yang
- Department of Forest Ecosystems and Society; College of Forestry; Oregon State University; Corvallis Oregon 97331 USA
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31
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Zaveri RA, Shilling JE, Zelenyuk A, Liu J, Bell DM, D'Ambro EL, Gaston CJ, Thornton JA, Laskin A, Lin P, Wilson J, Easter RC, Wang J, Bertram AK, Martin ST, Seinfeld JH, Worsnop DR. Growth Kinetics and Size Distribution Dynamics of Viscous Secondary Organic Aerosol. Environ Sci Technol 2018; 52:1191-1199. [PMID: 29244949 DOI: 10.1021/acs.est.7b04623] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/07/2023]
Abstract
Low bulk diffusivity inside viscous semisolid atmospheric secondary organic aerosol (SOA) can prolong equilibration time scale, but its broader impacts on aerosol growth and size distribution dynamics are poorly understood. Here, we present quantitative insights into the effects of bulk diffusivity on the growth and evaporation kinetics of SOA formed under dry conditions from photooxidation of isoprene in the presence of a bimodal aerosol consisting of Aitken (ammonium sulfate) and accumulation (isoprene or α-pinene SOA) mode particles. Aerosol composition measurements and evaporation kinetics indicate that isoprene SOA is composed of several semivolatile organic compounds (SVOCs), with some reversibly reacting to form oligomers. Model analysis shows that liquid-like bulk diffusivities can be used to fit the observed evaporation kinetics of accumulation mode particles but fail to explain the growth kinetics of bimodal aerosol by significantly under-predicting the evolution of the Aitken mode. In contrast, the semisolid scenario successfully reproduces both evaporation and growth kinetics, with the interpretation that hindered partitioning of SVOCs into large viscous particles effectively promotes the growth of smaller particles that have shorter diffusion time scales. This effect has important implications for the growth of atmospheric ultrafine particles to climatically active sizes.
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Affiliation(s)
- Rahul A Zaveri
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - John E Shilling
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - Alla Zelenyuk
- Physical Sciences Division, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - Jiumeng Liu
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - David M Bell
- Physical Sciences Division, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - Emma L D'Ambro
- Department of Atmospheric Sciences, University of Washington , Seattle, Washington 98195, United States
- Department of Chemistry, University of Washington , Seattle, Washington 98195, United States
| | - Cassandra J Gaston
- Department of Atmospheric Sciences, University of Washington , Seattle, Washington 98195, United States
| | - Joel A Thornton
- Department of Atmospheric Sciences, University of Washington , Seattle, Washington 98195, United States
- Department of Chemistry, University of Washington , Seattle, Washington 98195, United States
| | - Alexander Laskin
- William R. Wiley Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - Peng Lin
- William R. Wiley Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - Jacqueline Wilson
- Physical Sciences Division, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - Richard C Easter
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory , Richland, Washington 99352, United States
| | - Jian Wang
- Environmental and Climate Sciences Department, Brookhaven National Laboratory , Upton, New York 11973, United States
| | - Allan K Bertram
- Department of Chemistry, University of British Columbia , Vancouver, British Columbia V6T 1Z1, Canada
| | - Scot T Martin
- John A. Paulson 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
| | - John H Seinfeld
- Division of Chemistry and Chemical Engineering, California Institute of Technology , Pasadena, California 91125, United States
- Division of Engineering and Applied Science, California Institute of Technology , Pasadena, California 91125, United States
| | - Douglas R Worsnop
- Center for Aerosol and Cloud Chemistry, Aerodyne Research , Billerica, Massachusetts 01821, United States
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32
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Zelenyuk A, Imre DG, Wilson J, Bell DM, Suski KJ, Shrivastava M, Beránek J, Lizabeth Alexander M, Kramer AL, Massey Simonich SL. The effect of gas-phase polycyclic aromatic hydrocarbons on the formation and properties of biogenic secondary organic aerosol particles. Faraday Discuss 2017; 200:143-164. [PMID: 28581016 PMCID: PMC9918307 DOI: 10.1039/c7fd00032d] [Citation(s) in RCA: 25] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/13/2022]
Abstract
When secondary organic aerosol (SOA) particles are formed by ozonolysis in the presence of gas-phase polycyclic aromatic hydrocarbons (PAHs), their formation and properties are significantly different from SOA particles formed without PAHs. For all SOA precursors and all PAHs, discussed in this study, the presence of the gas-phase PAHs during SOA formation significantly affects particle mass loadings, composition, growth, evaporation kinetics, and viscosity. SOA particles formed in the presence of PAHs have, as part of their compositions, trapped unreacted PAHs and products of heterogeneous reactions between PAHs and ozone. Compared to 'pure' SOA particles, these particles exhibit slower evaporation kinetics, have higher fractions of non-volatile components, like oligomers, and higher viscosities, assuring their longer atmospheric lifetimes. In turn, the increased viscosity and decreased volatility provide a shield that protects PAHs from chemical degradation and evaporation, allowing for the long-range transport of these toxic pollutants. The magnitude of the effect of PAHs on SOA formation is surprisingly large. The presence of PAHs during SOA formation increases mass loadings by factors of two to five, and particle number concentrations, in some cases, by more than a factor of 100. Increases in SOA mass, particle number concentrations, and lifetime have important implications to many atmospheric processes related to climate, weather, visibility, and human health, all of which relate to the interactions between biogenic SOA and anthropogenic PAHs. The synergistic relationship between SOA and PAHs presented here are clearly complex and call for future research to elucidate further the underlying processes and their exact atmospheric implications.
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Affiliation(s)
| | | | | | - David M. Bell
- Pacific Northwest National Laboratory, Oregon State University
| | | | | | - Josef Beránek
- Pacific Northwest National Laboratory, Oregon State University
| | | | | | - Staci L. Massey Simonich
- Department of Chemistry, Oregon State University,Environmental and Molecular Toxicology, Oregon State University
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33
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Bell DM, Spies TA, Pabst R. Historical harvests reduce neighboring old-growth basal area across a forest landscape. Ecol Appl 2017; 27:1666-1676. [PMID: 28421698 DOI: 10.1002/eap.1560] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/20/2016] [Revised: 03/16/2017] [Accepted: 03/27/2017] [Indexed: 06/07/2023]
Abstract
While advances in remote sensing have made stand, landscape, and regional assessments of the direct impacts of disturbance on forests quite common, the edge influence of timber harvesting on the structure of neighboring unharvested forests has not been examined extensively. In this study, we examine the impact of historical timber harvests on basal area patterns of neighboring old-growth forests to assess the magnitude and scale of harvest edge influence in a forest landscape of western Oregon, USA. We used lidar data and forest plot measurements to construct 30-m resolution live tree basal area maps in lower and middle elevation mature and old-growth forests. We assessed how edge influence on total, upper canopy, and lower canopy basal area varied across this forest landscape as a function of harvest characteristics (i.e., harvest size and age) and topographic conditions in the unharvested area. Upper canopy, lower canopy, and total basal area increased with distance from harvest edge and elevation. Forests within 75 m of harvest edges (20% of unharvested forests) had 4% to 6% less live tree basal area compared with forest interiors. An interaction between distance from harvest edge and elevation indicated that elevation altered edge influence in this landscape. We observed a positive edge influence at low elevations (<800 m) and a negative edge influence at moderate to high elevations (>800 m). Surprisingly, we found no or weak effects of harvest age (13-60 yr) and harvest area (0.2-110 ha) on surrounding unharvested forest basal area, implying that edge influence was relatively insensitive to the scale of disturbance and multi-decadal recovery processes. Our study indicates that the edge influence of past clearcutting on the structure of neighboring uncut old-growth forests is widespread and persistent. These indirect and diffuse legacies of historical timber harvests complicate forest management decision-making in old-growth forest landscapes by broadening the traditional view of stand boundaries. Furthermore, the consequences of forest harvesting may reach across ownership boundaries, highlighting complex governance issues surrounding landscape management of old-growth forests.
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Affiliation(s)
- David M Bell
- USDA Forest Service Pacific Northwest Research Station, 3200 SW Jefferson Way, Corvallis, Oregon, 97331, USA
| | - Thomas A Spies
- USDA Forest Service Pacific Northwest Research Station, 3200 SW Jefferson Way, Corvallis, Oregon, 97331, USA
| | - Robert Pabst
- Department of Forest Ecosystems and Society, Oregon State University, 321 Richardson Hall, Corvallis, Oregon, 97331, USA
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Bell DM, Imre D, T. Martin S, Zelenyuk A. The properties and behavior of α-pinene secondary organic aerosol particles exposed to ammonia under dry conditions. Phys Chem Chem Phys 2017; 19:6497-6507. [DOI: 10.1039/c6cp08839b] [Citation(s) in RCA: 21] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
Chemical transformations and aging of secondary organic aerosol (SOA) particles can alter their physical and chemical properties, including particle morphology.
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Clark JS, Iverson L, Woodall CW, Allen CD, Bell DM, Bragg DC, D'Amato AW, Davis FW, Hersh MH, Ibanez I, Jackson ST, Matthews S, Pederson N, Peters M, Schwartz MW, Waring KM, Zimmermann NE. The impacts of increasing drought on forest dynamics, structure, and biodiversity in the United States. Glob Chang Biol 2016; 22:2329-2352. [PMID: 26898361 DOI: 10.1111/gcb.13160] [Citation(s) in RCA: 161] [Impact Index Per Article: 20.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/22/2015] [Revised: 10/02/2015] [Accepted: 10/05/2015] [Indexed: 06/05/2023]
Abstract
We synthesize insights from current understanding of drought impacts at stand-to-biogeographic scales, including management options, and we identify challenges to be addressed with new research. Large stand-level shifts underway in western forests already are showing the importance of interactions involving drought, insects, and fire. Diebacks, changes in composition and structure, and shifting range limits are widely observed. In the eastern US, the effects of increasing drought are becoming better understood at the level of individual trees, but this knowledge cannot yet be confidently translated to predictions of changing structure and diversity of forest stands. While eastern forests have not experienced the types of changes seen in western forests in recent decades, they too are vulnerable to drought and could experience significant changes with increased severity, frequency, or duration in drought. Throughout the continental United States, the combination of projected large climate-induced shifts in suitable habitat from modeling studies and limited potential for the rapid migration of tree populations suggests that changing tree and forest biogeography could substantially lag habitat shifts already underway. Forest management practices can partially ameliorate drought impacts through reductions in stand density, selection of drought-tolerant species and genotypes, artificial regeneration, and the development of multistructured stands. However, silvicultural treatments also could exacerbate drought impacts unless implemented with careful attention to site and stand characteristics. Gaps in our understanding should motivate new research on the effects of interactions involving climate and other species at the stand scale and how interactions and multiple responses are represented in models. This assessment indicates that, without a stronger empirical basis for drought impacts at the stand scale, more complex models may provide limited guidance.
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Affiliation(s)
- James S Clark
- Nicholas School of the Environment, Duke University, Durham, NC, 27708, USA
| | - Louis Iverson
- Forest Service, Northern Research Station, 359 Main Road, Delaware, OH, 43015, USA
| | | | - Craig D Allen
- U.S. Geological Survey, Fort Collins Science Center, Jemez Mountains Field Station, Los Alamos, NM, 87544, USA
| | - David M Bell
- Forest Service, Pacific Northwest Research Station, Corvallis, OR, 97331, USA
| | - Don C Bragg
- Forest Service, Southern Research Station, Monticello, AR, 71656, USA
| | - Anthony W D'Amato
- Rubenstein School of Environment and Natural Resources, University of Vermont, 04E Aiken Center, 81 Carrigan Dr., Burlington, VT, 05405, USA
| | - Frank W Davis
- Bren School of Environmental Science and Management, University of California, Santa Barbara, CA, 93106, USA
| | - Michelle H Hersh
- Department of Biology, Sarah Lawrence College, New York, NY, 10708, USA
| | - Ines Ibanez
- School of Natural Resources and Environment, University of Michigan, 2546 Dana Building, Ann Arbor, MI, 48109, USA
| | - Stephen T Jackson
- U.S. Geological Survey, Southwest Climate Science Center and Department of Geosciences, University of Arizona, 1064 E. Lowell St., PO Box 210137, Tucson, AZ, 85721, USA
| | - Stephen Matthews
- School of Environment and Natural Resources, Ohio State University, Columbus, OH, 43210, USA
| | | | - Matthew Peters
- Forest Service, Northern Research Station, Delaware, OH, 43015, USA
| | - Mark W Schwartz
- Department of Environmental Science and Policy, UC Davis, Davis, CA, 93106, USA
| | - Kristen M Waring
- School of Forestry, Northern Arizona University, Flagstaff, AZ, 86001, USA
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Riva M, Bell DM, Hansen AMK, Drozd GT, Zhang Z, Gold A, Imre D, Surratt JD, Glasius M, Zelenyuk A. Effect of Organic Coatings, Humidity and Aerosol Acidity on Multiphase Chemistry of Isoprene Epoxydiols. Environ Sci Technol 2016; 50:5580-8. [PMID: 27176464 DOI: 10.1021/acs.est.5b06050] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/03/2023]
Abstract
Multiphase chemistry of isomeric isoprene epoxydiols (IEPOX) has been shown to be the dominant source of isoprene-derived secondary organic aerosol (SOA). Recent studies have reported particles composed of ammonium bisulfate (ABS) mixed with model organics exhibit slower rates of IEPOX uptake. In the present study, we investigate the effect of atmospherically relevant organic coatings of α-pinene (AP) SOA on the reactive uptake of trans-β-IEPOX onto ABS particles under different conditions and coating thicknesses. Single particle mass spectrometry was used to characterize in real-time particle size, shape, density, and quantitative composition before and after reaction with IEPOX. We find that IEPOX uptake by pure sulfate particles is a volume-controlled process, which results in particles with uniform concentration of IEPOX-derived SOA across a wide range of sizes. Aerosol acidity was shown to enhance IEPOX-derived SOA formation, consistent with recent studies. The presence of water has a weaker impact on IEPOX-derived SOA yield, but significantly enhanced formation of 2-methyltetrols, consistent with offline filter analysis. In contrast, IEPOX uptake by ABS particles coated with AP-derived SOA is lower compared to that of pure ABS particles, strongly dependent on particle composition, and therefore on particle size.
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Affiliation(s)
- Matthieu Riva
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599-7400, United States
| | - David M Bell
- Pacific Northwest National Laboratory , 3335 Innovation Boulevard, Richland, Washington 99354, United States
| | | | - Greg T Drozd
- Department of Environmental Science, Policy, and Management, University of California , Berkeley, California 94720, United States
| | - Zhenfa Zhang
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599-7400, United States
| | - Avram Gold
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599-7400, United States
| | - Dan Imre
- Imre Consulting , Richland, Washington 99352, United States
| | - Jason D Surratt
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, The University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599-7400, United States
| | - Marianne Glasius
- Department of Chemistry, Aarhus University , Langelandsgade 140, DK-8000 Aarhus, Denmark
| | - Alla Zelenyuk
- Pacific Northwest National Laboratory , 3335 Innovation Boulevard, Richland, Washington 99354, United States
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Bell DM, Clark JS. Seed predation and climate impacts on reproductive variation in temperate forests of the southeastern USA. Oecologia 2016; 180:1223-34. [PMID: 26747267 DOI: 10.1007/s00442-015-3537-6] [Citation(s) in RCA: 15] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/26/2015] [Accepted: 12/17/2015] [Indexed: 11/26/2022]
Abstract
Climatic effects on tree recruitment will be determined by the interactive effects of fecundity and seed predation. Evaluating how insect and vertebrate seed predators mediate tree reproductive responses to climate depends on long-term studies of seed production, development, and predation. In this study, our objectives were to (1) assess the effects of interannual climate variation on seed abortion rates, (2) assess the impact of seed density on predation rates, and (3) examine the degree to which density-dependent seed predation would amplify or dampen interannual variation in fecundity associated with seed abortion. We used a 19-year study of seed abortion and pre-dispersal predation rates by insects and vertebrates (birds and rodents) for five temperate tree species across forest plots from the North Carolina Piedmont to the Southern Appalachian Mountains in the southeastern USA. We found that rates of seed abortion and predation increased reproductive variation for oaks (Quercus species). Probability of seed abortion was greatest during years with cool, dry springs. Responses of seed predation on Quercus species to current year's seed density varied by species, but exhibited positive density-dependence to previous year's seed density consistent with numerical responses of seed predators. Seed abortion and predation rates for two drupe species responded little to variation in climate or seed density, respectively. Given that predation increased interannual variation in seed availability and the negative density-dependence to previous year's seed density, our results indicate that consistent numerical responses of oak seed predators may amplify interannual variation due to climate-mediated processes like seed abortion.
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Affiliation(s)
- David M Bell
- Pacific Northwest Research Station, USDA Forest Service, 3200 SW Jefferson Way, Corvallis, OR, 97331, USA.
| | - James S Clark
- Nicholas School of the Environment, Duke University, Durham, NC, USA
- Department of Biology, Duke University, Durham, NC, USA
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Moran EV, Hartig F, Bell DM. Intraspecific trait variation across scales: implications for understanding global change responses. Glob Chang Biol 2016; 22:137-50. [PMID: 26061811 DOI: 10.1111/gcb.13000] [Citation(s) in RCA: 147] [Impact Index Per Article: 18.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/18/2015] [Accepted: 05/21/2015] [Indexed: 05/03/2023]
Abstract
Recognition of the importance of intraspecific variation in ecological processes has been growing, but empirical studies and models of global change have only begun to address this issue in detail. This review discusses sources and patterns of intraspecific trait variation and their consequences for understanding how ecological processes and patterns will respond to global change. We examine how current ecological models and theories incorporate intraspecific variation, review existing data sources that could help parameterize models that account for intraspecific variation in global change predictions, and discuss new data that may be needed. We provide guidelines on when it is most important to consider intraspecific variation, such as when trait variation is heritable or when nonlinear relationships are involved. We also highlight benefits and limitations of different model types and argue that many common modeling approaches such as matrix population models or global dynamic vegetation models can allow a stronger consideration of intraspecific trait variation if the necessary data are available. We recommend that existing data need to be made more accessible, though in some cases, new experiments are needed to disentangle causes of variation.
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Affiliation(s)
- Emily V Moran
- School of Natural Sciences, UC Merced, Merced, CA, 95343, USA
| | - Florian Hartig
- Department of Biometry and Environmental System Analysis, University of Freiburg, Freiburg, 79106, Germany
| | - David M Bell
- Pacific Northwest Research Station, USDA Forest Service, Portland, OR, 97204, USA
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Bell DM, Bradford JB, Lauenroth WK. Scale dependence of disease impacts on quaking aspen (Populus tremuloides) mortality in the southwestern United States. Ecology 2015; 96:1835-45. [PMID: 26378306 DOI: 10.1890/14-1184.1] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Submit a Manuscript] [Subscribe] [Scholar Register] [Indexed: 11/18/2022]
Abstract
Depending on how disease impacts tree exposure to risk, both the prevalence of disease and disease effects on survival may contribute to patterns of mortality risk across a species' range. Disease may accelerate tree species' declines in response to global change factors, such as drought, biotic interactions, such as competition, or functional traits, such as allometry. To assess the role of disease in mediating mortality risk in quaking aspen (Populus tremuloides), we developed hierarchical Bayesian models for both disease prevalence in live aspen stems and the resulting survival rates of healthy and diseased aspen near the species' southern range limit using 5088 individual trees on 281 United States Forest Service Forest Inventory and Analysis plots in the southwestern United States. We found that disease prevalence depended primarily on tree size, tree allometry, and spatial variation in precipitation, while mortality depended on tree size, allometry, competition, spatial variation in summer temperature, and both temporal and spatial variation in summer precipitation. Disease prevalence was highest in large trees with low slenderness found on dry sites. For healthy trees, mortality decreased with diameter, slenderness, and temporal variation in summer precipitation, but increased with competition and spatial variation in summer temperature. Mortality of diseased trees decreased with diameter and aspen relative basal area and increased with mean summer temperature and precipitation. Disease infection increased aspen mortality, especially in trees of intermediate size and trees on plots at climatic extremes (i.e., cool, wet and warm, dry climates). By examining variation in disease prevalence, mortality of healthy trees, and mortality of diseased trees, we showed that the role of disease in aspen tree mortality depended on the scale of inference. For variation among individuals in diameter, disease tended to expose intermediate-size trees experiencing moderate risk to greater risk. For spatial variation in summer temperature, disease exposed lower risk populations to greater mortality probabilities, but the magnitude of this exposure depended on summer precipitation. Furthermore, the importance of diameter and slenderness in mediating responses to climate supports the increasing emphasis on trait variation in studies of ecological responses to global change.
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Bell DM, Ward EJ, Oishi AC, Oren R, Flikkema PG, Clark JS. A state-space modeling approach to estimating canopy conductance and associated uncertainties from sap flux density data. Tree Physiol 2015; 35:792-802. [PMID: 26063709 DOI: 10.1093/treephys/tpv041] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/15/2014] [Accepted: 04/27/2015] [Indexed: 06/04/2023]
Abstract
Uncertainties in ecophysiological responses to environment, such as the impact of atmospheric and soil moisture conditions on plant water regulation, limit our ability to estimate key inputs for ecosystem models. Advanced statistical frameworks provide coherent methodologies for relating observed data, such as stem sap flux density, to unobserved processes, such as canopy conductance and transpiration. To address this need, we developed a hierarchical Bayesian State-Space Canopy Conductance (StaCC) model linking canopy conductance and transpiration to tree sap flux density from a 4-year experiment in the North Carolina Piedmont, USA. Our model builds on existing ecophysiological knowledge, but explicitly incorporates uncertainty in canopy conductance, internal tree hydraulics and observation error to improve estimation of canopy conductance responses to atmospheric drought (i.e., vapor pressure deficit), soil drought (i.e., soil moisture) and above canopy light. Our statistical framework not only predicted sap flux observations well, but it also allowed us to simultaneously gap-fill missing data as we made inference on canopy processes, marking a substantial advance over traditional methods. The predicted and observed sap flux data were highly correlated (mean sensor-level Pearson correlation coefficient = 0.88). Variations in canopy conductance and transpiration associated with environmental variation across days to years were many times greater than the variation associated with model uncertainties. Because some variables, such as vapor pressure deficit and soil moisture, were correlated at the scale of days to weeks, canopy conductance responses to individual environmental variables were difficult to interpret in isolation. Still, our results highlight the importance of accounting for uncertainty in models of ecophysiological and ecosystem function where the process of interest, canopy conductance in this case, is not observed directly. The StaCC modeling framework provides a statistically coherent approach to estimating canopy conductance and transpiration and propagating estimation uncertainty into ecosystem models, paving the way for improved prediction of water and carbon uptake responses to environmental change.
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Affiliation(s)
- David M Bell
- USDA Forest Service, Pacific Northwest Research Station, Corvallis, OR, USA
| | - Eric J Ward
- Department of Forestry and Environmental Resources, North Carolina State University, Raleigh, NC, USA
| | | | - Ram Oren
- Nicholas School of the Environment, Duke University, Durham, NC, USA
| | - Paul G Flikkema
- Department of Electrical Engineering and Computer Science, Northern Arizona University, Flagstaff, AZ, USA
| | - James S Clark
- Nicholas School of the Environment, Duke University, Durham, NC, USA
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McPherson SD, Bell DM. Combined cataract extraction and trabeculotomy; further experiences. Dev Ophthalmol 2015; 5:59-63. [PMID: 7343357 DOI: 10.1159/000400941] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/24/2023]
Abstract
A procedure combining external trabeculotomy with intracapsular cataract extraction was performed in 40 eyes of 28 patients. 77.5% were controlled without medication and there was no final reduction in visual acuity due to complication from the combined operations. The procedure is advocated for patients with glucoma who must undergo cataract extraction.
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Moore LM, Lauenroth WK, Bell DM, Schlaepfer DR. Soil Water and Temperature Explain Canopy Phenology and Onset of Spring in a Semiarid Steppe. ACTA ACUST UNITED AC 2015. [DOI: 10.1353/gpr.2015.0027] [Citation(s) in RCA: 19] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/11/2022]
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Howder CR, Long BA, Bell DM, Furakawa KH, Johnson RC, Fang Z, Anderson SL. Photoluminescence of charged CdSe/ZnS quantum dots in the gas phase: effects of charge and heating on absorption and emission probabilities. ACS Nano 2014; 8:12534-12548. [PMID: 25427008 DOI: 10.1021/nn505374d] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/04/2023]
Abstract
Gas phase spectral measurements for CdSe/ZnS core/shell nanocrystal quantum dots (QDs) before and after heating with both infrared (CO2) and visible lasers are reported. As-trapped QDs are spectrally similar to the same QDs in solution; however their photoluminescence (PL) intensities are very low, at least partly due to low absorption cross sections. After heating, the PL intensities brighten by factors ranging from ∼4 to 1800 depending on the QD size and pump laser wavelength. The emission spectra no longer resemble solution spectra and are similar, regardless of the QD diameter. Emission extends from the pump laser wavelength into the near-IR, with strong emission features above the band gap energy, between 645 and 775 nm, and in the near-infrared. Emission spectra from brightened QD ensembles, single QD aggregates, and single QD monomers are similar, showing that even single QDs support PL from a wide variety of states. The heating and cooling processes for QDs in this environment are analyzed, providing limits on the magnitudes of the absorption cross sections before and after thermal brightening. A model, based on absorption bleaching by extra electrons in the conduction band, appears to account for the changes in absorption and emission behavior induced by charging and heating.
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Affiliation(s)
- Collin R Howder
- Department of Chemistry, University of Utah , Salt Lake City, Utah 84112, United States
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Abstract
Because forest stand structure, age, and productivity can mediate the impacts of climate on quaking aspen (Populus tremuloides) mortality, ignoring stand-scale factors limits inference on the drivers of recent sudden aspen decline. Using the proportion of aspen trees that were dead as an index of recent mortality at 841 forest inventory plots, we examined the relationship of this mortality index to forest structure and climate in the Rocky Mountains and Intermountain Western United States. We found that forest structure explained most of the patterns in mortality indices, but that variation in growing-season vapor pressure deficit and winter precipitation over the last 20 years was important. Mortality index sensitivity to precipitation was highest in forests where aspen exhibited high densities, relative basal areas, quadratic mean diameters, and productivities, whereas sensitivity to vapor pressure deficit was highest in young forest stands. These results indicate that the effects of drought on mortality may be mediated by forest stand development, competition with encroaching conifers, and physiological vulnerabilities of large trees to drought. By examining mortality index responses to both forest structure and climate, we show that forest succession cannot be ignored in studies attempting to understand the causes and consequences of sudden aspen decline.
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Bell DM, Howder CR, Anderson SL. Effects of translational and vibrational excitation on the reaction of HOD+ with C2H2 and C2D2: mode- and bond-specific effects in exoergic proton transfer. J Phys Chem A 2014; 118:8360-72. [PMID: 24678576 DOI: 10.1021/jp501304v] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Abstract
Reactions of mode-selectively excited HOD(+) with C2H2 and C2D2 were studied over the center-of-mass collision energy (Ecol) range from 0.15 to 2.9 eV. HOD(+) was prepared in each of its fundamental vibrational states: ground state (000), bend (010), OD stretch (100), and the OH stretch (001). Charge transfer is the dominant reaction at all energies, although it is inhibited by increasing Ecol, and is accompanied by hydrogen exchange. The total charge transfer cross section is similar for C2H2 and C2D2, however, the tendency toward charge transfer with hydrogen exchange (CTHE) is significantly greater for C2D2 compared to C2H2. Charge transfer shows no significant effects of HOD(+) vibrational excitation, however, CTHE is significantly enhanced by vibration at Ecol < 0.62 eV. Both H(+) and D(+) transfer reactions (HT, and DT, respectively) are observed for both C2H2 and C2D2, with little dependence on collision energy, but with mode- and bond-specific enhancements from excitation of the OH and OD stretches. Recoil velocity measurements show that all channels are direct, except perhaps at the lowest collision energies. Mode-specific effects on the recoil velocity distributions are also observed, revealing how vibrational excitation affects reaction at different collision impact parameters.
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Affiliation(s)
- David M Bell
- Department of Chemistry, University of Utah , 315 South 1400 East, Salt Lake City, Utah 84112, United States
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Clark JS, Bell DM, Kwit MC, Zhu K. Competition-interaction landscapes for the joint response of forests to climate change. Glob Chang Biol 2014; 20:1979-1991. [PMID: 24932467 DOI: 10.1111/gcb.12425] [Citation(s) in RCA: 37] [Impact Index Per Article: 3.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/03/2023]
Abstract
The recent global increase in forest mortality episodes could not have been predicted from current vegetation models that are calibrated to regional climate data. Physiological studies show that mortality results from interactions between climate and competition at the individual scale. Models of forest response to climate do not include interactions because they are hard to estimate and require long-term observations on individual trees obtained at frequent (annual) intervals. Interactions involve multiple tree responses that can only be quantified if these responses are estimated as a joint distribution. A new approach provides estimates of climate–competition interactions in two critical ways, (i) among individuals, as a joint distribution of responses to combinations of inputs, such as resources and climate, and (ii) within individuals, due to allocation requirements that control outputs, such as demographic rates. Application to 20 years of data from climate and competition gradients shows that interactions control forest responses, and their omission from models leads to inaccurate predictions. Species most vulnerable to increasing aridity are not those that show the largest growth response to precipitation, but rather depend on interactions with the local resource environment. This first assessment of regional species vulnerability that is based on the scale at which climate operates, individual trees competing for carbon and water, supports predictions of potential savannification in the southeastern US.
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Bell DM, Bradford JB, Lauenroth WK. Mountain landscapes offer few opportunities for high-elevation tree species migration. Glob Chang Biol 2014; 20:1441-1451. [PMID: 24353188 DOI: 10.1111/gcb.12504] [Citation(s) in RCA: 19] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/08/2013] [Accepted: 11/24/2013] [Indexed: 06/03/2023]
Abstract
Climate change is anticipated to alter plant species distributions. Regional context, notably the spatial complexity of climatic gradients, may influence species migration potential. While high-elevation species may benefit from steep climate gradients in mountain regions, their persistence may be threatened by limited suitable habitat as land area decreases with elevation. To untangle these apparently contradictory predictions for mountainous regions, we evaluated the climatic suitability of four coniferous forest tree species of the western United States based on species distribution modeling (SDM) and examined changes in climatically suitable areas under predicted climate change. We used forest structural information relating to tree species dominance, productivity, and demography from an extensive forest inventory system to assess the strength of inferences made with a SDM approach. We found that tree species dominance, productivity, and recruitment were highest where climatic suitability (i.e., probability of species occurrence under certain climate conditions) was high, supporting the use of predicted climatic suitability in examining species risk to climate change. By predicting changes in climatic suitability over the next century, we found that climatic suitability will likely decline, both in areas currently occupied by each tree species and in nearby unoccupied areas to which species might migrate in the future. These trends were most dramatic for high elevation species. Climatic changes predicted over the next century will dramatically reduce climatically suitable areas for high-elevation tree species while a lower elevation species, Pinus ponderosa, will be well positioned to shift upslope across the region. Reductions in suitable area for high-elevation species imply that even unlimited migration would be insufficient to offset predicted habitat loss, underscoring the vulnerability of these high-elevation species to climatic changes.
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Affiliation(s)
- David M Bell
- Department of Botany, University of Wyoming, 1000 E. University Ave, Laramie, WY, 82071, US
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Bell DM, Howder CR, Johnson RC, Anderson SL. Single CdSe/ZnS nanocrystals in an ion trap: charge and mass determination and photophysics evolution with changing mass, charge, and temperature. ACS Nano 2014; 8:2387-2398. [PMID: 24410129 DOI: 10.1021/nn405920k] [Citation(s) in RCA: 20] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/03/2023]
Abstract
We report measurements of fluorescence intermittency (blinking) and spectral behavior for single semiconductor nanocrystal quantum dots (QDs) isolated in the gas phase and discuss the effects on fluorescence of the QD charge state and heating to the point of sublimation. Core-shell CdSe/ZnS QDs were trapped in a quadrupole ion trap and detected by laser-induced fluorescence. The mass (M) and charge (Q) were determined nondestructively, and both were followed continuously over the course of hours or days. Emission spectra of the trapped QDs are significantly red-shifted relative to the solution-phase emission from the same particles. The temperature of the trapped QDs is determined by the balance between laser heating and collisional cooling and thermal emission, and it is possible to heat the particles to remove ligands or to the point of sublimation. QDs are observed to be emissive during sublimation, for up to 85% mass loss, with emission intensity roughly proportional to the surface area. Eventually, the fluorescence quantum yield drops suddenly, and the QDs begin to blink. The method used is versatile and will allow studies of quantum dot optical properties as a function of size, ligand removal, heating, surface oxidation, and other manipulations, where these properties are continuously correlated with the mass and charge.
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Affiliation(s)
- David M Bell
- Department of Chemistry, University of Utah , Salt Lake City, Utah 84112, United States
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Howder CR, Bell DM, Anderson SL. Optically detected, single nanoparticle mass spectrometer with pre-filtered electrospray nanoparticle source. Rev Sci Instrum 2014; 85:014104. [PMID: 24517786 DOI: 10.1063/1.4861923] [Citation(s) in RCA: 15] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/03/2023]
Abstract
An instrument designed for non-destructive mass analysis of single trapped nanoparticles is described. The heart of the instrument is a 3D quadrupole (Paul) trap constructed to give optical access to the trap center along ten directions, allowing passage of lasers for particle heating and detection, particle injection, collection of scattered or fluorescent photons for particle detection and mass analysis, and collection of particles on TEM grids for analysis, as needed. Nanoparticles are injected using an electrospray ionization (ESI) source, and conditions are described for spraying and trapping polymer particles, bare metal particles, and ligand stabilized particles with masses ranging from 200 kDa to >3 GDa. Conditions appropriate to ESI and injection of different types of particles are described. The instrument is equipped with two ion guides separating the ESI source and nanoparticle trap. The first ion guide is mostly to allow desolvation and differential pumping before the particles enter the trap section of the instrument. The second is a linear quadrupole guide, which can be operated in mass selective or mass band-pass modes to limit transmission to species with mass-to-charge ratios in the range of interest. With a little experience, the design allows injection of single particles into the trap upon demand.
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Affiliation(s)
- Collin R Howder
- Chemistry Department, University of Utah, 315 S. 1400 E, Salt Lake City, Utah 84112, USA
| | - David M Bell
- Chemistry Department, University of Utah, 315 S. 1400 E, Salt Lake City, Utah 84112, USA
| | - Scott L Anderson
- Chemistry Department, University of Utah, 315 S. 1400 E, Salt Lake City, Utah 84112, USA
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Bell DM, Anderson SL. Vibrationally enhanced charge transfer and mode/bond-specific H+ and D+ transfer in the reaction of HOD+ with N2O. J Chem Phys 2013; 139:114305. [PMID: 24070288 DOI: 10.1063/1.4820955] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/15/2022] Open
Abstract
The reaction of HOD(+) with N2O was studied over the collision energy (E(col)) range from 0.20 eV to 2.88 eV, for HOD(+) in its ground state and in each of its fundamental vibrational states: bend (010), OD stretch (100), and OH stretch (001). The dominant reaction at low E(col) is H(+) and D(+) transfer, but charge transfer becomes dominant for E(col) > 0.5 eV. Increasing E(col) enhances charge transfer only in the threshold region (E(col) < 1 eV), but all modes of HOD(+) vibrational excitation enhance this channel over the entire energy range, by up to a factor of three. For reaction of ground state HOD(+), the H(+) and D(+) transfer channels have similar cross sections, enhanced by increasing collision energy for E(col) < 0.3 eV, but suppressed by E(col) at higher energies. OD stretch excitation enhances D(+) transfer by over a factor of 2, but has little effect on H(+) transfer, except at low E(col) where a modest enhancement is observed. Excitation of the OH stretch enhances H(+) transfer by up to a factor of 2.5, but actually suppresses D(+) transfer over most of the E(col) range. Excitation of the bend mode results in ~60% enhancement of both H(+) and D(+) transfer at low E(col) but has little effect at higher energies. Recoil velocity distributions at high E(col) are strongly backscattered in the center-of-mass frame, indicating direct reaction dominated by large impact parameter collisions. At low E(col) the distributions are compatible with mediation by a short-lived collision complex. Ab initio calculations find several complexes that may be important in this context, and RRKM calculations predict lifetimes and decay branching that is consistent with observations. The recoil velocity distributions show that HOD(+) vibrational excitation enhances reactivity in all collisions at low E(col), while for high E(col) with enhancement comes entirely from the subset of collisions that generate strongly back-scattered product ions.
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Affiliation(s)
- David M Bell
- Department of Chemistry, University of Utah, 315 S. 1400 E., Salt Lake City, Utah 84112, USA
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