The roles of sulfuric acid in new particle formation and growth in the mega-city of Beijing

dc.bibliographicCitation.firstPage4953eng
dc.bibliographicCitation.issue10eng
dc.bibliographicCitation.lastPage4960eng
dc.bibliographicCitation.volume10
dc.contributor.authorYue, D.L.
dc.contributor.authorHu, M.
dc.contributor.authorZhang, R.Y.
dc.contributor.authorWang, Z.B.
dc.contributor.authorZheng, J.
dc.contributor.authorWu, Z.J.
dc.contributor.authorWiedensohler, A.
dc.contributor.authorHe, L.Y.
dc.contributor.authorHuang, X.F.
dc.contributor.authorZhu, T.
dc.date.accessioned2017-11-06T18:30:09Z
dc.date.available2019-06-26T17:17:05Z
dc.date.issued2010
dc.description.abstractSimultaneous measurements of gaseous sulfuric acid and particle number size distributions were performed to investigate aerosol nucleation and growth during CAREBeijing-2008. The analysis of the measured aerosols and sulfuric acid with an aerosol dynamic model shows the dominant role of sulfuric acid in new particle formation (NPF) process but also in the subsequent growth in Beijing. Based on the data of twelve NPF events, the average formation rates (2–13 cm−3 s−1) show a linear correlation with the sulfuric acid concentrations (R2=0.85). Coagulation seems to play a significant role in reducing the number concentration of nucleation mode particles with the ratio of the coagulation loss to formation rate being 0.41±0.16. The apparent growth rates vary from 3 to 11 nm h−1. Condensation of sulfuric acid and its subsequent neutralization by ammonia and coagulation contribute to the apparent particle growth on average 45±18% and 34±17%, respectively. The 30% higher concentration of sulfate than organic compounds in particles during the seven sulfur-rich NPF events but 20% lower concentration of sulfate during the five sulfur-poor type suggest that organic compounds are an important contributor to the growth of the freshly nucleated particles, especially during the sulfur-poor cases.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1359
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/276
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/acp-10-4953-2010
dc.relation.ispartofseriesAtmospheric Chemistry and Physics, Volume 10, Issue 10, Page 4953-4960eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subject.ddc550eng
dc.titleThe roles of sulfuric acid in new particle formation and growth in the mega-city of Beijingeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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