Ion-induced nucleation of pure biogenic particles

dc.bibliographicCitation.firstPage521
dc.bibliographicCitation.lastPage526
dc.bibliographicCitation.volume533
dc.contributor.authorKirkby, Jasper
dc.contributor.authorDuplissy, Jonathan
dc.contributor.authorSengupta, Kamalika
dc.contributor.authorGordon, Hamish
dc.contributor.authorWilliamson, Christina
dc.contributor.authorHeinritzi, Martin
dc.contributor.authorSimon, Mario
dc.contributor.authorYan, Chao
dc.contributor.authorAlmeida, João
dc.contributor.authorTröstl, Jasmin
dc.contributor.authorNieminen, Tuomo
dc.contributor.authorOrtega, Ismael K.
dc.contributor.authorWagner, Robert
dc.contributor.authorAdamov, Alexey
dc.contributor.authorAmorim, Antonio
dc.contributor.authorBernhammer, Anne-Kathrin
dc.contributor.authorBianchi, Federico
dc.contributor.authorBreitenlechner, Martin
dc.contributor.authorBrilke, Sophia
dc.contributor.authorChen, Xuemeng
dc.contributor.authorCraven, Jill
dc.contributor.authorDias, Antonio
dc.contributor.authorEhrhart, Sebastian
dc.contributor.authorFlagan, Richard C.
dc.contributor.authorFranchin, Alessandro
dc.contributor.authorFuchs, Claudia
dc.contributor.authorGuida, Roberto
dc.contributor.authorHakala, Jani
dc.contributor.authorHoyle, Christopher R.
dc.contributor.authorJokinen, Tuija
dc.contributor.authorJunninen, Heikki
dc.contributor.authorKangasluoma, Juha
dc.contributor.authorKim, Jaeseok
dc.contributor.authorKrapf, Manuel
dc.contributor.authorKürten, Andreas
dc.contributor.authorLaaksonen, Ari
dc.contributor.authorLehtipalo, Katrianne
dc.contributor.authorMakhmutov, Vladimir
dc.contributor.authorMathot, Serge
dc.contributor.authorMolteni, Ugo
dc.contributor.authorOnnela, Antti
dc.contributor.authorPeräkylä, Otso
dc.contributor.authorPiel, Felix
dc.contributor.authorPetäjä, Tuukka
dc.contributor.authorPraplan, Arnaud P.
dc.contributor.authorPringle, Kirsty
dc.contributor.authorRap, Alexandru
dc.contributor.authorRichards, Nigel A.D.
dc.contributor.authorRiipinen, Ilona
dc.contributor.authorRissanen, Matti P.
dc.contributor.authorRondo, Linda
dc.contributor.authorSarnela, Nina
dc.contributor.authorSchobesberger, Siegfried
dc.contributor.authorScott, Catherine E.
dc.contributor.authorSeinfeld, John H.
dc.contributor.authorSipilä, Mikko
dc.contributor.authorSteiner, Gerhard
dc.contributor.authorStozhkov, Yuri
dc.contributor.authorStratmann, Frank
dc.contributor.authorTomé, Antonio
dc.contributor.authorVirtanen, Annele
dc.contributor.authorVogel, Alexander L.
dc.contributor.authorWagner, Andrea C.
dc.contributor.authorWagner, Paul E.
dc.contributor.authorWeingartner, Ernest
dc.contributor.authorWimmer, Daniela
dc.contributor.authorWinkler, Paul M.
dc.contributor.authorYe, Penglin
dc.contributor.authorZhang, Xuan
dc.contributor.authorHansel, Armin
dc.contributor.authorDommen, Josef
dc.contributor.authorDonahue, Neil M.
dc.contributor.authorWorsnop, Douglas R.
dc.contributor.authorBaltensperger, Urs
dc.contributor.authorKulmala, Markku
dc.contributor.authorCarslaw, Kenneth S.
dc.contributor.authorCurtius, Joachim
dc.date.accessioned2018-01-31T06:44:50Z
dc.date.available2019-06-26T17:21:27Z
dc.date.issued2016
dc.description.abstractAtmospheric aerosols and their effect on clouds are thought to be important for anthropogenic radiative forcing of the climate, yet remain poorly understood1. Globally, around half of cloud condensation nuclei originate from nucleation of atmospheric vapours2. It is thought that sulfuric acid is essential to initiate most particle formation in the atmosphere3,4, and that ions have a relatively minor role5. Some laboratory studies, however, have reported organic particle formation without the intentional addition of sulfuric acid, although contamination could not be excluded6,7. Here we present evidence for the formation of aerosol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a large chamber under atmospheric conditions. The highly oxygenated molecules (HOMs) are produced by ozonolysis of α-pinene. We find that ions from Galactic cosmic rays increase the nucleation rate by one to two orders of magnitude compared with neutral nucleation. Our experimental findings are supported by quantum chemical calculations of the cluster binding energies of representative HOMs. Ion-induced nucleation of pure organic particles constitutes a potentially widespread source of aerosol particles in terrestrial environments with low sulfuric acid pollution.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1067
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/862
dc.language.isoengeng
dc.publisherLondon : Nature Publishing Groupeng
dc.relation.doihttps://doi.org/10.1038/nature17953
dc.relation.ispartofseriesNature Letter, Volume 533, Page 521-526eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectAtmospheric chemistryeng
dc.subjectClimate-change impactseng
dc.subject.ddc550eng
dc.titleIon-induced nucleation of pure biogenic particleseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleNature Lettereng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
Files
Original bundle
Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
nature17953.pdf
Size:
3.88 MB
Format:
Adobe Portable Document Format
Description: