Measurements of PM10 ions and trace gases with the online system MARGA at the research station Melpitz in Germany – A five-year study

dc.bibliographicCitation.date2018
dc.bibliographicCitation.firstPage33
dc.bibliographicCitation.issue1
dc.bibliographicCitation.journalTitleJournal of Atmospheric Chemistryeng
dc.bibliographicCitation.lastPage70
dc.bibliographicCitation.volume75
dc.contributor.authorStieger, B.
dc.contributor.authorSpindler, G.
dc.contributor.authorFahlbusch, B.
dc.contributor.authorMüller, K.
dc.contributor.authorGrüner, A.
dc.contributor.authorPoulain, L.
dc.contributor.authorThöni, L.
dc.contributor.authorSeitler, E.
dc.contributor.authorWallasch, M.
dc.contributor.authorHerrmann, H.
dc.date.accessioned2023-01-27T09:31:11Z
dc.date.available2023-01-27T09:31:11Z
dc.date.issued2017
dc.description.abstractAn hourly quantification of inorganic water-soluble PM10 ions and corresponding trace gases was performed using the Monitor for AeRosols and Gases in ambient Air (MARGA) at the TROPOS research site in Melpitz, Germany. The data availability amounts to over 80% for the five-year measurement period from 2010 to 2014. Comparisons were performed for the evaluation of the MARGA, resulting in coefficients of determinations (slopes) of 0.91 (0.90) for the measurements against the SO2 gas monitor, 0.84 (0.88), 0.79 (1.39), 0.85 (1.20) for the ACSM NO3 −, SO4 2− and NH4 + measurements, respectively, and 0.85 (0.65), 0.88 (0.68), 0.91 (0.83), 0.86 (0.82) for the filter measurements of Cl−, NO3 −, SO4 2− and NH4 +, respectively. A HONO comparison with a batch denuder shows large scatter (R2 = 0.41). The MARGA HNO3 is underestimated compared to a batch and coated denuder with shorter inlets (slopes of 0.16 and 0.08, respectively). Less NH3 was observed in coated denuders for high ambient concentrations. Long-time measurements show clear daily and seasonal variabilities. Potential Source Contribution Function (PSCF) analysis indicates the emission area of particulate ions Cl−, NO3 −, SO4 2−, NH4 +, K+ and gaseous SO2 to lie in eastern European countries, predominantly in wintertime. Coarse mode sea salt particles are transported from the North Sea to Melpitz. The particles at Melpitz are nearly neutralised with a mean molar ratio of 0.90 for the five-year study. A slight increase of the neutralization ratio over the last three years indicates a stronger decrease of the anthropogenically emitted NO3 − and SO4 2− compared to NH4 +.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11127
dc.identifier.urihttp://dx.doi.org/10.34657/10153
dc.language.isoeng
dc.publisherDordrecht : Springer
dc.relation.doihttps://doi.org/10.1007/s10874-017-9361-0
dc.relation.essn1573-0662
dc.relation.issn0167-7764
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subject.ddc550
dc.subject.ddc540
dc.subject.otherAcidity investigationeng
dc.subject.otherAtmospheric long-term measurementseng
dc.subject.otherInstrument comparisoneng
dc.subject.otherMARGAeng
dc.subject.otherSource apportionmenteng
dc.subject.otherTemporal variationeng
dc.titleMeasurements of PM10 ions and trace gases with the online system MARGA at the research station Melpitz in Germany – A five-year studyeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.subjectChemieger
wgl.typeZeitschriftenartikelger
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