1. The role of ions in new particle formation in the CLOUD chamber
- Author
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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., Kürten, 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., Quéléver, L. L. J., Rissanen, M. P., Sarnela, N., Schallhart, S., Sengupta, K., Simon, M., Stolzenburg, D., Stozhkov, Y., Tröstl, 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., Tomé, A., Winkler, P. M., Worsnop, D., Ehn, M., Sipilä, M., Kerminen, V.-M., Petäjä, T., Kulmala, M., Department of Physics, Helsinki Institute of Physics, Polar and arctic atmospheric research (PANDA), University of Helsinki, University of Eastern Finland, CERN, University of Lisbon, University of Vienna, Goethe University Frankfurt, University of Innsbruck, University of California Irvine, Paul Scherrer Institute, Department of Applied Physics, Carnegie Mellon University, RAS - P.N. Lebedev Physics Institute, California Institute of Technology, University of Manchester, University of Leeds, Finnish Meteorological Institute, Aalto-yliopisto, Aalto University, and Department of Applied Physics, activities
- Subjects
Atmospheric Science ,010504 meteorology & atmospheric sciences ,Nucleation ,Analytical chemistry ,Nanoparticle ,ATMOSPHERIC AEROSOL NUCLEATION ,Cosmic ray ,010501 environmental sciences ,114 Physical sciences ,01 natural sciences ,Ion ,Atmosphere ,lcsh:Chemistry ,chemistry.chemical_compound ,SULFURIC-ACID ,HETEROGENEOUS NUCLEATION ,ddc:550 ,Cloud condensation nuclei ,Nuclear Physics - Experiment ,ResearchInstitutes_Networks_Beacons/MERI ,BOREAL-FOREST ,0105 earth and related environmental sciences ,FREE TROPOSPHERE ,GROWTH-RATES ,Chemistry ,MOLECULAR CLUSTERS ,Sulfuric acid ,Manchester Environmental Research Institute ,lcsh:QC1-999 ,SIZE MAGNIFIER ,lcsh:QD1-999 ,13. Climate action ,Chemical physics ,Particle ,NEUTRAL CLUSTER ,lcsh:Physics ,GALACTIC COSMIC-RAYS - 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 Hyytiälä, 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., published version, peerReviewed
- Published
- 2017