Evaluation on the role of sulfuric acid in the mechanisms of new particle formation for Beijing case

dc.bibliographicCitation.firstPage12663eng
dc.bibliographicCitation.issue24eng
dc.bibliographicCitation.lastPage12671eng
dc.bibliographicCitation.volume11
dc.contributor.authorWang, Z.B.
dc.contributor.authorHu, M.
dc.contributor.authorYue, D.L.
dc.contributor.authorZheng, J.
dc.contributor.authorZhang, R.Y.
dc.contributor.authorWiedensohler, A.
dc.contributor.authorWu, Z.J.
dc.contributor.authorNieminen, T.
dc.contributor.authorBoy, M.
dc.date.accessioned2017-11-09T18:30:55Z
dc.date.available2019-06-26T17:17:47Z
dc.date.issued2011
dc.description.abstractNew particle formation (NPF) is considered as an important mechanism for gas-to-particle transformation, and gaseous sulfuric acid is believed as a crucial precursor. Up to now few field-based studies on nucleation mechanisms and the role of sulfuric acid were conducted in China. In this study, simultaneously measurements of particle number size distributions and gaseous sulfuric acid concentrations were performed from July to September in 2008. Totally, 22 new particle formation events were observed during the entire 85 campaign days. The results show that in the case of both higher source and sink values, the result of the competition between source and sink is more likely the key limiting factor to determine the observation of NPF events in Beijing. The concentrations of gaseous sulfuric acid show good correlations with freshly nucleated particles (N3-6 and formation rates (J3 and J1.5. The power-law relationship between H2SO4 concentration and N3-6 or J is adopted to explore the nucleation mechanism. The exponents are showed a great range (from 1 to 7). More than half of the NPF events exhibit an exponent larger than 2.5. For these cases, the thermodynamic process works better than the activation or kinetic nucleation theories to explain the nucleation events in urban atmosphere of Beijing.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/941
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/467
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/acp-11-12663-2011
dc.relation.ispartofseriesAtmospheric Chemistry and Physics, Volume 11, Issue 24, Page 12663-12671eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectaerosoleng
dc.subjectaerosol compositioneng
dc.subjectconcentration (composition)eng
dc.subjectformation mechanismeng
dc.subjectparticle sizeeng
dc.subjectpower laweng
dc.subjectsize distributioneng
dc.subjectsulfuric acideng
dc.subjectthermodynamicseng
dc.subject.ddc550eng
dc.titleEvaluation on the role of sulfuric acid in the mechanisms of new particle formation for Beijing caseeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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