Hydroxymethanesulfonic acid in size-segregated aerosol particles at nine sites in Germany

dc.bibliographicCitation.firstPage4531eng
dc.bibliographicCitation.issue9eng
dc.bibliographicCitation.lastPage4538eng
dc.bibliographicCitation.volume14
dc.contributor.authorScheinhardt, S.
dc.contributor.authorvan Pinxteren, D.
dc.contributor.authorMüller, K.
dc.contributor.authorSpindler, G.
dc.contributor.authorHerrmann, H.
dc.date.accessioned2017-11-29T21:02:11Z
dc.date.available2019-06-26T17:19:33Z
dc.date.issued2014
dc.description.abstractIn the course of two field campaigns, size-segregated particle samples were collected at nine sites in Germany, including traffic, urban, rural, marine and mountain sites. During the chemical characterisation of the samples some of them were found to contain an unknown substance that was later identified as hydroxymethanesulfonic acid (HMSA). HMSA is known to be formed during the reaction of S(IV) (HSO3− or SO32−) with formaldehyde in the aqueous phase. Due to its stability, HMSA can act as a reservoir species for S(IV) in the atmosphere and is therefore of interest for the understanding of atmospheric sulfur chemistry. However, no HMSA data are available for atmospheric particles from central Europe, and even on a worldwide scale data are scarce. Thus, the present study now provides a representative data set with detailed information on HMSA concentrations in size-segregated central European aerosol particles. HMSA mass concentrations in this data set were highly variable: HMSA was found in 224 out of 738 samples (30%), sometimes in high mass concentrations exceeding those of oxalic acid. On average over all 154 impactor runs, 31.5 ng m−3 HMSA was found in PM10, contributing 0.21% to the total mass. The results show that the particle diameter, the sampling location, the sampling season and the air mass origin impact the HMSA mass concentration. Highest concentrations were found in the particle fraction 0.42–1.2 μm, at urban sites, in winter and with eastern (continental) air masses, respectively. The results suggest that HMSA is formed during aging of pollution plumes. A positive correlation of HMSA with sulfate, oxalate and PM is found (R2 > 0.4). The results furthermore suggest that the fraction of HMSA in PM slightly decreases with increasing pH.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1004
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/692
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/acp-14-4531-2014
dc.relation.ispartofseriesAtmospheric Chemistry and Physics, Volume 14, Issue 9, Page 4531-4538eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectaerosoleng
dc.subjectconcentration (composition)eng
dc.subjectformaldehydeeng
dc.subjectoxalic acideng
dc.subjectparticle sizeeng
dc.subjectparticulate mattereng
dc.subjectsulfureng
dc.subject.ddc550eng
dc.titleHydroxymethanesulfonic acid in size-segregated aerosol particles at nine sites in Germanyeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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