Evolution of particle composition in CLOUD nucleation experiments

dc.contributor.authorKeskinen, Helmi
dc.contributor.authorVirtanen, Annele
dc.contributor.authorJoutsensaari, Jorma
dc.contributor.authorTsagkogeorgas, Georgios
dc.contributor.authorDuplissy, Jonathan
dc.contributor.authorSchobesberger, Siegfried
dc.contributor.authorGysel, Martin
dc.contributor.authorRiccobono, Francesco
dc.contributor.authorSlowik, Jay Gates
dc.contributor.authorBianchi, Federico
dc.contributor.authorYli-Juuti, Taina
dc.contributor.authorLehtipalo, Katrianne
dc.contributor.authorRondo, Linda
dc.contributor.authorBreitenlechner, Martin
dc.contributor.authorKupc, Agnieszka
dc.contributor.authorAlmeida, João
dc.contributor.authorAmorim, Antonio
dc.contributor.authorDunne, Eimear M.
dc.contributor.authorDownard, Andrew J.
dc.contributor.authorEhrhart, Sebastian
dc.contributor.authorFranchin, Alessandro
dc.contributor.authorKajos, Maija K.
dc.contributor.authorKirkby, Jasper
dc.contributor.authorKürten, Andreas
dc.contributor.authorNieminen, Tuomo
dc.contributor.authorMakhmutov, Vladimir
dc.contributor.authorMathot, Serge
dc.contributor.authorMiettinen, Pasi
dc.contributor.authorOnnela, Antti
dc.contributor.authorPetäjä, Tuukka
dc.contributor.authorPraplan, Arnaud
dc.contributor.authorSantos, Felipe D.
dc.contributor.authorSchallhart, Simon
dc.contributor.authorSipilä, Mikko
dc.contributor.authorStozhkov, Yuri
dc.contributor.authorTomé, Antonio
dc.contributor.authorVaattovaara, Petri
dc.contributor.authorWimmer, Daniela
dc.contributor.authorPrévôt, André
dc.contributor.authorDommen, Josef
dc.contributor.authorDonahue, Neil M.
dc.contributor.authorFlagan, Richard C.
dc.contributor.authorWeingartner, Ernest
dc.contributor.authorViisanen, Yrjö
dc.contributor.authorRiipinen, Ilona
dc.contributor.authorHansel, Armin
dc.contributor.authorCurtius, Joachim
dc.contributor.authorKulmala, Markku
dc.contributor.authorWorsnop, Douglas R.
dc.contributor.authorBaltensperger, Urs
dc.contributor.authorWex, Heike
dc.contributor.authorStratmann, Frank
dc.contributor.authorLaaksonen, Ari
dc.date.accessioned2024-03-18T12:34:35Z
dc.date.available2024-03-18T12:34:35Z
dc.date.issued2013
dc.description.abstractSulphuric acid, ammonia, amines, and oxidised organics play a crucial role in nanoparticle formation in the atmosphere. In this study, we investigate the composition of nucleated nanoparticles formed from these compounds in the CLOUD (Cosmics Leaving Outdoor Droplets) chamber experiments at CERN (Centre européen pour la recherche nucléaire). The investigation was carried out via analysis of the particle hygroscopicity, ethanol affinity, oxidation state, and ion composition. Hygroscopicity was studied by a hygroscopic tandem differential mobility analyser and a cloud condensation nuclei counter, ethanol affinity by an organic differential mobility analyser and particle oxidation level by a high-resolution time-of-flight aerosol mass spectrometer. The ion composition was studied by an atmospheric pressure interface time-of-flight mass spectrometer. The volume fraction of the organics in the particles during their growth from sizes of a few nanometers to tens of nanometers was derived from measured hygroscopicity assuming the Zdanovskii–Stokes–Robinson relationship, and compared to values gained from the spectrometers. The ZSR-relationship was also applied to obtain the measured ethanol affinities during the particle growth, which were used to derive the volume fractions of sulphuric acid and the other inorganics (e.g. ammonium salts). In the presence of sulphuric acid and ammonia, particles with a mobility diameter of 150 nm were chemically neutralised to ammonium sulphate. In the presence of oxidation products of pinanediol, the organic volume fraction of freshly nucleated particles increased from 0.4 to ~0.9, with an increase in diameter from 2 to 63 nm. Conversely, the sulphuric acid volume fraction decreased from 0.6 to 0.1 when the particle diameter increased from 2 to 50 nm. The results provide information on the composition of nucleated aerosol particles during their growth in the presence of various combinations of sulphuric acid, ammonia, dimethylamine and organic oxidation products.
dc.identifier.doi10.5194/acp-13-5587-2013
dc.identifier.issn1680-7324
dc.identifier.issn1680-7316
dc.identifier.urihttps://irf.fhnw.ch/handle/11654/45163
dc.identifier.urihttps://doi.org/10.26041/fhnw-8599
dc.issue11
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.titleEvolution of particle composition in CLOUD nucleation experiments
dc.type01A - Beitrag in wissenschaftlicher Zeitschrift
dc.volume13
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.pagination5587-5600
fhnw.publicationStatePublished
relation.isAuthorOfPublication54997bb8-cf4a-4120-b0c7-f8e731e8eea1
relation.isAuthorOfPublication05dd9a19-7a24-4325-805a-2d121483b168
relation.isAuthorOfPublication.latestForDiscovery54997bb8-cf4a-4120-b0c7-f8e731e8eea1
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