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Fahy WD, Wania F, Abbatt JPD. When Does Multiphase Chemistry Influence Indoor Chemical Fate? ENVIRONMENTAL SCIENCE & TECHNOLOGY 2024; 58:4257-4267. [PMID: 38380897 DOI: 10.1021/acs.est.3c08751] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 02/22/2024]
Abstract
Human chemical exposure often occurs indoors, where large variability in contaminant concentrations and indoor chemical dynamics make assessments of these exposures challenging. A major source of uncertainty lies in the rates of chemical transformations which, due to high surface-to-volume ratios and rapid air change rates relative to rates of gas-phase reactions indoors, are largely gas-surface multiphase processes. It remains unclear how important such chemistry is in controlling indoor chemical lifetimes and, therefore, human exposure to both parent compounds and transformation products. We present a multimedia steady-state fugacity-based model to assess the importance of multiphase chemistry relative to cleaning and mass transfer losses, examine how the physicochemical properties of compounds and features of the indoor environment affect these processes, and investigate uncertainties pertaining to indoor multiphase chemistry and chemical lifetimes. We find that multiphase reactions can play an important role in chemical fate indoors for reactive compounds with low volatility, i.e., octanol-air equilibrium partitioning ratios (Koa) above 108, with the impact of this chemistry dependent on chemical identity, oxidant type and concentration, and other parameters. This work highlights the need for further research into indoor chemical dynamics and multiphase chemistry to constrain human exposure to chemicals in the built environment.
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Affiliation(s)
- William D Fahy
- Department of Chemistry, University of Toronto, Toronto, Ontario M5S 3H6, Canada
| | - Frank Wania
- Department of Physical and Environmental Sciences, University of Toronto at Scarborough, Toronto, Ontario M1C 1A4, Canada
| | - Jonathan P D Abbatt
- Department of Chemistry, University of Toronto, Toronto, Ontario M5S 3H6, Canada
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2
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Wan Z, Zhu C, Francisco JS. Molecular Insights into the Spontaneous Generation of Cl 2O in the Reaction of ClONO 2 and HOCl at the Air-Water Interface. J Am Chem Soc 2023; 145:17478-17484. [PMID: 37522957 DOI: 10.1021/jacs.3c06527] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 08/01/2023]
Abstract
Chemical processes involving chlorine nitrate (ClONO2) at the surface of stratospheric aerosols are crucial to ozone depletion. Herein, we show a reaction route for the formation of Cl2O, which is a source of stratospheric chlorine, in the ClONO2 + HOCl reaction at the air-water interface. Our ab initio molecular dynamics (AIMD) simulations show that the (ClONO2)Cl···O(HOCl) halogen bond plays a key role in the reaction and is the main interaction between ClONO2 and HOCl both at the air-water interface and in the bulk liquid water. Furthermore, metadynamics-based AIMD simulations reveal two pathways: (i) The OCl fragment of HOCl binds to the Cl atom in ClONO2, resulting in the formation of Cl2O and NO3-. Simultaneously, the remaining hydrogen atom is transferred to a water molecule to form H3O+. (ii) HOCl acts as a bridge for Cl atom transfer from ClONO2 to the O atom of a water molecule, and this water molecule transfers one of its H atoms to another water molecule, forming two HOCl molecules, NO3-, and H3O+. Free-energy calculations show that the former is the energetically more favorable process. More importantly, the free-energy barrier for Cl2O formation at the air-water interface is only ∼0.8 kcal/mol, and the reaction is exothermic. These findings provide insights into the importance of fundamental chlorine chemistry and the broader implications of the aerosol air-water interface for atmospheric chemistry.
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Affiliation(s)
- Zhengyi Wan
- Department of Chemistry, University of Pennsylvania, Philadelphia, Pennsylvania 19104, United States
| | - Chongqin Zhu
- College of Chemistry, Key Laboratory of Theoretical & Computational Photochemistry of Ministry of Education, Beijing Normal University, Beijing 100190, People's Republic of China
| | - Joseph S Francisco
- Department of Chemistry, University of Pennsylvania, Philadelphia, Pennsylvania 19104, United States
- Department of Earth & Environmental Science, University of Pennsylvania, Philadelphia, Pennsylvania 19104, United States
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3
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Wan Z, Fang Y, Liu Z, Francisco JS, Zhu C. Mechanistic Insights into the Reactive Uptake of Chlorine Nitrate at the Air-Water Interface. J Am Chem Soc 2023; 145:944-952. [PMID: 36595549 DOI: 10.1021/jacs.2c09837] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/04/2023]
Abstract
It is well-known that the aqueous-phase processing of chlorine nitrate (ClONO2) plays a crucial role in ozone depletion. However, many of the physical and chemical properties of ClONO2 at the air-water interface or in bulk water are unknown or not understood on a microscopic scale. Here, the solvation and hydrolysis of ClONO2 at the air-water interface and in bulk water at 300 K were investigated by classical and ab initio molecular dynamics (AIMD) simulations combined with free energy methods. Our results revealed that ClONO2 prefers to accumulate at the air-water interface rather than in the bulk phase. Specifically, halogen bonding interactions (ClONO2)Cl···O(H2O) were found to be the predominant interactions between ClONO2 and H2O. Moreover, metadynamics-biased AIMD simulations revealed that ClONO2 hydrolysis is catalyzed at the air-water interface with an activation barrier of only ∼0.2 kcal/mol; additionally, the difference in free energy between the product and reactant is only ∼0.1 kcal/mol. Surprisingly, the near-barrierless reaction and the comparable free energies of the reactant and product suggested that the ClONO2 hydrolysis at the air-water interface is reversible. When the temperature is lowered from 300 to 200 K, the activation barrier for the ClONO2 hydrolysis at the air-water interface is increased to ∼5.4 kcal/mol. These findings have important implications for the interpretation of experiments.
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Affiliation(s)
- Zhengyi Wan
- Department of Chemistry, University of Pennsylvania, Philadelphia, Pennsylvania19104, United States
| | - Yeguang Fang
- College of Chemistry, Key Laboratory of Theoretical & Computational Photochemistry of Ministry of Education, Beijing Normal University, Beijing100190, People's Republic of China
| | - Ziao Liu
- Department of Chemistry, University of Pennsylvania, Philadelphia, Pennsylvania19104, United States
| | - Joseph S Francisco
- Department of Chemistry, University of Pennsylvania, Philadelphia, Pennsylvania19104, United States.,Department of Earth & Environmental Science, University of Pennsylvania, Philadelphia, Pennsylvania19104, United States
| | - Chongqin Zhu
- College of Chemistry, Key Laboratory of Theoretical & Computational Photochemistry of Ministry of Education, Beijing Normal University, Beijing100190, People's Republic of China
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4
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Wilson KR, Prophet AM, Willis MD. A Kinetic Model for Predicting Trace Gas Uptake and Reaction. J Phys Chem A 2022; 126:7291-7308. [PMID: 36170058 DOI: 10.1021/acs.jpca.2c03559] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Abstract
A model is developed to describe trace gas uptake and reaction with applications to aerosols and microdroplets. Gas uptake by the liquid is formulated as a coupled equilibria that links gas, surface, and bulk regions of the droplet or solution. Previously, this framework was used in explicit stochastic reaction-diffusion simulations to predict the reactive uptake kinetics of ozone with droplets containing aqueous aconitic acid, maleic acid, and sodium nitrite. With the use of prior data and simulation results, a new equation for the uptake coefficient is derived, which accounts for both surface and bulk reactions. Lambert W functions are used to obtain closed form solutions to the integrated rate laws for the multiphase kinetics; similar to previous expressions that describe Michaelis-Menten enzyme kinetics. Together these equations couple interface and bulk processes over a wide range of conditions and do not require many of the limiting assumptions needed to apply resistor model formulations to explain trace gas uptake and reaction.
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Affiliation(s)
- Kevin R Wilson
- Chemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States
| | - Alexander M Prophet
- Chemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States.,Department of Chemistry, University of California, Berkeley, California 94720, United States
| | - Megan D Willis
- Department of Chemistry, Colorado State University, Fort Collins, Colorado 80523 United States
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5
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Alpert PA, Corral Arroyo P, Dou J, Krieger UK, Steimer SS, Förster JD, Ditas F, Pöhlker C, Rossignol S, Passananti M, Perrier S, George C, Shiraiwa M, Berkemeier T, Watts B, Ammann M. Visualizing reaction and diffusion in xanthan gum aerosol particles exposed to ozone. Phys Chem Chem Phys 2019; 21:20613-20627. [PMID: 31528972 DOI: 10.1039/c9cp03731d] [Citation(s) in RCA: 15] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/19/2022]
Abstract
Atmospheric aerosol particles with a high viscosity may become inhomogeneously mixed during chemical processing. Models have predicted gradients in condensed phase reactant concentration throughout particles as the result of diffusion and chemical reaction limitations, termed chemical gradients. However, these have never been directly observed for atmospherically relevant particle diameters. We investigated the reaction between ozone and aerosol particles composed of xanthan gum and FeCl2 and observed the in situ chemical reaction that oxidized Fe2+ to Fe3+ using X-ray spectromicroscopy. Iron oxidation state of particles as small as 0.2 μm in diameter were imaged over time with a spatial resolution of tens of nanometers. We found that the loss off Fe2+ accelerated with increasing ozone concentration and relative humidity, RH. Concentric 2-D column integrated profiles of the Fe2+ fraction, α, out of the total iron were derived and demonstrated that particle surfaces became oxidized while particle cores remained unreacted at RH = 0-20%. At higher RH, chemical gradients evolved over time, extended deeper from the particle surface, and Fe2+ became more homogeneously distributed. We used the kinetic multi-layer model for aerosol surface and bulk chemistry (KM-SUB) to simulate ozone reaction constrained with our observations and inferred key parameters as a function of RH including Henry's Law constant for ozone, HO3, and diffusion coefficients for ozone and iron, DO3 and DFe, respectively. We found that HO3 is higher in our xanthan gum/FeCl2 particles than for water and increases when RH decreased from about 80% to dry conditions. This coincided with a decrease in both DO3 and DFe. In order to reproduce observed chemical gradients, our model predicted that ozone could not be present further than a few nanometers from a particle surface indicating near surface reactions were driving changes in iron oxidation state. However, the observed chemical gradients in α observed over hundreds of nanometers must have been the result of iron transport from the particle interior to the surface where ozone oxidation occurred. In the context of our results, we examine the applicability of the reacto-diffusive framework and discuss diffusion limitations for other reactive gas-aerosol systems of atmospheric importance.
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Affiliation(s)
- Peter A Alpert
- Laboratory of Environmental Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland.
| | - Pablo Corral Arroyo
- Laboratory of Environmental Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland. and Institute for Physical Chemistry, ETH Zürich, 8092 Zürich, Switzerland
| | - Jing Dou
- Institute for Atmospheric and Climate Science, ETH Zürich, 8092 Zürich, Switzerland
| | - Ulrich K Krieger
- Institute for Atmospheric and Climate Science, ETH Zürich, 8092 Zürich, Switzerland
| | - Sarah S Steimer
- Department of Chemistry, University of Cambridge, Cambridge, CB2 1EW, UK
| | - Jan-David Förster
- Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - Florian Ditas
- Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - Christopher Pöhlker
- Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - Stéphanie Rossignol
- Univ. Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, F-69626, Villeurbanne, France and Aix Marseille Université, CNRS, LCE UMR 7376, 13331 Marseille, France
| | - Monica Passananti
- Univ. Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, F-69626, Villeurbanne, France and Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00710, Helsinki, Finland and Dipartimento di Chimica, Università di Torino, Via Giuria 5, 10125 Torino, Italy
| | - Sebastien Perrier
- Univ. Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, F-69626, Villeurbanne, France
| | - Christian George
- Univ. Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, F-69626, Villeurbanne, France
| | - Manabu Shiraiwa
- Department of Chemistry, University of California, Irvine, CA 92697-2025, USA
| | - Thomas Berkemeier
- Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany and School of Chemical & Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA 30332, USA
| | - Benjamin Watts
- Laboratory for Synchrotron Radiation-Condensed Matter, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
| | - Markus Ammann
- Laboratory of Environmental Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland.
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6
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Hoffmann EH, Tilgner A, Wolke R, Herrmann H. Enhanced Chlorine and Bromine Atom Activation by Hydrolysis of Halogen Nitrates from Marine Aerosols at Polluted Coastal Areas. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2019; 53:771-778. [PMID: 30557005 DOI: 10.1021/acs.est.8b05165] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/14/2023]
Abstract
Detailed multiphase chemistry box model studies are carried out, investigating halogen radical activation at polluted coastal areas. Simulations are performed for a nonpermanent cloud and a cloud-free scenario and reveal that ClNO2 photolysis and ICl photolysis are crucial for gas-phase Cl atom activation. In the cloud scenario, the integrated ClNO2 and ICl photolysis rates are 3.7 × 107 and 3.1 × 107 molecules cm-3 s-1. In the cloud-free scenario, the integrated ClNO2 and ICl photolysis rates are 8.1 × 107 and 3.6 × 107 molecules cm-3 s-1. The simulations show larger contributions of ClNO2 photolysis in the morning and higher ones of ICl photolysis during afternoon. Throughout the simulation, average contributions to Cl atom activation in the cloud and cloud-free scenarios by ClNO2 photolysis are 42% and 62% and by ICl photolysis 35% and 28%, respectively. ICl is formed through an aqueous-phase reaction of HOI with chloride. Two thirds of the formed ICl is released into the gas phase. The residual third reacts with bromide, creating IBr. Overall, the simulations emphasize the crucial role of INO3 hydrolysis for Cl and Br atom activation in polluted coastal areas. Therefore, it needs to be considered in chemical transport models to improve air quality predictions.
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Affiliation(s)
- Erik H Hoffmann
- Leibniz Institute for Tropospheric Research (TROPOS) , Permoserstrasse 15 , D-04318 Leipzig , Germany
| | - Andreas Tilgner
- Leibniz Institute for Tropospheric Research (TROPOS) , Permoserstrasse 15 , D-04318 Leipzig , Germany
| | - Ralf Wolke
- Leibniz Institute for Tropospheric Research (TROPOS) , Permoserstrasse 15 , D-04318 Leipzig , Germany
| | - Hartmut Herrmann
- Leibniz Institute for Tropospheric Research (TROPOS) , Permoserstrasse 15 , D-04318 Leipzig , Germany
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7
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Wren SN, Donaldson D. Glancing-angle Raman study of nitrate and nitric acid at the air–aqueous interface. Chem Phys Lett 2012. [DOI: 10.1016/j.cplett.2011.10.019] [Citation(s) in RCA: 28] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/16/2022]
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8
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Abbatt JPD, Lee AKY, Thornton JA. Quantifying trace gas uptake to tropospheric aerosol: recent advances and remaining challenges. Chem Soc Rev 2012; 41:6555-81. [DOI: 10.1039/c2cs35052a] [Citation(s) in RCA: 161] [Impact Index Per Article: 13.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/23/2022]
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9
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Davidovits P, Kolb CE, Williams LR, Jayne JT, Worsnop DR. Update 1 of: Mass Accommodation and Chemical Reactions at Gas−Liquid Interfaces. Chem Rev 2011; 111:PR76-109. [DOI: 10.1021/cr100360b] [Citation(s) in RCA: 54] [Impact Index Per Article: 4.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
- Paul Davidovits
- Chemistry Department, 2609 Beacon Street, Boston College, Chestnut Hill, Massachusetts 02467, United States
| | - Charles E. Kolb
- Center for Aerosol and Cloud Chemistry, Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, United States
- This is a Chemical Reviews Perennial Review. The root paper of this title was published in Chem. Rev.2006, 106 (4), 1323−1354, DOI: 10.1021.cr040366k; Published (Web) March 16, 2006. Updates to the text appear in red type
| | - Leah R. Williams
- Center for Aerosol and Cloud Chemistry, Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, United States
- This is a Chemical Reviews Perennial Review. The root paper of this title was published in Chem. Rev.2006, 106 (4), 1323−1354, DOI: 10.1021.cr040366k; Published (Web) March 16, 2006. Updates to the text appear in red type
| | - John T. Jayne
- Center for Aerosol and Cloud Chemistry, Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, United States
- This is a Chemical Reviews Perennial Review. The root paper of this title was published in Chem. Rev.2006, 106 (4), 1323−1354, DOI: 10.1021.cr040366k; Published (Web) March 16, 2006. Updates to the text appear in red type
| | - Douglas R. Worsnop
- Center for Aerosol and Cloud Chemistry, Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, United States
- This is a Chemical Reviews Perennial Review. The root paper of this title was published in Chem. Rev.2006, 106 (4), 1323−1354, DOI: 10.1021.cr040366k; Published (Web) March 16, 2006. Updates to the text appear in red type
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10
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Davis EJ. Interpretation of Uptake Coefficient Data Obtained with Flow Tubes. J Phys Chem A 2008; 112:1922-32. [DOI: 10.1021/jp074939j] [Citation(s) in RCA: 8] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/04/2023]
Affiliation(s)
- E. James Davis
- Department of Chemical Engineering, University of Washington, Box 351750, Seattle, Washington 98195-1750
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11
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Perkins BG, Nesbitt DJ. Quantum state-resolved CO2 collisions at the gas-liquid interface: surface temperature-dependent scattering dynamics. J Phys Chem B 2008; 112:507-19. [PMID: 18052277 DOI: 10.1021/jp077488b] [Citation(s) in RCA: 40] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Abstract
Energy transfer dynamics at the gas-liquid interface are investigated as a function of surface temperature both by experimental studies of CO2 + perfluorinated polyether (PFPE) and by molecular dynamics simulations of CO2 + fluorinated self-assembled monolayers (F-SAMs). Using a normal incident molecular beam, the experimental studies probe scattered CO2 internal-state and translational distributions with high resolution infrared spectroscopy. At low incident energies [Einc = 1.6(1) kcal/mol], CO2 J-state populations and transverse Doppler velocity distributions are characteristic of the surface temperature (Trot approximately Ttrans approximately TS) over the range from 232 to 323 K. In contrast, the rotational and translational distributions at high incident energies [Einc = 10.6(8) kcal/mol] show evidence for both trapping-desorption (TD) and impulsive scattering (IS) events. Specifically, the populations are surprisingly well-characterized by a sum of Boltzmann distributions where the two components include one (TD) that equilibrates with the surface (TTD approximately TS) and a second (IS) that is much hotter than the surface temperature (TIS > TS). Support for the superthermal, yet Boltzmann, nature of the IS channel is provided by molecular dynamics (MD) simulations of CO2 + F-SAMs [Einc = 10.6 kcal/mol], which reveal two-temperature distributions, sticking probabilities, and angular distributions in near quantitative agreement with the experimental PFPE results. Finally, experiments as a function of surface temperature reveal an increase in both sticking probability and rotational/translational temperature of the IS component. Such a trend is consistent with increased surface roughness at higher surface temperature, which increases the overall probability of trapping, yet preferentially leads to impulsive scattering of more highly internally excited CO2 from the surface.
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Affiliation(s)
- Bradford G Perkins
- JILA, University of Colorado and National Institute of Standards and Technology, and Department of Chemistry and Biochemistry, University of Colorado, Boulder, Colorado 80309-0440, USA
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12
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Knopf DA, Cosman LM, Mousavi P, Mokamati S, Bertram AK. A Novel Flow Reactor for Studying Reactions on Liquid Surfaces Coated by Organic Monolayers: Methods, Validation, and Initial Results. J Phys Chem A 2007; 111:11021-32. [DOI: 10.1021/jp075724c] [Citation(s) in RCA: 38] [Impact Index Per Article: 2.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- D. A. Knopf
- Department of Chemistry and Department of Mechanical Engineering, University of British Columbia, British Columbia, Canada, and School of Marine and Atmospheric Sciences/Institute for Terrestrial and Planetary Atmospheres, Stony Brook University, New York 11794
| | - L. M. Cosman
- Department of Chemistry and Department of Mechanical Engineering, University of British Columbia, British Columbia, Canada, and School of Marine and Atmospheric Sciences/Institute for Terrestrial and Planetary Atmospheres, Stony Brook University, New York 11794
| | - P. Mousavi
- Department of Chemistry and Department of Mechanical Engineering, University of British Columbia, British Columbia, Canada, and School of Marine and Atmospheric Sciences/Institute for Terrestrial and Planetary Atmospheres, Stony Brook University, New York 11794
| | - S. Mokamati
- Department of Chemistry and Department of Mechanical Engineering, University of British Columbia, British Columbia, Canada, and School of Marine and Atmospheric Sciences/Institute for Terrestrial and Planetary Atmospheres, Stony Brook University, New York 11794
| | - A. K. Bertram
- Department of Chemistry and Department of Mechanical Engineering, University of British Columbia, British Columbia, Canada, and School of Marine and Atmospheric Sciences/Institute for Terrestrial and Planetary Atmospheres, Stony Brook University, New York 11794
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13
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Davidovits P, Kolb CE, Williams LR, Jayne JT, Worsnop DR. Mass accommodation and chemical reactions at gas-liquid interfaces. Chem Rev 2007; 106:1323-54. [PMID: 16608183 DOI: 10.1021/cr040366k] [Citation(s) in RCA: 210] [Impact Index Per Article: 12.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/12/2022]
Affiliation(s)
- Paul Davidovits
- Chemistry Department, 2609 Beacon Street, Boston College, Chestnut Hill, Massachusetts 02467, USA.
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14
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Bogdan A, Molina MJ, Sassen K, Kulmala M. Formation of Low-Temperature Cirrus from H2SO4/H2O Aerosol Droplets. J Phys Chem A 2006; 110:12541-2. [PMID: 17107102 DOI: 10.1021/jp065898e] [Citation(s) in RCA: 15] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Abstract
We present experimental results obtained with a differential scanning calorimeter (DSC) that indicate the small ice particles in low-temperature cirrus clouds are not completely solid but rather coated with an unfrozen H2SO4/H2O overlayer. Our results provide a new look on the formation, development, and microphysical properties of low-temperature cirrus clouds.
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15
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Davidovits P, Worsnop DR, Williams LR, Kolb CE, Gershenzon M. Comment on “Mass Accommodation Coefficient of Water: Molecular Dynamics Simulation and Revised Analysis of Droplet Train/Flow Reactor Experiment”. J Phys Chem B 2005; 109:14742-6; discussion 14747-9. [PMID: 16852859 DOI: 10.1021/jp0449915] [Citation(s) in RCA: 17] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/28/2023]
Affiliation(s)
- P Davidovits
- Chemistry Department, Merkert Chemistry Center, Boston College, Chestnut Hill, Massachusetts 02167-3809, USA.
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16
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Hanson DR, Kosciuch E. Reply to “Comment on ‘The NH3 Mass Accommodation Coefficient for Uptake onto Sulfuric Acid Solutions'”. J Phys Chem A 2004. [DOI: 10.1021/jp0311761] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
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17
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Givan A, Loewenschuss A, Nielsen CJ. Infrared spectra and ab initio calculations of the matrix isolated (CO2)·(H2SO4) and (CO2)·(SO3) complexes. J Mol Struct 2002. [DOI: 10.1016/s0022-2860(01)00644-5] [Citation(s) in RCA: 15] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/27/2022]
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18
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Shi Q, Jayne JT, Kolb CE, Worsnop DR, Davidovits P. Kinetic model for reaction of ClONO2with H2O and HCl and HOCl with HCl in sulfuric acid solutions. ACTA ACUST UNITED AC 2001. [DOI: 10.1029/2000jd000181] [Citation(s) in RCA: 74] [Impact Index Per Article: 3.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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19
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Givan A, Loewenschuss A, Nielsen CJ. Infrared Evidence for the Existence of the (HCl)*(H2SO4) Complex Trapped in Argon at 5 K. J Phys Chem A 2000. [DOI: 10.1021/jp9926241] [Citation(s) in RCA: 8] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- Aharon Givan
- Department of Inorganic and Analytical Chemistry, The Hebrew University of Jerusalem, Jerusalem 91904, Israel, and Department of Chemistry, University of Oslo, Blindern, N-0315 Oslo, Norway
| | - Aharon Loewenschuss
- Department of Inorganic and Analytical Chemistry, The Hebrew University of Jerusalem, Jerusalem 91904, Israel, and Department of Chemistry, University of Oslo, Blindern, N-0315 Oslo, Norway
| | - Claus J. Nielsen
- Department of Inorganic and Analytical Chemistry, The Hebrew University of Jerusalem, Jerusalem 91904, Israel, and Department of Chemistry, University of Oslo, Blindern, N-0315 Oslo, Norway
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20
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Robinson GN, Worsnop DR, Jayne JT, Kolb CE, Swartz E, Davidovits P. Heterogeneous uptake of HCl by sulfuric acid solutions. ACTA ACUST UNITED AC 1998. [DOI: 10.1029/98jd02085] [Citation(s) in RCA: 35] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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21
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Hanson DR. Reaction of ClONO2 with H2O and HCl in Sulfuric Acid and HNO3/H2SO4/H2O Mixtures. J Phys Chem A 1998. [DOI: 10.1021/jp972767s] [Citation(s) in RCA: 62] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Affiliation(s)
- David R. Hanson
- CIRES and NOAA Aeronomy Laboratory, Boulder, Colorado 80303-3328
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22
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Abstract
Liquid and solid particles in polar stratospheric clouds are of central importance for the depletion of stratospheric ozone. Surface-catalyzed reactions on these particles, and diffusion-controlled processes in the bulk of the particles, convert halogens, which derive from compounds of mainly anthropogenic origin, from relatively inert reservoir species into forms that efficiently destroy ozone. The microphysics of these particles under cold stratospheric conditions is still uncertain in many respects, in particular concerning phase transitions such as freezing nucleation and deposition nucleation. Furthermore, there are indications that the rates of key heterogeneous reactions have not yet been established with sufficient accuracy to enable a reliable diagnosis of observed ozone losses by means of global models. The present paper reviews the current (late 1996) knowledge of the physico-chemistry of polar stratospheric clouds and evaluates the remaining uncertainties with respect to their ozone depletion potential.
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Affiliation(s)
- T Peter
- Max Planck Institute for Chemistry, Postfach 3060, D-55020 Mainz, Germany
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Robinson GN, Worsnop DR, Jayne JT, Kolb CE, Davidovits P. Heterogeneous uptake of ClONO2and N2O5by sulfuric acid solutions. ACTA ACUST UNITED AC 1997. [DOI: 10.1029/96jd03457] [Citation(s) in RCA: 103] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Kawa SR, Newman PA, Lait LR, Schoeberl MR, Stimpfle RM, Kohn DW, Webster CR, May RD, Baumgardner D, Dye JE, Wilson JC, Chan KR, Loewenstein M. Activation of chlorine in sulfate aerosol as inferred from aircraft observations. ACTA ACUST UNITED AC 1997. [DOI: 10.1029/96jd01992] [Citation(s) in RCA: 49] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Hu JH, Abbatt JPD. Reaction Probabilities for N2O5 Hydrolysis on Sulfuric Acid and Ammonium Sulfate Aerosols at Room Temperature. J Phys Chem A 1997. [DOI: 10.1021/jp9627436] [Citation(s) in RCA: 110] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- J. H. Hu
- Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Ave., Chicago, Illinois 60637
| | - J. P. D. Abbatt
- Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Ave., Chicago, Illinois 60637
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Jucks KW, Johnson DG, Chance KV, Traub WA, Salawitch RJ, Stachnik RA. Ozone production and loss rate measurements in the middle stratosphere. ACTA ACUST UNITED AC 1996. [DOI: 10.1029/96jd02739] [Citation(s) in RCA: 35] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Molina MJ, Molina LT, Kolb CE. GAS-PHASE AND HETEROGENEOUS CHEMICAL KINETICS OF THE TROPOSPHERE AND STRATOSPHERE. Annu Rev Phys Chem 1996. [DOI: 10.1146/annurev.physchem.47.1.327] [Citation(s) in RCA: 125] [Impact Index Per Article: 4.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Mario J. Molina
- Department of Earth, Atmospheric and Planetary Sciences and Department of Chemistry, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139
| | - Luisa T. Molina
- Department of Earth, Atmospheric and Planetary Sciences and Department of Chemistry, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139
| | - Charles E. Kolb
- Center for Chemical and Environmental Physics, Aerodyne Research, Inc, Billerica, Massachusetts 01821-3976
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Aker PM, Moortgat PA, Aiello D, Zhang JX, Nichols W. Reply [to “Comment on ‘A spectroscopic tour through the liquid aerosol interface: Implications for atmospheric chemistry’ by Jian-Xiang Zhang, Denise Aiello, and Pamela M. Aker”]. ACTA ACUST UNITED AC 1996. [DOI: 10.1029/95jd03789] [Citation(s) in RCA: 10] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Molina MJ, Molina LT, Golden DM. Environmental Chemistry (Gas and Gas−Solid Interactions): The Role of Physical Chemistry. ACTA ACUST UNITED AC 1996. [DOI: 10.1021/jp960146d] [Citation(s) in RCA: 48] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Affiliation(s)
- Mario J. Molina
- Department of Earth, Atmospheric and Planetary Sciences and Department of Chemistry, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139
| | - Luisa T. Molina
- Department of Earth, Atmospheric and Planetary Sciences and Department of Chemistry, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139
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Klassen JK, Nathanson GM. Hydrogen-Bond Breaking and Proton Exchange in Collisions of Gaseous Formic Acid with Liquid Sulfuric Acid. Science 1996; 273:333-5. [PMID: 8662514 DOI: 10.1126/science.273.5273.333] [Citation(s) in RCA: 19] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/01/2023]
Abstract
Gas-liquid scattering experiments provide direct observations of the fate of hydrogen-bonding molecules striking the surfaces of acidic liquids. Collisions of gaseous formic acid with concentrated sulfuric acid show that impinging monomers (HCOOH and DCOOD) scatter inelastically from the interface or become trapped by surface H2SO4. Most trapped DCOOD molecules undergo proton exchange before desorbing from the acid, indicating that gas-surface accommodation almost always leads to reaction with H2SO4 molecules. This proton transfer is not inhibited by dimerization of the formic acid: The dimers readily undergo intramolecular hydrogen bond cleavage and D-H exchange before desorbing from the acid.
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Affiliation(s)
- JK Klassen
- Department of Chemistry, University of Wisconsin, 1101 University Avenue, Madison, WI 53706, USA
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Hanson DR, Lovejoy ER. Heterogeneous Reactions in Liquid Sulfuric Acid: HOCl + HCl as a Model System. ACTA ACUST UNITED AC 1996. [DOI: 10.1021/jp953250o] [Citation(s) in RCA: 67] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- David R. Hanson
- Aeronomy Laboratory, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, Colorado 80303
| | - Edward R. Lovejoy
- Aeronomy Laboratory, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, Colorado 80303
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Hanson DR, Ravishankara AR, Lovejoy ER. Reaction of BrONO2with H2O on submicron sulfuric acid aerosol and the implications for the lower stratosphere. ACTA ACUST UNITED AC 1996. [DOI: 10.1029/96jd00347] [Citation(s) in RCA: 116] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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