Contribution of sulfuric acid and oxidized organic compounds to particle formation and growth

dc.contributor.authorRiccobono, Francesco
dc.contributor.authorRondo, Linda
dc.contributor.authorSipilä, Mikko
dc.contributor.authorBarmet, Peter
dc.contributor.authorCurtius, Joachim
dc.contributor.authorDommen, Josef
dc.contributor.authorEhn, Mikael
dc.contributor.authorEhrhart, Sebastian
dc.contributor.authorKulmala, Markku
dc.contributor.authorKürten, Andreas
dc.contributor.authorMikkilä, Jyri
dc.contributor.authorPaasonen, Pauli
dc.contributor.authorPetäjä, Tuukka
dc.contributor.authorWeingartner, Ernest
dc.contributor.authorBaltensperger, Urs
dc.date.accessioned2024-06-03T13:48:55Z
dc.date.available2024-06-03T13:48:55Z
dc.date.issued2012
dc.description.abstract<jats:p>Abstract. Lack of knowledge about the mechanisms underlying new particle formation and their subsequent growth is one of the main causes for the large uncertainty in estimating the radiative forcing of atmospheric aerosols in global models. We performed chamber experiments designed to study the contributions of sulfuric acid and organic vapors to the formation and early growth of nucleated particles. Distinct experiments in the presence of two different organic precursors (1,3,5-trimethylbenzene and α-pinene) showed the ability of these compounds to reproduce the formation rates observed in the low troposphere. These results were obtained measuring the sulfuric acid concentrations with two chemical ionization mass spectrometers confirming the results of a previous study which modeled the sulfuric acid concentrations in presence of 1,3,5-trimethylbenzene. New analysis methods were applied to the data collected with a condensation particle counter battery and a scanning mobility particle sizer, allowing the assessment of the size resolved growth rates of freshly nucleated particles. The effect of organic vapors on particle growth was investigated by means of the growth rate enhancement factor (Γ), defined as the ratio between the measured growth rate in the presence of α-pinene and the kinetically limited growth rate of the sulfuric acid and water system. The observed Γ values indicate that the growth is already dominated by organic compounds at particle diameters of 2 nm. Both the absolute growth rates and Γ showed a strong dependence on particle size, supporting the nano-Köhler theory. Moreover, the separation of the contributions from sulfuric acid and organic compounds to particle growth reveals that the organic contribution seems to be enhanced by the sulfuric acid concentration. Finally, the size resolved growth analysis indicates that both condensation of oxidized organic compounds and reactive uptake contribute to particle growth. </jats:p>
dc.identifier.doi10.5194/acp-12-9427-2012
dc.identifier.issn1680-7324
dc.identifier.issn1680-7316
dc.identifier.urihttps://irf.fhnw.ch/handle/11654/45874
dc.identifier.urihttps://doi.org/10.26041/fhnw-9103
dc.issue20
dc.language.isoen
dc.publisherCopernicus
dc.relation.ispartofAtmospheric Chemistry and Physics
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subject.ddc550 - Geowissenschaften
dc.titleContribution of sulfuric acid and oxidized organic compounds to particle formation and growth
dc.type01A - Beitrag in wissenschaftlicher Zeitschrift
dc.volume12
dspace.entity.typePublication
fhnw.InventedHereNo
fhnw.ReviewTypeAnonymous ex ante peer review of a complete publication
fhnw.affiliation.hochschuleHochschule für Technikde_CH
fhnw.affiliation.institutlnstitut für Sensorik und Elektronikde_CH
fhnw.openAccessCategoryGold
fhnw.pagination9427-9439
fhnw.publicationStatePublished
relation.isAuthorOfPublication05dd9a19-7a24-4325-805a-2d121483b168
relation.isAuthorOfPublication.latestForDiscovery05dd9a19-7a24-4325-805a-2d121483b168
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