1
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Xie Q, Halpern ER, Zhang J, Shrivastava M, Zelenyuk A, Zaveri RA, Laskin A. Volatility Basis Set Distributions and Viscosity of Organic Aerosol Mixtures: Insights from Chemical Characterization Using Temperature-Programmed Desorption-Direct Analysis in Real-Time High-Resolution Mass Spectrometry. Anal Chem 2024. [PMID: 38815054 DOI: 10.1021/acs.analchem.4c01003] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 06/01/2024]
Abstract
Quantitative assessment of gas-particle partitioning of individual components within complex atmospheric organic aerosol (OA) mixtures is critical for predicting and comprehending the formation and evolution of OA particles in the atmosphere. This investigation leverages previously documented data obtained through a temperature-programmed desorption-direct analysis in real-time, high-resolution mass spectrometry (TPD-DART-HRMS) platform. This methodology facilitates the bottom-up construction of volatility basis set (VBS) distributions for constituents found in three biogenic secondary organic aerosol (SOA) mixtures produced through the ozonolysis of α-pinene, limonene, and ocimene. The apparent enthalpies (ΔH*, kJ mol-1) and saturation mass concentrations (CT*, μg·m-3) of individual SOA components, determined as a function of temperature (T, K), facilitated an assessment of changes in VBS distributions and gas-particle partitioning with respect to T and atmospheric total organic mass loadings (tOM, μg·m-3). The VBS distributions reveal distinct differences in volatilities among monomers, dimers, and trimers, categorized into separate volatility bins. At the ambient temperature of T = 298 K, only monomers efficiently partition between gas and particle phases across a broad range of atmospherically relevant tOM values of 1-100 μg·m-3. Partitioning of dimers and trimers becomes notable only at T > 360 K and T > 420 K, respectively. The viscosity of SOA mixtures is assessed using a bottom-up calculation approach, incorporating the input of elemental formulas, ΔH*, CT*, and particle-phase mass fractions of the SOA components. Through this approach, we are able to accurately estimate the variations in SOA viscosity that result from the evaporation of its components. These variations are, in turn, influenced by atmospherically relevant changes in tOM and T. Comparison of the calculated SOA viscosity and diffusivity values with literature reported experimental results shows close agreement, thereby validating the employed calculation approach. These findings underscore the significant potential for TPD-DART-HRMS measurements in enabling the untargeted analysis of organic molecules within OA mixtures. This approach facilitates quantitative assessment of their gas-particle partitioning and allows for the estimation of their viscosity and condensed-phase diffusion, thereby contributing valuable insights to atmospheric models.
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Affiliation(s)
- Qiaorong Xie
- Department of Chemistry, Purdue University, West Lafayette, Indiana 47907, United States
| | - Emily R Halpern
- Department of Chemistry, Purdue University, West Lafayette, Indiana 47907, United States
| | - Jie Zhang
- Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Manish Shrivastava
- Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Alla Zelenyuk
- Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Rahul A Zaveri
- Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, Washington 99352, United States
| | - Alexander Laskin
- Department of Chemistry, Purdue University, West Lafayette, Indiana 47907, United States
- Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, Indiana 47907, United States
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2
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Huang Q, Lu H, Li J, Ying Q, Gao Y, Wang H, Guo S, Lu K, Qin M, Hu J. Modeling the molecular composition of secondary organic aerosol under highly polluted conditions: A case study in the Yangtze River Delta Region in China. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 938:173327. [PMID: 38761930 DOI: 10.1016/j.scitotenv.2024.173327] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/06/2024] [Revised: 05/07/2024] [Accepted: 05/15/2024] [Indexed: 05/20/2024]
Abstract
A near-explicit mechanism, the master chemical mechanism (MCMv3.3.1), coupled with the Community Multiscale Air Quality (CMAQ) model (CMAQ-MCM-SOA), was applied to investigate the characteristics of secondary organic aerosol (SOA) during a pollution event in the Yangtze River Delta (YRD) region in summer 2018. Model performances in predicting explicit volatile organic compounds (VOCs), organic aerosol (OA), secondary organic carbon (SOC), and other related pollutants in Taizhou, as well as ozone (O3) and fine particulate matter (PM2.5) in multiple cities in this region, were evaluated against observations and model predictions by the CMAQ model coupled with a lumped photochemical mechanism (SAPRC07tic, S07). MCM and S07 exhibited similar performances in predicting gaseous species, while MCM better captured the observed PM2.5 and inorganic aerosols. Both models underpredicted OA concentrations. When excluding data during biomass burning events, SOC concentrations were underpredicted by the CMAQ-MCM-SOA model (-28.4 %) and overpredicted by the CMAQ-S07 model (134.4 %), with better agreement with observations in the trend captured by the CMAQ-MCM-SOA model. Dicarbonyl SOA accounted for a significant fraction of total SOA in the YRD, while organic nitrates originating from aromatics were the most abundant species contributing to the SOA formation from gas-particle partitioning. The oxygen-to‑carbon ratio (O/C) for SOA and OA were 0.68-0.75 and 0.20-0.65, respectively, indicating a higher oxidation state in the areas influenced by biogenic emissions. Finally, the phase state of SOA was examined by calculating the glass transition temperature (Tg) based on its molecular composition. It was found that semi-solid state characterized SOA in the YRD, which could potentially impact their chemical transformation and lifetimes along with those of their precursors.
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Affiliation(s)
- Qi Huang
- Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China
| | - Hutao Lu
- Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China
| | - Jingyi Li
- Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China.
| | - Qi Ying
- Zachry Department of Civil and Environmental Engineering, Texas A&M University, College Station, TX 77843, USA
| | - Yaqin Gao
- State Environmental Protection Key Laboratory of the Formation and Prevention of Urban Air Pollution Complex, Shanghai Academy of Environmental Sciences, Shanghai 200233, China
| | - Hongli Wang
- State Environmental Protection Key Laboratory of the Formation and Prevention of Urban Air Pollution Complex, Shanghai Academy of Environmental Sciences, Shanghai 200233, China
| | - Song Guo
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Keding Lu
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Momei Qin
- Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China
| | - Jianlin Hu
- Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China
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3
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Chen B, Mirrielees JA, Chen Y, Onasch TB, Zhang Z, Gold A, Surratt JD, Zhang Y, Brooks SD. Glass Transition Temperatures of Organic Mixtures from Isoprene Epoxydiol-Derived Secondary Organic Aerosol. J Phys Chem A 2023; 127:4125-4136. [PMID: 37129903 PMCID: PMC10863072 DOI: 10.1021/acs.jpca.2c08936] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/21/2022] [Revised: 04/18/2023] [Indexed: 05/03/2023]
Abstract
The phase states and glass transition temperatures (Tg) of secondary organic aerosol (SOA) particles are important to resolve for understanding the formation, growth, and fate of SOA as well as their cloud formation properties. Currently, there is a limited understanding of how Tg changes with the composition of organic and inorganic components of atmospheric aerosol. Using broadband dielectric spectroscopy, we measured the Tg of organic mixtures containing isoprene epoxydiol (IEPOX)-derived SOA components, including 2-methyltetrols (2-MT), 2-methyltetrol-sulfate (2-MTS), and 3-methyltetrol-sulfate (3-MTS). The results demonstrate that the Tg of mixtures depends on their composition. The Kwei equation, a modified Gordon-Taylor equation with an added quadratic term and a fitting parameter representing strong intermolecular interactions, provides a good fit for the Tg-composition relationship of complex mixtures. By combining Raman spectroscopy with geometry optimization simulations obtained using density functional theory, we demonstrate that the non-linear deviation of Tg as a function of composition may be caused by changes in the extent of hydrogen bonding in the mixture.
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Affiliation(s)
- Bo Chen
- Department
of Atmospheric Sciences, Texas A&M University, Eller O&M Building, 1204, 3150
TAMU, 797 Lamar Street, College Station, Texas 77843, United States
| | - Jessica A. Mirrielees
- Department
of Chemistry, University of Michigan, 930 N University Avenue, Ann Arbor, Michigan 48104, United States
| | - Yuzhi Chen
- Gillings
School of Global Public Health, Department of Environmental Sciences
and Engineering, University of North Carolina
at Chapel Hill, 170 Rosenau Hall, Campus Box #7400, 135 Dauer Drive, Chapel Hill, North Carolina 27599, United States
| | - Timothy B. Onasch
- Aerodyne
Research, Inc, 45 Manning
Road, Billerica, Massachusetts 01821, United States
| | - Zhenfa Zhang
- Gillings
School of Global Public Health, Department of Environmental Sciences
and Engineering, University of North Carolina
at Chapel Hill, 170 Rosenau Hall, Campus Box #7400, 135 Dauer Drive, Chapel Hill, North Carolina 27599, United States
| | - Avram Gold
- Gillings
School of Global Public Health, Department of Environmental Sciences
and Engineering, University of North Carolina
at Chapel Hill, 170 Rosenau Hall, Campus Box #7400, 135 Dauer Drive, Chapel Hill, North Carolina 27599, United States
| | - Jason D. Surratt
- Gillings
School of Global Public Health, Department of Environmental Sciences
and Engineering, University of North Carolina
at Chapel Hill, 170 Rosenau Hall, Campus Box #7400, 135 Dauer Drive, Chapel Hill, North Carolina 27599, United States
- College
of Arts and Sciences, Department of Chemistry, University of North Carolina at Chapel Hill, Campus Box #3290, 125 South Road, Chapel Hill, North Carolina 27599, United States
| | - Yue Zhang
- Department
of Atmospheric Sciences, Texas A&M University, Eller O&M Building, 1204, 3150
TAMU, 797 Lamar Street, College Station, Texas 77843, United States
| | - Sarah D. Brooks
- Department
of Atmospheric Sciences, Texas A&M University, Eller O&M Building, 1204, 3150
TAMU, 797 Lamar Street, College Station, Texas 77843, United States
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4
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Armeli G, Peters JH, Koop T. Machine-Learning-Based Prediction of the Glass Transition Temperature of Organic Compounds Using Experimental Data. ACS OMEGA 2023; 8:12298-12309. [PMID: 37033862 PMCID: PMC10077449 DOI: 10.1021/acsomega.2c08146] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/02/2023] [Accepted: 03/07/2023] [Indexed: 06/19/2023]
Abstract
Knowledge of the glass transition temperature of molecular compounds that occur in atmospheric aerosol particles is important for estimating their viscosity, as it directly influences the kinetics of chemical reactions and particle phase state. While there is a great diversity of organic compounds present in aerosol particles, for only a minor fraction of them experimental glass transition temperatures are known. Therefore, we have developed a machine learning model designed to predict the glass transition temperature of organic molecular compounds based on molecule-derived input variables. The extremely randomized trees (extra trees) procedure was chosen for this purpose. Two approaches using different sets of input variables were followed. The first one uses the number of selected functional groups present in the compound, while the second one generates descriptors from a SMILES (Simplified Molecular Input Line Entry System) string. Organic compounds containing carbon, hydrogen, oxygen, nitrogen, and halogen atoms are included. For improved results, both approaches can be combined with the melting temperature of the compound as an additional input variable. The results show that the predictions of both approaches show a similar mean absolute error of about 12-13 K, with the SMILES-based predictions performing slightly better. In general, the model shows good predictive power considering the diversity of the experimental input data. Furthermore, we also show that its performance exceeds that of previous parameterizations developed for this purpose and also performs better than existing machine learning models. In order to provide user-friendly versions of the model for applications, we have developed a web site where the model can be run by interested scientists via a web-based interface without prior technical knowledge. We also provide Python code of the model. Additionally, all experimental input data are provided in form of the Bielefeld Molecular Organic Glasses (BIMOG) database. We believe that this model is a powerful tool for many applications in atmospheric aerosol science and material science.
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5
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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. ENVIRONMENTAL SCIENCE & TECHNOLOGY 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] [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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6
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Groth R, Niazi S, Johnson GR, Ristovski Z. Nanomechanics and Morphology of Simulated Respiratory Particles. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:10879-10890. [PMID: 35852155 DOI: 10.1021/acs.est.2c01829] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/15/2023]
Abstract
The impact of respiratory particle composition on the equilibrium morphology and phase is not well understood. Furthermore, the effects of these different phases and morphologies on the viability of viruses embedded within these particles are equally unknown. Physiologically relevant respiratory fluid analogues were constructed, and their hygroscopic behavior was measured using an ensemble technique. A relationship between hygroscopicity and protein concentration was determined, providing additional validation to the high protein content of respiratory aerosol measured in prior works (>90%). It was found that the salt component of the respiratory particles could crystallize as a single crystal, multiple crystals, or would not crystallize at all. It was found that dried protein particles at indoor-relevant climatic conditions could exist separately in a glassy (∼77% of particles) or viscoelastic state (∼23% of particles). The phase state and morphology of respiratory particles may influence the viability of embedded pathogens. We recommend that pathogen research aiming to mimic the native composition of respiratory fluid should use a protein concentration of at least 90% by solute volume to improve the representativity of the pathogen's microenvironment.
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Affiliation(s)
- Robert Groth
- International Laboratory for Air Quality and Health (ILAQH), School of Earth and Atmospheric Sciences, Queensland University of Technology, Brisbane, QLD 4000, Australia
| | - Sadegh Niazi
- International Laboratory for Air Quality and Health (ILAQH), School of Earth and Atmospheric Sciences, Queensland University of Technology, Brisbane, QLD 4000, Australia
| | - Graham R Johnson
- International Laboratory for Air Quality and Health (ILAQH), School of Earth and Atmospheric Sciences, Queensland University of Technology, Brisbane, QLD 4000, Australia
| | - Zoran Ristovski
- International Laboratory for Air Quality and Health (ILAQH), School of Earth and Atmospheric Sciences, Queensland University of Technology, Brisbane, QLD 4000, Australia
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7
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O'Brien RE, Li Y, Kiland KJ, Katz EF, Or VW, Legaard E, Walhout EQ, Thrasher C, Grassian VH, DeCarlo PF, Bertram AK, Shiraiwa M. Emerging investigator series: chemical and physical properties of organic mixtures on indoor surfaces during HOMEChem. ENVIRONMENTAL SCIENCE. PROCESSES & IMPACTS 2021; 23:559-568. [PMID: 33870396 DOI: 10.1039/d1em00060h] [Citation(s) in RCA: 9] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
Organic films on indoor surfaces serve as a medium for reactions and for partitioning of semi-volatile organic compounds and thus play an important role in indoor chemistry. However, the chemical and physical properties of these films are poorly characterized. Here, we investigate the chemical composition of an organic film collected during the HOMEChem campaign, over three cumulative weeks in the kitchen, using both Fourier Transform Ion Cyclotron Resonance Mass Spectrometry (FT-ICR MS) and offline Aerosol Mass Spectrometry (AMS). We also characterize the viscosity of this film using a model based on molecular formulas as well as poke-flow measurements. We find that the film contains organic material similar to cooking organic aerosol (COA) measured during the campaign using on-line AMS. However, the average molecular formula observed using FT-ICR MS is ∼C50H90O11, which is larger and more oxidized than fresh COA. Solvent extracted film material is a low viscous semisolid, with a measured viscosity <104 Pa s. This is much lower than the viscosity model predicts, which is parametrized with atmospherically relevant organic molecules, but sensitivity tests demonstrate that including unsaturation can explain the differences. The presence of unsaturation is supported by reactions of film material with ozone. In contrast to the solvent extract, manually removed material appears to be highly viscous, highlighting the need for continued work understanding both viscosity measurements as well as parameterizations for modeled viscosity of indoor organic films.
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Affiliation(s)
- Rachel E O'Brien
- Department of Chemistry, William & Mary, Williamsburg, VA 23185, USA.
| | - Ying Li
- Department of Chemistry, University of California Irvine, Irvine, CA 92697, USA
| | - Kristian J Kiland
- Department of Chemistry, University of British Columbia, Vancouver, British Columbia V6T 1Z1, Canada
| | - Erin F Katz
- Department of Chemistry, Drexel University, Philadelphia, PA 19104, USA
| | - Victor W Or
- Department of Chemistry and Biochemistry, University of California San Diego, La Jolla, California 92093, USA
| | - Emily Legaard
- Department of Chemistry, William & Mary, Williamsburg, VA 23185, USA.
| | - Emma Q Walhout
- Department of Chemistry, William & Mary, Williamsburg, VA 23185, USA.
| | - Corey Thrasher
- Department of Chemistry, William & Mary, Williamsburg, VA 23185, USA.
| | - Vicki H Grassian
- Department of Chemistry and Biochemistry, University of California San Diego, La Jolla, California 92093, USA and Scripps Institution of Oceanography and Department of Nanoengineering, University of California San Diego, La Jolla, California 92093, USA
| | - Peter F DeCarlo
- Department of Environmental Health and Engineering, Johns Hopkins University, Baltimore, MD 21218, USA
| | - Allan K Bertram
- Department of Chemistry, University of British Columbia, Vancouver, British Columbia V6T 1Z1, Canada
| | - Manabu Shiraiwa
- Department of Chemistry, University of California Irvine, Irvine, CA 92697, USA
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8
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Cummings BE, Li Y, DeCarlo PF, Shiraiwa M, Waring MS. Indoor aerosol water content and phase state in U.S. residences: impacts of relative humidity, aerosol mass and composition, and mechanical system operation. ENVIRONMENTAL SCIENCE. PROCESSES & IMPACTS 2020; 22:2031-2057. [PMID: 33084679 DOI: 10.1039/d0em00122h] [Citation(s) in RCA: 12] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/11/2023]
Abstract
Hygroscopic particulate matter (PM) constituents promote uptake of aerosol water (AW), depending on relative humidity (RH), which can constrain qualities such as organic aerosol (OA) phase state and inorganic aerosol (IA) deliquescence and efflorescence. This work provides a first incorporation of AW predictions into residential indoor PM simulations. The indoor model, IMAGES, which simulates factored OA concentrations and thermodynamics using the 2D-volatility basis set, was expanded to predict speciated IA concentrations, AW with κ-Köhler theory of hygroscopic growth, and OA phase state with glass transition temperatures. Since RH is the largest driver of AW and varies with meteorology, simulations were conducted using a database of historical ambient weather and pollution records spanning the sixteen U.S. climate zones, facilitating assessment of seasonal and regional trends. Over this diverse simulation set, the residential indoor AW mass was ∼10 to 100 times smaller than dry PM mass. This relative AW amount indoors was about ∼10 times smaller than outdoors, since indoor-emitted aerosol is likely less hygroscopic. The indoor OA phase state was typically semisolid, suggesting kinetic limitations might inhibit thermodynamic OA partitioning equilibrium from being established indoors. Residences in hot and humid climates during the summertime may have liquid indoor OA, while amorphous solid indoor OA can exist in cold climates. Deliquescence and efflorescence of recirculated IA within HVAC systems during cooling or heating, respectively, was also modeled. Oftentimes, two IA populations with different histories existing as wet or dry aerosol were generated by HVAC operation depending on indoor and outdoor environmental conditions and the HVAC operating mode.
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9
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Kołodziejczyk A, Pyrcz P, Błaziak K, Pobudkowska A, Sarang K, Szmigielski R. Physicochemical Properties of Terebic Acid, MBTCA, Diaterpenylic Acid Acetate, and Pinanediol as Relevant α-Pinene Oxidation Products. ACS OMEGA 2020; 5:7919-7927. [PMID: 32309701 PMCID: PMC7160834 DOI: 10.1021/acsomega.9b04231] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/10/2019] [Accepted: 03/20/2020] [Indexed: 05/14/2023]
Abstract
The physicochemical properties and the synthesis of four α-pinene oxidation products, terebic acid, 3-methyl-1,2,3-butanetricarboxylic acid (MBTCA), diaterpenylic acid acetate (DTAA), and pinanediol, are presented in this study. The physicochemical properties encompass thermal properties, solubility in water, and dissociation constant (pK a) for the investigated compounds. It was found that terebic acid exhibits a relatively high melting temperature of 449.29 K, whereas pinanediol revealed a low melting temperature of 329.26 K. The solubility in water was determined with the dynamic method and the experimental results were correlated using three different mathematical models: Wilson, NRTL, and UNIQUAC equations. The results of the correlation indicate that the Wilson equation appears to work the best for terebic acid and pinanediol. The calculated standard deviation was for 3.79 for terebic acid and 1.25 for pinanediol. In contrast, UNIQUAC was the best mathematical model for DTAA and MBTCA. The calculated standard deviation was 0.57 for DTAA and 2.21 for MBTCA. The measured water solubility increased in the following order: pinanediol > DTAA ≥ MBTCA > terebic acid, which affects their multiphase aging chemistry in the atmosphere. Moreover, acidity constants (pK a) at 298, 303, and 308 K were determined for DTAA with the Bates-Schwarzenbach spectrophotometric method. The pK a values obtained at 298, 303, and 308 K were found to be 3.76, 3.85, and 3.88, respectively.
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Affiliation(s)
- Agata Kołodziejczyk
- Institute
of Physical Chemistry, Polish Academy of
Sciences, ul. Kasprzaka
44/52, 01-224 Warsaw, Poland
- E-mail: . Phone: +48 22 343 34 02
| | - Patryk Pyrcz
- Institute
of Physical Chemistry, Polish Academy of
Sciences, ul. Kasprzaka
44/52, 01-224 Warsaw, Poland
- Department
of Physical Chemistry, Faculty of Chemistry, Warsaw University of Technology, ul. Noakowskiego 3, 00-664 Warsaw, Poland
| | - Kacper Błaziak
- University
of Warsaw, Faculty of Chemistry, ul. Pasteura 1, 02-093 Warsaw, Poland
| | - Aneta Pobudkowska
- Department
of Physical Chemistry, Faculty of Chemistry, Warsaw University of Technology, ul. Noakowskiego 3, 00-664 Warsaw, Poland
| | - Kumar Sarang
- Institute
of Physical Chemistry, Polish Academy of
Sciences, ul. Kasprzaka
44/52, 01-224 Warsaw, Poland
| | - Rafał Szmigielski
- Institute
of Physical Chemistry, Polish Academy of
Sciences, ul. Kasprzaka
44/52, 01-224 Warsaw, Poland
- E-mail:
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10
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Zhang Y, Nichman L, Spencer P, Jung JI, Lee A, Heffernan BK, Gold A, Zhang Z, Chen Y, Canagaratna MR, Jayne JT, Worsnop DR, Onasch TB, Surratt JD, Chandler D, Davidovits P, Kolb CE. The Cooling Rate- and Volatility-Dependent Glass-Forming Properties of Organic Aerosols Measured by Broadband Dielectric Spectroscopy. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2019; 53:12366-12378. [PMID: 31490675 DOI: 10.1021/acs.est.9b03317] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/10/2023]
Abstract
Glass transitions of secondary organic aerosols (SOA) from liquid/semisolid to solid phase states have important implications for aerosol reactivity, growth, and cloud formation properties. In the present study, glass transition temperatures (Tg) of isoprene SOA components, including isoprene hydroxy hydroperoxide (ISOPOOH), isoprene-derived epoxydiols (IEPOX), 2-methyltetrols, and 2-methyltetrol sulfates, were measured at atmospherically relevant cooling rates (2-10 K/min) by thin film broadband dielectric spectroscopy. The results indicate that 2-methyltetrol sulfates have the highest glass transition temperature, while ISOPOOH has the lowest glass transition temperature. By varying the cooling rate of the same compound from 2 to 10 K/min, the Tg of these compounds increased by 4-5 K. This temperature difference leads to a height difference of 400-800 m in the atmosphere for the corresponding updraft induced cooling rates, assuming a hygroscopicity value (κ) of 0.1 and relative humidity less than 95%. The Tg of the organic compounds was found to be strongly correlated with volatility, and a semiempirical formula between glass transition temperatures and volatility was derived. The Gordon-Taylor equation was applied to calculate the effect of relative humidity (RH) and water content at five mixing ratios on the Tg of organic aerosols. The model shows that Tg could drop by 15-40 K as the RH changes from <5 to 90%, whereas the mixing ratio of water in the particle increases from 0 to 0.5. These results underscore the importance of chemical composition, updraft rates, and water content (RH) in determining the phase states and hygroscopic properties of organic particles.
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Affiliation(s)
- Yue Zhang
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
- Aerodyne Research Inc. , Billerica , Massachusetts 01821 , United States
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health , University of North Carolina at Chapel Hill , Chapel Hill , North Carolina 27599 , United States
| | - Leonid Nichman
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
| | - Peyton Spencer
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
| | - Jason I Jung
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
| | - Andrew Lee
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
| | - Brian K Heffernan
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
| | - Avram Gold
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health , University of North Carolina at Chapel Hill , Chapel Hill , North Carolina 27599 , United States
| | - Zhenfa Zhang
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health , University of North Carolina at Chapel Hill , Chapel Hill , North Carolina 27599 , United States
| | - Yuzhi Chen
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health , University of North Carolina at Chapel Hill , Chapel Hill , North Carolina 27599 , United States
| | | | - John T Jayne
- Aerodyne Research Inc. , Billerica , Massachusetts 01821 , United States
| | - Douglas R Worsnop
- Aerodyne Research Inc. , Billerica , Massachusetts 01821 , United States
| | - Timothy B Onasch
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
- Aerodyne Research Inc. , Billerica , Massachusetts 01821 , United States
| | - Jason D Surratt
- Department of Environmental Sciences and Engineering, Gillings School of Global Public Health , University of North Carolina at Chapel Hill , Chapel Hill , North Carolina 27599 , United States
| | - David Chandler
- Department of Chemistry , University of California, Berkeley , Berkeley , California 94720 , United States
| | - Paul Davidovits
- Department of Chemistry , Boston College , Chestnut Hill , Massachusetts 02459 , United States
| | - Charles E Kolb
- Aerodyne Research Inc. , Billerica , Massachusetts 01821 , United States
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11
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Zuth C, Vogel AL, Ockenfeld S, Huesmann R, Hoffmann T. Ultrahigh-Resolution Mass Spectrometry in Real Time: Atmospheric Pressure Chemical Ionization Orbitrap Mass Spectrometry of Atmospheric Organic Aerosol. Anal Chem 2018; 90:8816-8823. [DOI: 10.1021/acs.analchem.8b00671] [Citation(s) in RCA: 31] [Impact Index Per Article: 5.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/06/2023]
Affiliation(s)
- Christoph Zuth
- Institute of Inorganic Chemistry and Analytical Chemistry, Johannes Gutenberg-University, Mainz 55128, Germany
| | - Alexander L. Vogel
- Laboratory for Environmental Chemistry & Laboratory for Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland
| | - Sara Ockenfeld
- Institute of Inorganic Chemistry and Analytical Chemistry, Johannes Gutenberg-University, Mainz 55128, Germany
| | - Regina Huesmann
- Institute of Inorganic Chemistry and Analytical Chemistry, Johannes Gutenberg-University, Mainz 55128, Germany
| | - Thorsten Hoffmann
- Institute of Inorganic Chemistry and Analytical Chemistry, Johannes Gutenberg-University, Mainz 55128, Germany
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12
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Liu P, Li YJ, Wang Y, Bateman AP, Zhang Y, Gong Z, Bertram AK, Martin ST. Highly Viscous States Affect the Browning of Atmospheric Organic Particulate Matter. ACS CENTRAL SCIENCE 2018; 4. [PMID: 29532020 PMCID: PMC5832997 DOI: 10.1021/acscentsci.7b00452] [Citation(s) in RCA: 26] [Impact Index Per Article: 4.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/16/2023]
Abstract
Initially transparent organic particulate matter (PM) can become shades of light-absorbing brown via atmospheric particle-phase chemical reactions. The production of nitrogen-containing compounds is one important pathway for browning. Semisolid or solid physical states of organic PM might, however, have sufficiently slow diffusion of reactant molecules to inhibit browning reactions. Herein, organic PM of secondary organic material (SOM) derived from toluene, a common SOM precursor in anthropogenically affected environments, was exposed to ammonia at different values of relative humidity (RH). The production of light-absorbing organonitrogen imines from ammonia exposure, detected by mass spectrometry and ultraviolet-visible spectrophotometry, was kinetically inhibited for RH < 20% for exposure times of 6 min to 24 h. By comparison, from 20% to 60% RH organonitrogen production took place, implying ammonia uptake and reaction. Correspondingly, the absorption index k across 280 to 320 nm increased from 0.012 to 0.02, indicative of PM browning. The k value across 380 to 420 nm increased from 0.001 to 0.004. The observed RH-dependent behavior of ammonia uptake and browning was well captured by a model that considered the diffusivities of both the large organic molecules that made up the PM and the small reactant molecules taken up from the gas phase into the PM. Within the model, large-molecule diffusivity was calculated based on observed SOM viscosity and evaporation. Small-molecule diffusivity was represented by the water diffusivity measured by a quartz-crystal microbalance. The model showed that the browning reaction rates at RH < 60% could be controlled by the low diffusivity of the large organic molecules from the interior region of the particle to the reactive surface region. The results of this study have implications for accurate modeling of atmospheric brown carbon production and associated influences on energy balance.
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Affiliation(s)
- Pengfei Liu
- John A. Paulson School of Engineering and Applied
Sciences and Department
of Earth and
Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, United States
| | - Yong Jie Li
- John A. Paulson School of Engineering and Applied
Sciences and Department
of Earth and
Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, United States
- Department
of Civil and Environmental Engineering, Faculty of Science and Technology, University of Macau, Macau, China
| | - Yan Wang
- John A. Paulson School of Engineering and Applied
Sciences and Department
of Earth and
Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, United States
- T. H.
Chan School of Public Health, Harvard University, Boston, Massachusetts 02115, United States
| | - Adam P. Bateman
- John A. Paulson School of Engineering and Applied
Sciences and Department
of Earth and
Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, United States
| | - Yue Zhang
- John A. Paulson School of Engineering and Applied
Sciences and Department
of Earth and
Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, United States
- Aerodyne
Research Inc., Billerica, Massachusetts 01821, United States
| | - Zhaoheng Gong
- John A. Paulson School of Engineering and Applied
Sciences and Department
of Earth and
Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, United States
| | - Allan K. Bertram
- Department
of Chemistry, University of British Columbia, Vancouver, British Columbia, Canada
| | - Scot T. Martin
- John A. Paulson School of Engineering and Applied
Sciences and Department
of Earth and
Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, United States
- E-mail:
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13
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Global distribution of particle phase state in atmospheric secondary organic aerosols. Nat Commun 2017; 8:15002. [PMID: 28429776 PMCID: PMC5413943 DOI: 10.1038/ncomms15002] [Citation(s) in RCA: 105] [Impact Index Per Article: 15.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/30/2016] [Accepted: 02/20/2017] [Indexed: 12/26/2022] Open
Abstract
Secondary organic aerosols (SOA) are a large source of uncertainty in our current understanding of climate change and air pollution. The phase state of SOA is important for quantifying their effects on climate and air quality, but its global distribution is poorly characterized. We developed a method to estimate glass transition temperatures based on the molar mass and molecular O:C ratio of SOA components, and we used the global chemistry climate model EMAC with the organic aerosol module ORACLE to predict the phase state of atmospheric SOA. For the planetary boundary layer, global simulations indicate that SOA are mostly liquid in tropical and polar air with high relative humidity, semi-solid in the mid-latitudes and solid over dry lands. We find that in the middle and upper troposphere SOA should be mostly in a glassy solid phase state. Thus, slow diffusion of water, oxidants and organic molecules could kinetically limit gas–particle interactions of SOA in the free and upper troposphere, promote ice nucleation and facilitate long-range transport of reactive and toxic organic pollutants embedded in SOA. Secondary organic aerosols (SOA) are important for climate and aerosol quality, but the phase state is unclear. Here, the authors show that SOA is liquid in tropical and polar air, semi-solid in the mid-latitudes, solid over dry lands and in a glassy solid phase state in the middle and upper troposphere.
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14
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Rothfuss NE, Petters MD. Influence of Functional Groups on the Viscosity of Organic Aerosol. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2017; 51:271-279. [PMID: 27990815 DOI: 10.1021/acs.est.6b04478] [Citation(s) in RCA: 34] [Impact Index Per Article: 4.9] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/06/2023]
Abstract
Organic aerosols can exist in highly viscous or glassy phase states. A viscosity database for organic compounds with atmospherically relevant functional groups is compiled and analyzed to quantify the influence of number and location of functional groups on viscosity. For weakly functionalized compounds the trend in viscosity sensitivity to functional group addition is carboxylic acid (COOH) ≈ hydroxyl (OH) > nitrate (ONO2) > carbonyl (CO) ≈ ester (COO) > methylene (CH2). Sensitivities to group addition increase with greater levels of prior functionalization and decreasing temperature. For carboxylic acids a sharp increase in sensitivity is likely present already at the second addition at room temperature. Ring structures increase viscosity relative to linear structures. Sensitivities are correlated with analogously derived sensitivities of vapor pressure reduction. This may be exploited in the future to predict viscosity in numerical models by piggybacking on schemes that track the evolution of organic aerosol volatility with age.
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Affiliation(s)
- Nicholas E Rothfuss
- Department of Marine Earth and Atmospheric Sciences, North Carolina State University , Raleigh, North Carolina 27695, United States
| | - Markus D Petters
- Department of Marine Earth and Atmospheric Sciences, North Carolina State University , Raleigh, North Carolina 27695, United States
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15
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Enami S, Sakamoto Y. OH-Radical Oxidation of Surface-Active cis-Pinonic Acid at the Air–Water Interface. J Phys Chem A 2016; 120:3578-87. [DOI: 10.1021/acs.jpca.6b01261] [Citation(s) in RCA: 63] [Impact Index Per Article: 7.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
- Shinichi Enami
- The
Hakubi Center for Advanced Research, Kyoto University, Kyoto 606-8302, Japan
- Research
Institute for Sustainable Humanosphere, Kyoto University, Uji 611-0011, Japan
- PRESTO, Japan Science and Technology Agency, Kawaguchi 332-0012, Japan
| | - Yosuke Sakamoto
- Graduate
School of Human and Environmental Studies, Kyoto University, Kyoto, 606-8316, Japan
- Graduate
School of Global Environmental Studies, Kyoto University, Kyoto, 606-8501, Japan
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16
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Pöschl U, Shiraiwa M. Multiphase chemistry at the atmosphere-biosphere interface influencing climate and public health in the anthropocene. Chem Rev 2015; 115:4440-75. [PMID: 25856774 DOI: 10.1021/cr500487s] [Citation(s) in RCA: 214] [Impact Index Per Article: 23.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/07/2023]
Affiliation(s)
- Ulrich Pöschl
- Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - Manabu Shiraiwa
- Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
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17
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Nozière B, Kalberer M, Claeys M, Allan J, D'Anna B, Decesari S, Finessi E, Glasius M, Grgić I, Hamilton JF, Hoffmann T, Iinuma Y, Jaoui M, Kahnt A, Kampf CJ, Kourtchev I, Maenhaut W, Marsden N, Saarikoski S, Schnelle-Kreis J, Surratt JD, Szidat S, Szmigielski R, Wisthaler A. The molecular identification of organic compounds in the atmosphere: state of the art and challenges. Chem Rev 2015; 115:3919-83. [PMID: 25647604 DOI: 10.1021/cr5003485] [Citation(s) in RCA: 203] [Impact Index Per Article: 22.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/13/2022]
Affiliation(s)
- Barbara Nozière
- †Ircelyon/CNRS and Université Lyon 1, 69626 Villeurbanne Cedex, France
| | | | | | | | - Barbara D'Anna
- †Ircelyon/CNRS and Université Lyon 1, 69626 Villeurbanne Cedex, France
| | | | | | | | - Irena Grgić
- ○National Institute of Chemistry, 1000 Ljubljana, Slovenia
| | | | | | - Yoshiteru Iinuma
- ¶Leibniz-Institut für Troposphärenforschung, 04318 Leipzig, Germany
| | | | | | | | - Ivan Kourtchev
- ‡University of Cambridge, Cambridge CB2 1EW, United Kingdom
| | - Willy Maenhaut
- §University of Antwerp, 2000 Antwerp, Belgium.,□Ghent University, 9000 Gent, Belgium
| | | | | | | | - Jason D Surratt
- ▼University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599, United States
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18
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Dette HP, Koop T. Glass Formation Processes in Mixed Inorganic/Organic Aerosol Particles. J Phys Chem A 2014; 119:4552-61. [DOI: 10.1021/jp5106967] [Citation(s) in RCA: 32] [Impact Index Per Article: 3.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/07/2023]
Affiliation(s)
- Hans P. Dette
- Faculty of Chemistry and
Center for Molecular Materials, Bielefeld University, Universitätsstraße
25, D-33615 Bielefeld, Germany
| | - Thomas Koop
- Faculty of Chemistry and
Center for Molecular Materials, Bielefeld University, Universitätsstraße
25, D-33615 Bielefeld, Germany
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19
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Wang B, O’Brien RE, Kelly ST, Shilling JE, Moffet RC, Gilles MK, Laskin A. Reactivity of Liquid and Semisolid Secondary Organic Carbon with Chloride and Nitrate in Atmospheric Aerosols. J Phys Chem A 2014; 119:4498-508. [DOI: 10.1021/jp510336q] [Citation(s) in RCA: 62] [Impact Index Per Article: 6.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/06/2023]
Affiliation(s)
- Bingbing Wang
- Environmental
Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354 United States
| | - Rachel E. O’Brien
- Chemical
Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States
- Department
of Chemistry, University of the Pacific, Stockton, California 95211, United States
| | - Stephen T. Kelly
- Chemical
Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States
| | - John E. Shilling
- Atmospheric
Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, Washington 99354, United States
| | - Ryan C. Moffet
- Department
of Chemistry, University of the Pacific, Stockton, California 95211, United States
| | - Mary K. Gilles
- Chemical
Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States
| | - Alexander Laskin
- Environmental
Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354 United States
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