The role of ions in new particle formation in the CLOUD chamber

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Wagner , R , Yan , C , Lehtipalo , K , Duplissy , J , Nieminen , T , Kangasluoma , J , Ahonen , L R , Dada , L , Kontkanen , J , Manninen , H E , Dias , A , Amorim , A , Bauer , P S , Bergen , A , Bernhammer , A-K , Bianchi , F , Brilke , S , Mazon , S B , Chen , X , Draper , D C , Fischer , L , Frege , C , Fuchs , C , Garmash , O , Gordon , H , Hakala , J , Heikkinen , L , Heinritzi , M , Hofbauer , V , Hoyle , C R , Kirkby , J , Kurten , A , Kvashnin , A N , Laurila , T , Lawler , M J , Mai , H , Makhmutov , V , Mauldin III , R L , Molteni , U , Nichman , L , Nie , W , Ojdanic , A , Onnela , A , Piel , F , Quelever , L L J , Rissanen , M P , Sarnela , N , Schallhart , S , Sengupta , K , Simon , M , Stolzenburg , D , Stozhkov , Y , Trostl , J , Viisanen , Y , Vogel , A L , Wagner , A C , Xiao , M , Ye , P , Baltensperger , U , Curtius , J , Donahue , N M , Flagan , R C , Gallagher , M , Hansel , A , Smith , J N , Tome , A , Winkler , P M , Worsnop , D , Ehn , M , Sipilä , M , Kerminen , V-M , Petäjä , T & Kulmala , M 2017 , ' The role of ions in new particle formation in the CLOUD chamber ' , Atmospheric Chemistry and Physics , vol. 17 , no. 24 , pp. 15181-15197 . https://doi.org/10.5194/acp-17-15181-2017

Title: The role of ions in new particle formation in the CLOUD chamber
Author: Wagner, Robert; Yan, Chao; Lehtipalo, Katrianne; Duplissy, Jonathan; Nieminen, Tuomo; Kangasluoma, Juha; Ahonen, Lauri R.; Dada, Lubna; Kontkanen, Jenni; Manninen, Hanna E.; Dias, Antonio; Amorim, Antonio; Bauer, Paulus S.; Bergen, Anton; Bernhammer, Anne-Kathrin; Bianchi, Federico; Brilke, Sophia; Mazon, Stephany Buenrostro; Chen, Xuemeng; Draper, Danielle C.; Fischer, Lukas; Frege, Carla; Fuchs, Claudia; Garmash, Olga; Gordon, Hamish; Hakala, Jani; Heikkinen, Liine; Heinritzi, Martin; Hofbauer, Victoria; Hoyle, Christopher R.; Kirkby, Jasper; Kurten, Andreas; Kvashnin, Alexander N.; Laurila, Tiia; Lawler, Michael J.; Mai, Huajun; Makhmutov, Vladimir; Mauldin III, Roy L.; Molteni, Ugo; Nichman, Leonid; Nie, Wei; Ojdanic, Andrea; Onnela, Antti; Piel, Felix; Quelever, Lauriane L. J.; Rissanen, Matti P.; Sarnela, Nina; Schallhart, Simon; Sengupta, Kamalika; Simon, Mario; Stolzenburg, Dominik; Stozhkov, Yuri; Trostl, Jasmin; Viisanen, Yrjö; Vogel, Alexander L.; Wagner, Andrea C.; Xiao, Mao; Ye, Penglin; Baltensperger, Urs; Curtius, Joachim; Donahue, Neil M.; Flagan, Richard C.; Gallagher, Martin; Hansel, Armin; Smith, James N.; Tome, Antonio; Winkler, Paul M.; Worsnop, Douglas; Ehn, Mikael; Sipilä, Mikko; Kerminen, Veli-Matti; Petäjä, Tuukka; Kulmala, Markku
Contributor organization: Department of Physics
Helsinki Institute of Physics
Polar and arctic atmospheric research (PANDA)
Date: 2017-12-21
Language: eng
Number of pages: 17
Belongs to series: Atmospheric Chemistry and Physics
ISSN: 1680-7316
DOI: https://doi.org/10.5194/acp-17-15181-2017
URI: http://hdl.handle.net/10138/230848
Abstract: The formation of secondary particles in the atmosphere accounts for more than half of global cloud condensation nuclei. Experiments at the CERN CLOUD (Cosmics Leaving OUtdoor Droplets) chamber have underlined the importance of ions for new particle formation, but quantifying their effect in the atmosphere remains challenging. By using a novel instrument setup consisting of two nanoparticle counters, one of them equipped with an ion filter, we were able to further investigate the ion-related mechanisms of new particle formation. In autumn 2015, we carried out experiments at CLOUD on four systems of different chemical compositions involving monoterpenes, sulfuric acid, nitrogen oxides, and ammonia. We measured the influence of ions on the nucleation rates under precisely controlled and atmospherically relevant conditions. Our results indicate that ions enhance the nucleation process when the charge is necessary to stabilize newly formed clusters, i.e., in conditions in which neutral clusters are unstable. For charged clusters that were formed by ion-induced nucleation, we were able to measure, for the first time, their progressive neutralization due to recombination with oppositely charged ions. A large fraction of the clusters carried a charge at 1.5 nm diameter. However, depending on particle growth rates and ion concentrations, charged clusters were largely neutralized by ion-ion recombination before they grew to 2.5 nm. At this size, more than 90% of particles were neutral. In other words, particles may originate from ion-induced nucleation, although they are neutral upon detection at diameters larger than 2.5 nm. Observations at Hyytiala, Finland, showed lower ion concentrations and a lower contribution of ion-induced nucleation than measured at CLOUD under similar conditions. Although this can be partly explained by the observation that ion-induced fractions decrease towards lower ion concentrations, further investigations are needed to resolve the origin of the discrepancy.
Subject: ATMOSPHERIC AEROSOL NUCLEATION
GALACTIC COSMIC-RAYS
SULFURIC-ACID
MOLECULAR CLUSTERS
NEUTRAL CLUSTER
SIZE MAGNIFIER
BOREAL-FOREST
GROWTH-RATES
HETEROGENEOUS NUCLEATION
FREE TROPOSPHERE
114 Physical sciences
Peer reviewed: Yes
Rights: cc_by
Usage restriction: openAccess
Self-archived version: publishedVersion


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