Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system

Sulfuric acid is an important gas influencing atmospheric new particle formation (NPF). Both the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) system and the ternary system involving ammonia (H<sub>2</sub>SO<sub>4</sub>–H<sub>2&...

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Main Authors: A. Kürten, S. Münch, L. Rondo, F. Bianchi, J. Duplissy, T. Jokinen, H. Junninen, N. Sarnela, S. Schobesberger, M. Simon, M. Sipilä, J. Almeida, A. Amorim, J. Dommen, N. M. Donahue, E. M. Dunne, R. C. Flagan, A. Franchin, J. Kirkby, A. Kupc, V. Makhmutov, T. Petäjä, A. P. Praplan, F. Riccobono, G. Steiner, A. Tomé, G. Tsagkogeorgas, P. E. Wagner, D. Wimmer, U. Baltensperger, M. Kulmala, D. R. Worsnop, J. Curtius
Format: Article
Language:English
Published: Copernicus Publications 2015-09-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/10701/2015/acp-15-10701-2015.pdf
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author A. Kürten
S. Münch
L. Rondo
F. Bianchi
J. Duplissy
T. Jokinen
H. Junninen
N. Sarnela
S. Schobesberger
M. Simon
M. Sipilä
J. Almeida
A. Amorim
J. Dommen
N. M. Donahue
E. M. Dunne
R. C. Flagan
A. Franchin
J. Kirkby
A. Kupc
V. Makhmutov
T. Petäjä
A. P. Praplan
F. Riccobono
G. Steiner
A. Tomé
G. Tsagkogeorgas
P. E. Wagner
D. Wimmer
U. Baltensperger
M. Kulmala
D. R. Worsnop
J. Curtius
spellingShingle A. Kürten
S. Münch
L. Rondo
F. Bianchi
J. Duplissy
T. Jokinen
H. Junninen
N. Sarnela
S. Schobesberger
M. Simon
M. Sipilä
J. Almeida
A. Amorim
J. Dommen
N. M. Donahue
E. M. Dunne
R. C. Flagan
A. Franchin
J. Kirkby
A. Kupc
V. Makhmutov
T. Petäjä
A. P. Praplan
F. Riccobono
G. Steiner
A. Tomé
G. Tsagkogeorgas
P. E. Wagner
D. Wimmer
U. Baltensperger
M. Kulmala
D. R. Worsnop
J. Curtius
Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system
Atmospheric Chemistry and Physics
author_facet A. Kürten
S. Münch
L. Rondo
F. Bianchi
J. Duplissy
T. Jokinen
H. Junninen
N. Sarnela
S. Schobesberger
M. Simon
M. Sipilä
J. Almeida
A. Amorim
J. Dommen
N. M. Donahue
E. M. Dunne
R. C. Flagan
A. Franchin
J. Kirkby
A. Kupc
V. Makhmutov
T. Petäjä
A. P. Praplan
F. Riccobono
G. Steiner
A. Tomé
G. Tsagkogeorgas
P. E. Wagner
D. Wimmer
U. Baltensperger
M. Kulmala
D. R. Worsnop
J. Curtius
author_sort A. Kürten
title Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system
title_short Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system
title_full Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system
title_fullStr Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system
title_full_unstemmed Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system
title_sort thermodynamics of the formation of sulfuric acid dimers in the binary (h<sub>2</sub>so<sub>4</sub>–h<sub>2</sub>o) and ternary (h<sub>2</sub>so<sub>4</sub>–h<sub>2</sub>o–nh<sub>3</sub>) system
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2015-09-01
description Sulfuric acid is an important gas influencing atmospheric new particle formation (NPF). Both the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) system and the ternary system involving ammonia (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) may be important in the free troposphere. An essential step in the nucleation of aerosol particles from gas-phase precursors is the formation of a dimer, so an understanding of the thermodynamics of dimer formation over a wide range of atmospheric conditions is essential to describe NPF. We have used the CLOUD chamber to conduct nucleation experiments for these systems at temperatures from 208 to 248 K. Neutral monomer and dimer concentrations of sulfuric acid were measured using a chemical ionization mass spectrometer (CIMS). From these measurements, dimer evaporation rates in the binary system were derived for temperatures of 208 and 223 K. We compare these results to literature data from a previous study that was conducted at higher temperatures but is in good agreement with the present study. For the ternary system the formation of H<sub>2</sub>SO<sub>4</sub>·NH<sub>3</sub> is very likely an essential step in the formation of sulfuric acid dimers, which were measured at 210, 223, and 248 K. We estimate the thermodynamic properties (d<i>H</i> and d<i>S</i>) of the H<sub>2</sub>SO<sub>4</sub>·NH<sub>3</sub> cluster using a simple heuristic model and the measured data. Furthermore, we report the first measurements of large neutral sulfuric acid clusters containing as many as 10 sulfuric acid molecules for the binary system using chemical ionization–atmospheric pressure interface time-of-flight (CI-APi-TOF) mass spectrometry.
url http://www.atmos-chem-phys.net/15/10701/2015/acp-15-10701-2015.pdf
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spelling doaj-846a76561268477ab7186ecbb4852fa92020-11-25T01:00:40ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-09-011518107011072110.5194/acp-15-10701-2015Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) systemA. Kürten0S. Münch1L. Rondo2F. Bianchi3J. Duplissy4T. Jokinen5H. Junninen6N. Sarnela7S. Schobesberger8M. Simon9M. Sipilä10J. Almeida11A. Amorim12J. Dommen13N. M. Donahue14E. M. Dunne15R. C. Flagan16A. Franchin17J. Kirkby18A. Kupc19V. Makhmutov20T. Petäjä21A. P. Praplan22F. Riccobono23G. Steiner24A. Tomé25G. Tsagkogeorgas26P. E. Wagner27D. Wimmer28U. Baltensperger29M. Kulmala30D. R. Worsnop31J. Curtius32Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, Frankfurt am Main, GermanyInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, Frankfurt am Main, GermanyInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, Frankfurt am Main, GermanyLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, SwitzerlandCERN (European Organization for Nuclear Research), Geneva, SwitzerlandDepartment of Physics, University of Helsinki, Helsinki, FinlandDepartment of Physics, University of Helsinki, Helsinki, FinlandDepartment of Physics, University of Helsinki, Helsinki, FinlandDepartment of Physics, University of Helsinki, Helsinki, FinlandInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, Frankfurt am Main, GermanyDepartment of Physics, University of Helsinki, Helsinki, FinlandCERN (European Organization for Nuclear Research), Geneva, SwitzerlandLaboratory for Systems, Instrumentation, and Modeling in Science and Technology for Space and the Environment (SIM), University of Lisbon and University of Beira Interior, Lisbon, PortugalLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, SwitzerlandCenter for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, USASchool of Earth and Environment, University of Leeds, Leeds, UKDivision of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, USADepartment of Physics, University of Helsinki, Helsinki, FinlandInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, Frankfurt am Main, GermanyAerosol Physics and Environmental Physics, University of Vienna, Vienna, AustriaSolar and Cosmic Ray Research Laboratory, Lebedev Physical Institute, Moscow, RussiaDepartment of Physics, University of Helsinki, Helsinki, FinlandLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, SwitzerlandLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, SwitzerlandDepartment of Physics, University of Helsinki, Helsinki, FinlandLaboratory for Systems, Instrumentation, and Modeling in Science and Technology for Space and the Environment (SIM), University of Lisbon and University of Beira Interior, Lisbon, PortugalLeibniz Institute for Tropospheric Research, Leipzig, GermanyAerosol Physics and Environmental Physics, University of Vienna, Vienna, AustriaInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, Frankfurt am Main, GermanyLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, SwitzerlandDepartment of Physics, University of Helsinki, Helsinki, FinlandDepartment of Physics, University of Helsinki, Helsinki, FinlandInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt am Main, Frankfurt am Main, GermanySulfuric acid is an important gas influencing atmospheric new particle formation (NPF). Both the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) system and the ternary system involving ammonia (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) may be important in the free troposphere. An essential step in the nucleation of aerosol particles from gas-phase precursors is the formation of a dimer, so an understanding of the thermodynamics of dimer formation over a wide range of atmospheric conditions is essential to describe NPF. We have used the CLOUD chamber to conduct nucleation experiments for these systems at temperatures from 208 to 248 K. Neutral monomer and dimer concentrations of sulfuric acid were measured using a chemical ionization mass spectrometer (CIMS). From these measurements, dimer evaporation rates in the binary system were derived for temperatures of 208 and 223 K. We compare these results to literature data from a previous study that was conducted at higher temperatures but is in good agreement with the present study. For the ternary system the formation of H<sub>2</sub>SO<sub>4</sub>·NH<sub>3</sub> is very likely an essential step in the formation of sulfuric acid dimers, which were measured at 210, 223, and 248 K. We estimate the thermodynamic properties (d<i>H</i> and d<i>S</i>) of the H<sub>2</sub>SO<sub>4</sub>·NH<sub>3</sub> cluster using a simple heuristic model and the measured data. Furthermore, we report the first measurements of large neutral sulfuric acid clusters containing as many as 10 sulfuric acid molecules for the binary system using chemical ionization–atmospheric pressure interface time-of-flight (CI-APi-TOF) mass spectrometry.http://www.atmos-chem-phys.net/15/10701/2015/acp-15-10701-2015.pdf