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Wong C, Vuong J, Nizkorodov SA. Biogenic and Anthropogenic Secondary Organic Aerosols Become Fluorescent after Highly Acidic Aging. J Phys Chem A 2024; 128:7657-7668. [PMID: 39213482 PMCID: PMC11403668 DOI: 10.1021/acs.jpca.4c04287] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 09/04/2024]
Abstract
Primary biological aerosol particles (PBAPs) and secondary organic aerosol (SOA) both contain organic compounds that share similar chemical and optical properties. Fluorescence is often used to characterize PBAPs; however, this may be hindered due to interferences from fluorophores in SOA. Despite extensive efforts to understand the aging of SOA under elevated particle acidity conditions, little is known about how these processes affect the fluorescence of SOA and thereby their interference with the measurements of PBAPs. The objective of this study is to investigate the fluorescence of SOA and understand the influence of acidity on the optical properties of organic aerosols and potential interference for the analysis of bioaerosols. The SOA was generated by O3- or OH-initiated oxidation of d-limonene or α-pinene, as well as by OH-initiated oxidation of toluene or xylene. The SOA compounds were then aged by exposure to varying concentrations of aqueous H2SO4 for 2 days. Absorption and fluorescence spectrophotometry were used to examine the changes in the optical properties before and after aging. The key observation was the appearance of strongly light-absorbing and fluorescent compounds at pH = ∼-1, suggesting that acidity is a major driver of SOA aging. The aged SOA from biogenic precursors (d-limonene and α-pinene) resulted in stronger fluorescence than the aged SOA from toluene and xylene. The absorption spectra of the aged SOA changed drastically in shape upon dilution, whereas the shapes of the fluorescence spectra remained the same, suggesting that the fluorophores and chromophores in SOA are separate sets of species. The fluorescence spectra of aged SOA overlapped with the fluorescence spectra of PBAPs, suggesting that SOA exposed to highly acidic conditions can be confused with PBAPs detected by fluorescence-based methods. These processes are likely to play a role in the atmospheric regions where high concentrations of H2SO4 persist, such as the upper troposphere and lower stratosphere.
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Affiliation(s)
- Cynthia Wong
- Department of Chemistry, University of California, Irvine, Irvine, California 92697-2025, United States
| | - Jett Vuong
- Department of Chemistry, University of California, Irvine, Irvine, California 92697-2025, United States
| | - Sergey A Nizkorodov
- Department of Chemistry, University of California, Irvine, Irvine, California 92697-2025, United States
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2
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Wong C, Pazienza JE, Rychnovsky SD, Nizkorodov SA. Formation of Chromophores from cis-Pinonaldehyde Aged in Highly Acidic Conditions. J Am Chem Soc 2024; 146:11702-11710. [PMID: 38640258 PMCID: PMC11066867 DOI: 10.1021/jacs.3c14177] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/14/2023] [Revised: 03/28/2024] [Accepted: 03/29/2024] [Indexed: 04/21/2024]
Abstract
Sulfuric acid in the atmosphere can participate in acid-catalyzed and acid-driven reactions, including those within secondary organic aerosols (SOA). Previous studies have observed enhanced absorption at visible wavelengths and significant changes in the chemical composition when SOA was exposed to sulfuric acid. However, the specific chromophores responsible for these changes could not be identified. The goals of this study are to identify the chromophores and determine the mechanism of browning in highly acidified α-pinene SOA by following the behavior of specific common α-pinene oxidation products, namely, cis-pinonic acid and cis-pinonaldehyde, when they are exposed to highly acidic conditions. The products of these reactions were analyzed with ultra-performance liquid chromatography coupled with photodiode array spectrophotometry and high-resolution mass spectrometry, UV-vis spectrophotometry, and nuclear magnetic resonance spectroscopy. cis-Pinonic acid (2) was found to form homoterpenyl methyl ketone (4), which does not absorb visible radiation, while cis-pinonaldehyde (3) formed weakly absorbing 1-(4-(propan-2-ylidene)cyclopent-1-en-1-yl)ethan-1-one (5) and 1-(4-isopropylcyclopenta-1,3-dien-1-yl)ethan-1-one (6) via an acid-catalyzed aldol condensation. This chemistry could be relevant for environments characterized by high sulfuric acid concentrations, for example, during the transport of organic compounds from the lower to the upper atmosphere by fast updrafts.
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Affiliation(s)
| | | | - Scott D. Rychnovsky
- Department of Chemistry, University of California, Irvine, Irvine, California 92697-2025, United
States
| | - Sergey A. Nizkorodov
- Department of Chemistry, University of California, Irvine, Irvine, California 92697-2025, United
States
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3
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Benoit R, Vernier H, Vernier JP, Joly L, Dumelié N, Wienhold FG, Crevoisier C, Delpeux S, Bernard F, Dagaut P, Berthet G. The first balloon-borne sample analysis of atmospheric carbonaceous components reveals new insights into formation processes. CHEMOSPHERE 2023; 326:138421. [PMID: 36935062 DOI: 10.1016/j.chemosphere.2023.138421] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/09/2022] [Revised: 03/08/2023] [Accepted: 03/14/2023] [Indexed: 06/18/2023]
Abstract
Atmospheric aerosol optical, physical, and chemical properties play a fundamental role in the Earth's climate system. A better understanding of the processes involved in their formation, evolution, and interaction with radiation and the water cycle is critical. We report the analysis of atmospheric molecules/particles collected with a new sampling system that flew under regular weather balloons for the first time. The flight took place on January 18, 2022 from Reims (France). The samples were subsequently analyzed by high-resolution mass spectrometry (Orbitrap) to specifically infer hundreds of organic components present in 4 different layers from the troposphere to the stratosphere (up to 20 km). Additional measurements of O3, CO, and aerosol concentrations a few hours before this flight took place to contextualize the sampling. After separating common species found on each filter that might be common to atmospheric layers or residuals for contaminations, we found that each sample yields significant differences in the number and size of organic species detected that should reflect the unique composition of atmospheric layers. While tropospheric samples yield significantly oxidized and saturated components, with carbon numbers below 30 that might be explained by complex organics chemistry from local and distant source emissions, the upper tropospheric and stratospheric samples were associated with increased carbon numbers (C > 30), with a significantly reduced unsaturation number for the stratosphere, that might be induced by strong UV radiations. The multimodal distributions of carbon numbers in chemical formulas observed between 15 and 20 km suggest that oligomerization and growth of organic molecules may take place in aged air masses of tropical origin that are known to carry organic compounds even several km above the tropopause where their lifetime significantly increases. In addition, the presence of organics may also reflect the extended influence of wildfires smoke injected during the spring and summer in the NH hemisphere before the in situ observations and their long-lifetime in the upper troposphere and stratosphere.
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Affiliation(s)
| | - Hazel Vernier
- LPC2E, UMR 7328 CNRS-Université d'Orléans-CNES, Orléans, France
| | - Jean-Paul Vernier
- NASA Langley Research Center, Hampton, VA, USA; National Institute of Aerospace, Hampton, VA, USA
| | - Lilian Joly
- GSMA, UMR 7331 CNRS-Université de Reims Champagne-Ardenne, Reims, France
| | - Nicolas Dumelié
- GSMA, UMR 7331 CNRS-Université de Reims Champagne-Ardenne, Reims, France
| | | | - Cyril Crevoisier
- Laboratoire de Météorologie Dynamique (LMD/IPSL), CNRS, Ecole Polytechnique, Université Paris-Saclay, Palaiseau, France
| | | | | | | | - Gwenaël Berthet
- LPC2E, UMR 7328 CNRS-Université d'Orléans-CNES, Orléans, France
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4
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Solomon S, Stone K, Yu P, Murphy DM, Kinnison D, Ravishankara AR, Wang P. Chlorine activation and enhanced ozone depletion induced by wildfire aerosol. Nature 2023; 615:259-264. [PMID: 36890371 DOI: 10.1038/s41586-022-05683-0] [Citation(s) in RCA: 5] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/09/2022] [Accepted: 12/22/2022] [Indexed: 03/10/2023]
Abstract
Remarkable perturbations in the stratospheric abundances of chlorine species and ozone were observed over Southern Hemisphere mid-latitudes following the 2020 Australian wildfires1,2. These changes in atmospheric chemical composition suggest that wildfire aerosols affect stratospheric chlorine and ozone depletion chemistry. Here we propose that wildfire aerosol containing a mixture of oxidized organics and sulfate3-7 increases hydrochloric acid solubility8-11 and associated heterogeneous reaction rates, activating reactive chlorine species and enhancing ozone loss rates at relatively warm stratospheric temperatures. We test our hypothesis by comparing atmospheric observations to model simulations that include the proposed mechanism. Modelled changes in 2020 hydrochloric acid, chlorine nitrate and hypochlorous acid abundances are in good agreement with observations1,2. Our results indicate that wildfire aerosol chemistry, although not accounting for the record duration of the 2020 Antarctic ozone hole, does yield an increase in its area and a 3-5% depletion of southern mid-latitude total column ozone. These findings increase concern2,12,13 that more frequent and intense wildfires could delay ozone recovery in a warming world.
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Affiliation(s)
- Susan Solomon
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA.
| | - Kane Stone
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA.
| | - Pengfei Yu
- Institute for Environmental and Climate Research, Jinan University, Guangzhou, China
| | - D M Murphy
- NOAA Chemical Sciences Laboratory, Boulder, CO, USA
| | - Doug Kinnison
- Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
| | - A R Ravishankara
- Department of Chemistry, Colorado State University, Fort Collins, CO, USA.,Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA
| | - Peidong Wang
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA
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5
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Wong C, Liu S, Nizkorodov SA. Highly Acidic Conditions Drastically Alter the Chemical Composition and Absorption Coefficient of α-Pinene Secondary Organic Aerosol. ACS EARTH & SPACE CHEMISTRY 2022; 6:2983-2994. [PMID: 36561193 PMCID: PMC9762236 DOI: 10.1021/acsearthspacechem.2c00249] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 08/14/2022] [Revised: 11/08/2022] [Accepted: 11/09/2022] [Indexed: 06/17/2023]
Abstract
Secondary organic aerosols (SOA), formed through the gas-phase oxidation of volatile organic compounds (VOCs), can reside in the atmosphere for many days. The formation of SOA takes place rapidly within hours after VOC emissions, but SOA can undergo much slower physical and chemical processes throughout their lifetime in the atmosphere. The acidity of atmospheric aerosols spans a wide range, with the most acidic particles having negative pH values, which can promote acid-catalyzed reactions. The goal of this work is to elucidate poorly understood mechanisms and rates of acid-catalyzed aging of mixtures of representative SOA compounds. SOA were generated by the ozonolysis of α-pinene in a continuous flow reactor and then collected using a foil substrate. SOA samples were extracted and aged by exposure to varying concentrations of aqueous H2SO4 for 1-2 days. Chemical analysis of fresh and aged samples was conducted using ultra-performance liquid chromatography coupled with photodiode array spectrophotomety and high-resolution mass spectrometry. In addition, UV-vis spectrophotometry and fluorescence spectrophotometry were used to examine the changes in optical properties before and after aging. We observed that SOA that aged in moderately acidic conditions (pH from 0 to 4) experienced small changes in composition, while SOA that aged in a highly acidic environment (pH from -1 to 0) experienced more dramatic changes in composition, including the formation of compounds containing sulfur. Additionally, at highly acidic conditions, light-absorbing and fluorescent compounds appeared, but their identities could not be ascertained due to their small relative abundance. This study shows that acidity is a major driver of SOA aging, resulting in a large change in the chemical composition and optical properties of aerosols in regions where high concentrations of H2SO4 persist, such as upper troposphere and lower stratosphere.
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6
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Stratospheric Chemical Lifetime of Aviation Fuel Incomplete Combustion Products. ATMOSPHERE 2022. [DOI: 10.3390/atmos13081209] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
The stratosphere contains haze rich in sulfuric acid, which plays a significant role in stratospheric chemistry and in global climate. Commercial aircraft deposit significant amounts of incomplete combustion products into the lower stratosphere. We have studied the stability of these incomplete combustion products to reaction with sulfuric acid, using a predictive model based on experimental reaction kinetics. We demonstrate that sulfuric acid chemistry is likely to be a significant component of the chemistry of organics in the stratosphere. We find that at least 25 of the 40 known incomplete combustion products from aviation fuel have lifetimes to reaction with aerosol sulfuric acid of at least months. We estimate that ~109 kg of long-lived products could be deposited per year in the lower stratosphere. We suggest that the high molecular weight organic compounds formed as incomplete combustion products of commercial long-haul aviation could play a significant role in the stratosphere.
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Wang F, Yu H, Wang Z, Liang W, Shi G, Gao J, Li M, Feng Y. Review of online source apportionment research based on observation for ambient particulate matter. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 762:144095. [PMID: 33360453 DOI: 10.1016/j.scitotenv.2020.144095] [Citation(s) in RCA: 15] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/29/2020] [Revised: 11/13/2020] [Accepted: 11/20/2020] [Indexed: 06/12/2023]
Abstract
Particulate matter source apportionment (SA) is the basis and premise for preventing and controlling haze pollution scientifically and effectively. Traditional offline SA methods lack the capability of handling the rapid changing pollution sources during heavy air pollution periods. With the development of multiple online observation techniques, online SA of particulate matter can now be realized with high temporal resolution, stable and reliable continuous observation data on particle compositions. Here, we start with a summary of online measuring instruments for monitoring particulate matters that contains both online mass concentration (online MC) measurement, and online mass spectrometric (online MS) techniques. The former technique collects ambient particulate matter onto filter membrane and measures the concentrations of chemical components in the particulate matter subsequently. The latter technique could be further divided into two categories: bulk measurement and single particle measurement. Aerosol Mass Spectrometers (AMS) could provide mass spectral information of chemical components of non-refractory aerosols, especially organic aerosols. While the emergence of single-particle aerosol mass spectrometer (SPAMS) technology can provide large number of high time resolution data for online source resolution. This is closely followed by an overview of the methods and results of SA. However, online instruments are still facing challenges, such as abnormal or missing measurements, that could impact the accuracy of online dataset. Machine leaning algorithm are suited for processing the large amount of online observation data, which could be further considered. In addition, the key research challenges and future directions are presented including the integration of online dataset from different online instruments, the ensemble-trained source apportionment approach, and the quantification of source-category-specific human health risk based on online instrumentation and SA methods.
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Affiliation(s)
- Feng Wang
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Tianjin Key Laboratory of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin 300350, China
| | - Haofei Yu
- Department of Civil, Environmental, and Construction Engineering, University of Central Florida, Orlando, FL, USA
| | - Zhenyu Wang
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Tianjin Key Laboratory of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin 300350, China
| | - Weiqing Liang
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Tianjin Key Laboratory of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin 300350, China
| | - Guoliang Shi
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Tianjin Key Laboratory of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin 300350, China.
| | - Jian Gao
- State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 10084, China.
| | - Mei Li
- Institute of Mass Spectrometry and Atmospheric Environment, Guangdong Provincial Engineering Research Center for on-line source apportionment system of air pollution Jinan University, Guangzhou 510632, China; Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou 510632, China.
| | - Yinchang Feng
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Tianjin Key Laboratory of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin 300350, China
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8
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Baumgartner M, Weigel R, Harvey AH, Plöger F, Achatz U, Spichtinger P. Reappraising the appropriate calculation of a common meteorological quantity: Potential Temperature. ATMOSPHERIC CHEMISTRY AND PHYSICS 2020; 20:10.5194/acp-20-15585-2020. [PMID: 34093695 PMCID: PMC8174307 DOI: 10.5194/acp-20-15585-2020] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
The potential temperature is a widely used quantity in atmospheric science since it is conserved for dry air's adiabatic changes of state. Its definition involves the specific heat capacity of dry air, which is traditionally assumed as constant. However, the literature provides different values of this allegedly constant parameter, which are reviewed and discussed in this study. Furthermore, we derive the potential temperature for a temperature-dependent parameterisation of the specific heat capacity of dry air, thus providing a new reference potential temperature with a more rigorous basis. This new reference shows different values and vertical gradients, in particular in the stratosphere and above, compared to the potential temperature that assumes constant heat capacity. The application of the new reference potential temperature is discussed for computations of the Brunt-Väisälä frequency, Ertel's potential vorticity, diabatic heating rates, and for the vertical sorting of observational data.
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Affiliation(s)
- Manuel Baumgartner
- Zentrum für Datenverarbeitung, Johannes Gutenberg University Mainz, Germany
- Institute for Atmospheric Physics, Johannes Gutenberg University Mainz, Germany
| | - Ralf Weigel
- Institute for Atmospheric Physics, Johannes Gutenberg University Mainz, Germany
| | - Allan H. Harvey
- Applied Chemicals and Materials Division, National Institute of Standards and Technology, Boulder, CO, USA
| | - Felix Plöger
- Forschungszentrum Jülich GmbH, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
- Institute for Atmospheric and Environmental Research, University of Wuppertal, Wuppertal, Germany
| | - Ulrich Achatz
- Institut für Atmosphäre und Umwelt, Goethe-Universität Frankfurt, Frankfurt am Main, Germany
| | - Peter Spichtinger
- Institute for Atmospheric Physics, Johannes Gutenberg University Mainz, Germany
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9
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Origins and Spatial Distribution of Non-Pure Sulfate Particles (NSPs) in the Stratosphere Detected by the Balloon-Borne Light Optical Aerosols Counter (LOAC). ATMOSPHERE 2020. [DOI: 10.3390/atmos11101031] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
While water and sulfuric acid droplets are the main component of stratospheric aerosols, measurements performed for about 30 years have shown that non-sulfate particles (NSPs) are also present. Such particles, released from the Earth mainly through volcanic eruptions, pollution or biomass burning, or coming from space, present a wide variety of compositions, sizes, and shapes. To better understand the origin of NSPs, we have performed measurements with the Light Optical Aerosol Counter (LOAC) during 151 flights under weather balloons in the 2013–2019 period reaching altitudes up to 35 km. Coupled with previous counting measurements conducted over the 2004–2011 period, the LOAC measurements indicate the presence of stratospheric layers of enhanced concentrations associated with NSPs, with a bimodal vertical repartition ranging between 17 and 30 km altitude. Such enhancements are not correlated with permanent meteor shower events. They may be linked to dynamical and photophoretic effects lifting and sustaining particles coming from the Earth. Besides, large particles, up to several tens of μm, were detected and present decreasing concentrations with increasing altitudes. All these particles can originate from Earth but also from meteoroid disintegrations and from the interplanetary dust cloud and comets.
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10
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Sandvik OS, Friberg J, Martinsson BG, van Velthoven PFJ, Hermann M, Zahn A. Intercomparison of in-situ aircraft and satellite aerosol measurements in the stratosphere. Sci Rep 2019; 9:15576. [PMID: 31666595 PMCID: PMC6821816 DOI: 10.1038/s41598-019-52089-6] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/03/2018] [Accepted: 10/10/2019] [Indexed: 11/18/2022] Open
Abstract
Aerosol composition and optical scattering from particles in the lowermost stratosphere (LMS) have been studied by comparing in-situ aerosol samples from the IAGOS-CARIBIC passenger aircraft with vertical profiles of aerosol backscattering obtained from the CALIOP lidar aboard the CALIPSO satellite. Concentrations of the dominating fractions of the stratospheric aerosol, being sulphur and carbon, have been obtained from post-flight analysis of IAGOS-CARIBIC aerosol samples. This information together with literature data on black carbon concentrations were used to calculate the aerosol backscattering which subsequently is compared with measurements by CALIOP. Vertical optical profiles were taken in an altitude range of several kilometres from and above the northern hemispheric extratropical tropopause for the years 2006-2014. We find that the two vastly different measurement platforms yield different aerosol backscattering, especially close to the tropopause where the influence from tropospheric aerosol is strong. The best agreement is found when the LMS is affected by volcanism, i.e., at elevated aerosol loadings. At background conditions, best agreement is obtained some distance (>2 km) above the tropopause in winter and spring, i.e., at likewise elevated aerosol loadings from subsiding aerosol-rich stratospheric air. This is to our knowledge the first time the CALIPSO lidar measurements have been compared to in-situ long-term aerosol measurements.
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Affiliation(s)
| | - Johan Friberg
- Division of Nuclear Physics, Lund University, Lund, Sweden
| | | | | | - Markus Hermann
- Leibniz Institute for Tropospheric Research, Leipzig, Germany
| | - Andreas Zahn
- Institute of Meteorology and Climate Research, Institute of Technology, Karlsruhe, Germany
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11
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Chen Y, Xu L, Humphry T, Hettiyadura APS, Ovadnevaite J, Huang S, Poulain L, Schroder JC, Campuzano-Jost P, Jimenez JL, Herrmann H, O'Dowd C, Stone EA, Ng NL. Response of the Aerodyne Aerosol Mass Spectrometer to Inorganic Sulfates and Organosulfur Compounds: Applications in Field and Laboratory Measurements. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2019; 53:5176-5186. [PMID: 30939000 DOI: 10.1021/acs.est.9b00884] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/05/2023]
Abstract
Organosulfur compounds are important components of secondary organic aerosols (SOA). While the Aerodyne high-resolution time-of-flight aerosol mass spectrometer (AMS) has been extensively used in aerosol studies, the response of the AMS to organosulfur compounds is not well-understood. Here, we investigated the fragmentation patterns of organosulfurs and inorganic sulfates in the AMS, developed a method to deconvolve total sulfate into components of inorganic and organic origins, and applied this method in both laboratory and field measurements. Apportionment results from laboratory isoprene photooxidation experiment showed that with inorganic sulfate seed, sulfate functionality of organic origins can contribute ∼7% of SOA mass at peak growth. Results from measurements in the Southeastern U.S. showed that 4% of measured sulfate is from organosulfur compounds. Methanesulfonic acid was estimated for measurements in the coastal and remote marine boundary layer. We explored the application of this method to unit mass-resolution data, where it performed less well due to interferences. Our apportionment results demonstrate that organosulfur compounds could be a non-negligible source of sulfate fragments in AMS laboratory and field data sets. A reevaluation of previous AMS measurements over the full range of atmospheric conditions using this method could provide a global estimate/constraint on the contribution of organosulfur compounds.
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Affiliation(s)
- Yunle Chen
- School of Earth and Atmospheric Sciences , Georgia Institute of Technology , Atlanta , Georgia 30332 , United States
| | - Lu Xu
- School of Chemical and Biomolecular Engineering , Georgia Institute of Technology , Atlanta , Georgia 30332 , United States
- Now at Division of Geological and Planetary Sciences , California Institute of Technology , Pasadena , California 91125 , United States
| | - Tim Humphry
- Department of Chemistry , Truman State University , Kirksville , Missouri 63501 , United States
| | | | - Jurgita Ovadnevaite
- School of Physics and Centre for Climate and Air Pollution Studies, Ryan Institute , National University of Ireland Galway , Galway H91 TK33 , Ireland
| | - Shan Huang
- Now at Institute for Environmental and Climate Research , Jinan University , Guangzhou , Guangdong 511443 , China
- Leibniz Institute for Tropospheric Research , Leipzig , Sachsen 04318 , Germany
| | - Laurent Poulain
- Leibniz Institute for Tropospheric Research , Leipzig , Sachsen 04318 , Germany
| | - Jason C Schroder
- Department of Chemistry , University of Colorado , Boulder , Colorado 80309 , United States
- Cooperative Institute for Research in the Environmental Sciences (CIRES) , University of Colorado , Boulder , Colorado 80309 , United States
| | - Pedro Campuzano-Jost
- Department of Chemistry , University of Colorado , Boulder , Colorado 80309 , United States
- Cooperative Institute for Research in the Environmental Sciences (CIRES) , University of Colorado , Boulder , Colorado 80309 , United States
| | - Jose L Jimenez
- Department of Chemistry , University of Colorado , Boulder , Colorado 80309 , United States
- Cooperative Institute for Research in the Environmental Sciences (CIRES) , University of Colorado , Boulder , Colorado 80309 , United States
| | - Hartmut Herrmann
- Leibniz Institute for Tropospheric Research , Leipzig , Sachsen 04318 , Germany
| | - Colin O'Dowd
- School of Physics and Centre for Climate and Air Pollution Studies, Ryan Institute , National University of Ireland Galway , Galway H91 TK33 , Ireland
| | - Elizabeth A Stone
- Department of Chemistry , University of Iowa , Iowa City , Iowa 52242 , United States
| | - Nga Lee Ng
- School of Earth and Atmospheric Sciences , Georgia Institute of Technology , Atlanta , Georgia 30332 , United States
- School of Chemical and Biomolecular Engineering , Georgia Institute of Technology , Atlanta , Georgia 30332 , United States
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12
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Kroll JH, Lim CY, Kessler SH, Wilson KR. Heterogeneous Oxidation of Atmospheric Organic Aerosol: Kinetics of Changes to the Amount and Oxidation State of Particle-Phase Organic Carbon. J Phys Chem A 2015; 119:10767-83. [PMID: 26381466 DOI: 10.1021/acs.jpca.5b06946] [Citation(s) in RCA: 90] [Impact Index Per Article: 10.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Abstract
Atmospheric oxidation reactions are known to affect the chemical composition of organic aerosol (OA) particles over timescales of several days, but the details of such oxidative aging reactions are poorly understood. In this study we examine the rates and products of a key class of aging reaction, the heterogeneous oxidation of particle-phase organic species by the gas-phase hydroxyl radical (OH). We compile and reanalyze a number of previous studies from our laboratories involving the oxidation of single-component organic particles. All kinetic and product data are described on a common basis, enabling a straightforward comparison among different chemical systems and experimental conditions. Oxidation chemistry is described in terms of changes to key ensemble properties of the OA, rather than to its detailed molecular composition, focusing on two quantities in particular, the amount and the oxidation state of the particle-phase carbon. Heterogeneous oxidation increases the oxidation state of particulate carbon, with the rate of increase determined by the detailed chemical mechanism. At the same time, the amount of particle-phase carbon decreases with oxidation, due to fragmentation (C-C scission) reactions that form small, volatile products that escape to the gas phase. In contrast to the oxidation state increase, the rate of carbon loss is nearly uniform among most systems studied. Extrapolation of these results to atmospheric conditions indicates that heterogeneous oxidation can have a substantial effect on the amount and composition of atmospheric OA over timescales of several days, a prediction that is broadly in line with available measurements of OA evolution over such long timescales. In particular, 3-13% of particle-phase carbon is lost to the gas phase after one week of heterogeneous oxidation. Our results indicate that oxidative aging represents an important sink for particulate organic carbon, and more generally that fragmentation reactions play a major role in the lifecycle of atmospheric OA.
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Affiliation(s)
| | | | | | - Kevin R Wilson
- Chemical Sciences Division, Lawrence Berkeley National Laboratory , Berkeley, California 94720, United States
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Yu P, Toon OB, Bardeen CG, Mills MJ, Fan T, English JM, Neely RR. Evaluations of tropospheric aerosol properties simulated by the community earth system model with a sectional aerosol microphysics scheme. JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS 2015; 7:865-914. [PMID: 27668039 PMCID: PMC5020605 DOI: 10.1002/2014ms000421] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/23/2014] [Accepted: 05/18/2015] [Indexed: 05/16/2023]
Abstract
A sectional aerosol model (CARMA) has been developed and coupled with the Community Earth System Model (CESM1). Aerosol microphysics, radiative properties, and interactions with clouds are simulated in the size-resolving model. The model described here uses 20 particle size bins for each aerosol component including freshly nucleated sulfate particles, as well as mixed particles containing sulfate, primary organics, black carbon, dust, and sea salt. The model also includes five types of bulk secondary organic aerosols with four volatility bins. The overall cost of CESM1-CARMA is approximately ∼2.6 times as much computer time as the standard three-mode aerosol model in CESM1 (CESM1-MAM3) and twice as much computer time as the seven-mode aerosol model in CESM1 (CESM1-MAM7) using similar gas phase chemistry codes. Aerosol spatial-temporal distributions are simulated and compared with a large set of observations from satellites, ground-based measurements, and airborne field campaigns. Simulated annual average aerosol optical depths are lower than MODIS/MISR satellite observations and AERONET observations by ∼32%. This difference is within the uncertainty of the satellite observations. CESM1/CARMA reproduces sulfate aerosol mass within 8%, organic aerosol mass within 20%, and black carbon aerosol mass within 50% compared with a multiyear average of the IMPROVE/EPA data over United States, but differences vary considerably at individual locations. Other data sets show similar levels of comparison with model simulations. The model suggests that in addition to sulfate, organic aerosols also significantly contribute to aerosol mass in the tropical UTLS, which is consistent with limited data.
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Affiliation(s)
- Pengfei Yu
- Department of Atmospheric and Oceanic Sciences University of Colorado Boulder Colorado USA; Laboratory for Atmospheric and Space Physics University of Colorado Boulder Colorado USA
| | - Owen B Toon
- Department of Atmospheric and Oceanic Sciences University of Colorado Boulder Colorado USA; Laboratory for Atmospheric and Space Physics University of Colorado Boulder Colorado USA
| | | | - Michael J Mills
- National Center for Atmospheric Research Boulder Colorado USA
| | - Tianyi Fan
- Department of Atmospheric and Oceanic Sciences University of Colorado Boulder Colorado USA; Laboratory for Atmospheric and Space Physics University of Colorado Boulder Colorado USA; Now at College of Global Change and Earth System Science, Beijing Normal University Beijing China
| | - Jason M English
- Laboratory for Atmospheric and Space Physics University of Colorado Boulder Colorado USA
| | - Ryan R Neely
- National Center for Atmospheric Research Boulder Colorado USA; National Centre for Atmospheric Science and Institute of Climate and Atmospheric Science, School of the Earth and Environment, University of Leeds Leeds UK
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14
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Liao J, Froyd KD, Murphy DM, Keutsch FN, Yu G, Wennberg PO, St Clair JM, Crounse JD, Wisthaler A, Mikoviny T, Jimenez JL, Campuzano-Jost P, Day DA, Hu W, Ryerson TB, Pollack IB, Peischl J, Anderson BE, Ziemba LD, Blake DR, Meinardi S, Diskin G. Airborne measurements of organosulfates over the continental U.S. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2015; 120:2990-3005. [PMID: 26702368 PMCID: PMC4677836 DOI: 10.1002/2014jd022378] [Citation(s) in RCA: 32] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/01/2014] [Revised: 02/25/2015] [Accepted: 02/26/2015] [Indexed: 05/19/2023]
Abstract
Organosulfates are important secondary organic aerosol (SOA) components and good tracers for aerosol heterogeneous reactions. However, the knowledge of their spatial distribution, formation conditions, and environmental impact is limited. In this study, we report two organosulfates, an isoprene-derived isoprene epoxydiols (IEPOX) (2,3-epoxy-2-methyl-1,4-butanediol) sulfate and a glycolic acid (GA) sulfate, measured using the NOAA Particle Analysis Laser Mass Spectrometer (PALMS) on board the NASA DC8 aircraft over the continental U.S. during the Deep Convective Clouds and Chemistry Experiment (DC3) and the Studies of Emissions and Atmospheric Composition, Clouds, and Climate Coupling by Regional Surveys (SEAC4RS). During these campaigns, IEPOX sulfate was estimated to account for 1.4% of submicron aerosol mass (or 2.2% of organic aerosol mass) on average near the ground in the southeast U.S., with lower concentrations in the western U.S. (0.2-0.4%) and at high altitudes (<0.2%). Compared to IEPOX sulfate, GA sulfate was more uniformly distributed, accounting for about 0.5% aerosol mass on average, and may be more abundant globally. A number of other organosulfates were detected; none were as abundant as these two. Ambient measurements confirmed that IEPOX sulfate is formed from isoprene oxidation and is a tracer for isoprene SOA formation. The organic precursors of GA sulfate may include glycolic acid and likely have both biogenic and anthropogenic sources. Higher aerosol acidity as measured by PALMS and relative humidity tend to promote IEPOX sulfate formation, and aerosol acidity largely drives in situ GA sulfate formation at high altitudes. This study suggests that the formation of aerosol organosulfates depends not only on the appropriate organic precursors but also on emissions of anthropogenic sulfur dioxide (SO2), which contributes to aerosol acidity. KEY POINTS IEPOX sulfate is an isoprene SOA tracer at acidic and low NO conditions Glycolic acid sulfate may be more abundant than IEPOX sulfate globally SO2 impacts IEPOX sulfate by increasing aerosol acidity and water uptake.
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Affiliation(s)
- Jin Liao
- Chemical Sciences Division, Earth System Research Laboratory, NOAABoulder, Colorado, USA
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
| | - Karl D Froyd
- Chemical Sciences Division, Earth System Research Laboratory, NOAABoulder, Colorado, USA
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
| | - Daniel M Murphy
- Chemical Sciences Division, Earth System Research Laboratory, NOAABoulder, Colorado, USA
| | - Frank N Keutsch
- Department of Chemistry, University of Wisconsin-MadisonMadison, Wisconsin, USA
- Now at Department of Chemistry and Chemical Biology, Harvard UniversityCambridge, Massachusetts, USA
| | - Ge Yu
- Department of Chemistry, University of Wisconsin-MadisonMadison, Wisconsin, USA
| | - Paul O Wennberg
- Division of Geology & Planetary SciencesPasadena, California, USA
- Division of Engineering and Applied SciencePasadena, California, USA
| | - Jason M St Clair
- Division of Geology & Planetary SciencesPasadena, California, USA
| | - John D Crounse
- Division of Geology & Planetary SciencesPasadena, California, USA
| | - Armin Wisthaler
- Institut für Ionenphysik und Angewandte Physik, Leopold-Franzens Universität InnsbruckInnsbruck, Austria
- Now at Department of Chemistry, University of OlsoOslo, Norway
| | - Tomas Mikoviny
- Institut für Ionenphysik und Angewandte Physik, Leopold-Franzens Universität InnsbruckInnsbruck, Austria
- Now at Department of Chemistry, University of OlsoOslo, Norway
| | - Jose L Jimenez
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
- Department of Chemistry and Biochemistry, University of Colorado BoulderBoulder, Colorado, USA
| | - Pedro Campuzano-Jost
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
- Department of Chemistry and Biochemistry, University of Colorado BoulderBoulder, Colorado, USA
| | - Douglas A Day
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
- Department of Chemistry and Biochemistry, University of Colorado BoulderBoulder, Colorado, USA
| | - Weiwei Hu
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
- Department of Chemistry and Biochemistry, University of Colorado BoulderBoulder, Colorado, USA
| | - Thomas B Ryerson
- Chemical Sciences Division, Earth System Research Laboratory, NOAABoulder, Colorado, USA
| | - Ilana B Pollack
- Chemical Sciences Division, Earth System Research Laboratory, NOAABoulder, Colorado, USA
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
| | - Jeff Peischl
- Chemical Sciences Division, Earth System Research Laboratory, NOAABoulder, Colorado, USA
- Cooperative Institute for Research in Environmental Sciences, University of Colorado BoulderBoulder, Colorado, USA
| | | | | | - Donald R Blake
- Department of Chemistry, University of CaliforniaIrvine, California, USA
| | - Simone Meinardi
- Department of Chemistry, University of CaliforniaIrvine, California, USA
| | - Glenn Diskin
- NASA Langley Research CenterHampton, Virginia, USA
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15
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Van Wyngarden AL, Pérez-Montaño S, Bui JVH, Li ESW, Nelson TE, Ha KT, Leong L, Iraci LT. Complex chemical composition of colored surface films formed from reactions of propanal in sulfuric acid at upper troposphere/lower stratosphere aerosol acidities. ATMOSPHERIC CHEMISTRY AND PHYSICS 2015; 15:4225-4239. [PMID: 27212937 PMCID: PMC4874526 DOI: 10.5194/acp-15-4225-2015] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/14/2023]
Abstract
Particles in the upper troposphere and lower stratosphere (UT/LS) consist mostly of concentrated sulfuric acid (40-80 wt %) in water. However, airborne measurements have shown that these particles also contain a significant fraction of organic compounds of unknown chemical composition. Acid-catalyzed reactions of carbonyl species are believed to be responsible for significant transfer of gas phase organic species into tropospheric aerosols and are potentially more important at the high acidities characteristic of UT/LS particles. In this study, experiments combining sulfuric acid (H2SO4) with propanal and with mixtures of propanal with glyoxal and/or methylglyoxal at acidities typical of UT/LS aerosols produced highly colored surface films (and solutions) that may have implications for aerosol properties. In order to identify the chemical processes responsible for the formation of the surface films, attenuated total reflectance-Fourier transform infrared (ATR-FTIR) and 1H nuclear magnetic resonance (NMR) spectroscopies were used to analyze the chemical composition of the films. Films formed from propanal were a complex mixture of aldol condensation products, acetals and propanal itself. The major aldol condensation products were the dimer (2-methyl-2-pentenal) and 1,3,5-trimethylbenzene that was formed by cyclization of the linear aldol condensation trimer. Additionally, the strong visible absorption of the films indicates that higher-order aldol condensation products must also be present as minor species. The major acetal species were 2,4,6-triethyl-1,3,5-trioxane and longer-chain linear polyacetals which are likely to separate from the aqueous phase. Films formed on mixtures of propanal with glyoxal and/or methylglyoxal also showed evidence of products of cross-reactions. Since cross-reactions would be more likely than self-reactions under atmospheric conditions, similar reactions of aldehydes like propanal with common aerosol organic species like glyoxal and methylglyoxal have the potential to produce significant organic aerosol mass and therefore could potentially impact chemical, optical and/or cloud-forming properties of aerosols, especially if the products partition to the aerosol surface.
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Affiliation(s)
| | - S. Pérez-Montaño
- Department of Chemistry, San José State University, San José, CA 95192, USA
| | - J. V. H. Bui
- Department of Chemistry, San José State University, San José, CA 95192, USA
| | - E. S. W. Li
- Department of Chemistry, San José State University, San José, CA 95192, USA
| | - T. E. Nelson
- Department of Chemistry, San José State University, San José, CA 95192, USA
| | - K. T. Ha
- Department of Chemistry, San José State University, San José, CA 95192, USA
| | - L. Leong
- Department of Chemistry, San José State University, San José, CA 95192, USA
| | - L. T. Iraci
- Atmospheric Science Branch, NASA Ames Research Center, Moffett Field, CA 94035, USA
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16
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Wang B, Laskin A, Roedel T, Gilles MK, Moffet RC, Tivanski AV, Knopf DA. Heterogeneous ice nucleation and water uptake by field-collected atmospheric particles below 273 K. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2012jd017446] [Citation(s) in RCA: 47] [Impact Index Per Article: 3.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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17
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Pratt KA, Prather KA. Mass spectrometry of atmospheric aerosols--recent developments and applications. Part II: On-line mass spectrometry techniques. MASS SPECTROMETRY REVIEWS 2012; 31:17-48. [PMID: 21449003 DOI: 10.1002/mas.20330] [Citation(s) in RCA: 48] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/09/2009] [Revised: 08/19/2010] [Accepted: 08/19/2010] [Indexed: 05/30/2023]
Abstract
Many of the significant advances in our understanding of atmospheric particles can be attributed to the application of mass spectrometry. Mass spectrometry provides high sensitivity with fast response time to probe chemically complex particles. This review focuses on recent developments and applications in the field of mass spectrometry of atmospheric aerosols. In Part II of this two-part review, we concentrate on real-time mass spectrometry techniques, which provide high time resolution for insight into brief events and diurnal changes while eliminating the potential artifacts acquired during long-term filter sampling. In particular, real-time mass spectrometry has been shown recently to provide the ability to probe the chemical composition of ambient individual particles <30 nm in diameter to further our understanding of how particles are formed through nucleation in the atmosphere. Further, transportable real-time mass spectrometry techniques are now used frequently on ground-, ship-, and aircraft-based studies around the globe to further our understanding of the spatial distribution of atmospheric aerosols. In addition, coupling aerosol mass spectrometry techniques with other measurements in series has allowed the in situ determination of chemically resolved particle effective density, refractive index, volatility, and cloud activation properties.
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Affiliation(s)
- Kerri A Pratt
- Department of Chemistry and Biochemistry, University of California, San Diego, La Jolla, California 92093, USA
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18
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Wang B, Knopf DA. Heterogeneous ice nucleation on particles composed of humic-like substances impacted by O3. ACTA ACUST UNITED AC 2011. [DOI: 10.1029/2010jd014964] [Citation(s) in RCA: 62] [Impact Index Per Article: 4.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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19
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Pratt KA, Prather KA. Aircraft measurements of vertical profiles of aerosol mixing states. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2009jd013150] [Citation(s) in RCA: 88] [Impact Index Per Article: 6.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/16/2022]
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20
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Nguyen HN, Martinsson BG, Wagner JB, Carlemalm E, Ebert M, Weinbruch S, Brenninkmeijer CAM, Heintzenberg J, Hermann M, Schuck T, van Velthoven PFJ, Zahn A. Chemical composition and morphology of individual aerosol particles from a CARIBIC flight at 10 km altitude between 50°N and 30°S. ACTA ACUST UNITED AC 2008. [DOI: 10.1029/2008jd009956] [Citation(s) in RCA: 25] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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21
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Renard JB, Brogniez C, Berthet G, Bourgeois Q, Gaubicher B, Chartier M, Balois JY, Verwaerde C, Auriol F, Francois P, Daugeron D, Engrand C. Vertical distribution of the different types of aerosols in the stratosphere: Detection of solid particles and analysis of their spatial variability. ACTA ACUST UNITED AC 2008. [DOI: 10.1029/2008jd010150] [Citation(s) in RCA: 52] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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22
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Prather KA, Hatch CD, Grassian VH. Analysis of atmospheric aerosols. ANNUAL REVIEW OF ANALYTICAL CHEMISTRY (PALO ALTO, CALIF.) 2008; 1:485-514. [PMID: 20636087 DOI: 10.1146/annurev.anchem.1.031207.113030] [Citation(s) in RCA: 58] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/29/2023]
Abstract
Aerosols represent an important component of the Earth's atmosphere. Because aerosols are composed of solid and liquid particles of varying chemical complexity, size, and phase, large challenges exist in understanding how they impact climate, health, and the chemistry of the atmosphere. Only through the integration of field, laboratory, and modeling analysis can we begin to unravel the roles atmospheric aerosols play in these global processes. In this article, we provide a brief review of the current state of the science in the analysis of atmospheric aerosols and some important challenges that need to be overcome before they can become fully integrated. It is clear that only when these areas are effectively bridged can we fully understand the impact that atmospheric aerosols have on our environment and the Earth's system at the level of scientific certainty necessary to design and implement sound environmental policies.
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Affiliation(s)
- Kimberly A Prather
- Department of Chemistry and Biochemistry, Scripps Institution of Oceanography, University of California, San Diego, 92093-0314, USA.
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23
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Murphy DM, Cziczo DJ, Froyd KD, Hudson PK, Matthew BM, Middlebrook AM, Peltier RE, Sullivan A, Thomson DS, Weber RJ. Single-particle mass spectrometry of tropospheric aerosol particles. ACTA ACUST UNITED AC 2006. [DOI: 10.1029/2006jd007340] [Citation(s) in RCA: 375] [Impact Index Per Article: 20.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
Affiliation(s)
- D. M. Murphy
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - D. J. Cziczo
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - K. D. Froyd
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - P. K. Hudson
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - B. M. Matthew
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | | | - R. E. Peltier
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
| | - A. Sullivan
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
| | - D. S. Thomson
- Earth System Research Laboratory; NOAA; Boulder Colorado USA
| | - R. J. Weber
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
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