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Dall'Osto M, Beddows DCS, Asmi A, Poulain L, Hao L, Freney E, Allan JD, Canagaratna M, Crippa M, Bianchi F, de Leeuw G, Eriksson A, Swietlicki E, Hansson HC, Henzing JS, Granier C, Zemankova K, Laj P, Onasch T, Prevot A, Putaud JP, Sellegri K, Vidal M, Virtanen A, Simo R, Worsnop D, O'Dowd C, Kulmala M, Harrison RM. Novel insights on new particle formation derived from a pan-european observing system. Sci Rep 2018; 8:1482. [PMID: 29367716 PMCID: PMC5784154 DOI: 10.1038/s41598-017-17343-9] [Citation(s) in RCA: 34] [Impact Index Per Article: 5.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/04/2017] [Accepted: 11/20/2017] [Indexed: 11/10/2022] Open
Abstract
The formation of new atmospheric particles involves an initial step forming stable clusters less than a nanometre in size (<~1 nm), followed by growth into quasi-stable aerosol particles a few nanometres (~1–10 nm) and larger (>~10 nm). Although at times, the same species can be responsible for both processes, it is thought that more generally each step comprises differing chemical contributors. Here, we present a novel analysis of measurements from a unique multi-station ground-based observing system which reveals new insights into continental-scale patterns associated with new particle formation. Statistical cluster analysis of this unique 2-year multi-station dataset comprising size distribution and chemical composition reveals that across Europe, there are different major seasonal trends depending on geographical location, concomitant with diversity in nucleating species while it seems that the growth phase is dominated by organic aerosol formation. The diversity and seasonality of these events requires an advanced observing system to elucidate the key processes and species driving particle formation, along with detecting continental scale changes in aerosol formation into the future.
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Affiliation(s)
- M Dall'Osto
- Institute of Marine Science, Consejo Superior de Investigaciones Científicas (CSIC), Barcelona, Spain. .,National Centre for Atmospheric Science Division of Environmental Health & Risk Management School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom. .,School of Physics, Centre for Climate & Air Pollution Studies, National University of Ireland Galway, University Road Galway, Galway, Ireland. .,Aerodyne Research, Inc., Billerica, MA, USA.
| | - D C S Beddows
- National Centre for Atmospheric Science Division of Environmental Health & Risk Management School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom
| | - A Asmi
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland
| | - L Poulain
- Leibniz Institute for Tropospheric Research, Permoserstr. 15, 04318, Leipzig, Germany
| | - L Hao
- University of Eastern Finland, Department of Applied Physics, P.O.Box 1627, FIN-70211, Kuopio, Finland
| | - E Freney
- Laboratoire de Météorologie Physique, CNRS-Université Blaise Pascal, UMR6016, 63117, Clermont, Ferrand, France
| | - J D Allan
- School of Earth, Atmospheric and Environmental Sciences, The University of Manchester, Manchester, UK
| | | | - M Crippa
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland.,European Commission, Joint Research Centre (JRC), Directorate for Energy, Transport and Climate, Air and Climate Unit, Via E. Fermi 2749, I-21027, Ispra, (VA), Italy
| | - F Bianchi
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland.,Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland
| | - G de Leeuw
- Finnish Meteorological Institute, Climate Change Unit, P.O. Box 503, 00101, Helsinki, Finland.,Netherlands Organisation for Applied Scientific Research TNO, Princetonlaan 6, 3508 TA, Utrecht, The Netherlands
| | - A Eriksson
- Division of Ergonomics and Aerosol Technology, Lund University, Box 118, SE-22100, Lund, Sweden
| | - E Swietlicki
- Division of Nuclear Physics, Lund University, Box 118, SE-22100, Lund, Sweden
| | - H C Hansson
- Department of Environmental Science and Analytical Chemistry, Stockholm University, 10691, Stockholm, Sweden
| | - J S Henzing
- Netherlands Organisation for Applied Scientific Research TNO, Princetonlaan 6, 3508 TA, Utrecht, The Netherlands
| | - C Granier
- Laboratoire d'Aérologie, Toulouse, France.,NOAA Earth System Laboratory and CIRES, University of Colorado, Boulder, USA
| | - K Zemankova
- Charles University, Faculty of Mathematics and Physics, Dept. of Atmospheric Physcis, Prague, Czechia
| | - P Laj
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland.,Univ. Grenoble-Alpes, CNRS, IRD, INPG, Institut des Géosciences de l'Environnement, Grenoble, France.,Univ. Grenoble-Alpes, CNRS, IRD, Observatoire des Sciences de l'Univers, Grenoble, France
| | - T Onasch
- Aerodyne Research, Inc., Billerica, MA, USA
| | - A Prevot
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232, PSI, Villigen, Switzerland
| | - J P Putaud
- European Commission, Joint Research Centre, Institute for Environment and Sustainability, 21027, (VA), Italy
| | - K Sellegri
- Laboratoire de Météorologie Physique, CNRS-Université Blaise Pascal, UMR6016, 63117, Clermont, Ferrand, France
| | - M Vidal
- Department of Evolutionary Biology, Ecology and Environmental Sciences, Universitat de Barcelona, Av. Diagonal 643, 08028, Barcelona, Catalonia, Spain
| | - A Virtanen
- University of Eastern Finland, Department of Applied Physics, P.O.Box 1627, FIN-70211, Kuopio, Finland
| | - R Simo
- Institute of Marine Science, Consejo Superior de Investigaciones Científicas (CSIC), Barcelona, Spain
| | - D Worsnop
- Aerodyne Research, Inc., Billerica, MA, USA.,Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland
| | - C O'Dowd
- School of Physics, Centre for Climate & Air Pollution Studies, National University of Ireland Galway, University Road Galway, Galway, Ireland
| | - M Kulmala
- Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland
| | - Roy M Harrison
- National Centre for Atmospheric Science Division of Environmental Health & Risk Management School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom.,Department of Environmental Sciences / Center of Excellence in Environmental Studies, King Abdulaziz University, PO Box 80203, 21589, Jeddah, Saudi Arabia
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Canagaratna M, Phillips JA, Goodfriend H, Fiacco DL, Ott ME, Harms B, Leopold KR. Structures of the van der Waals Isomers of Halosulfuric Acids: Microwave Spectra of HX-SO3 (X = F, Cl, Br). J Mol Spectrosc 1998; 192:338-347. [PMID: 9831500 DOI: 10.1006/jmsp.1998.7712] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/22/2023]
Abstract
The complexes of SO3 with HF, HCl, and HBr have been studied by microwave spectroscopy. In all three systems, the halogen atom approaches the SO3 on or near its C3 axis, and the vibrationally averaged structure is that of a symmetric top. The S-X bond lengths are 2.655(10), 3.1328(57), and 3.2339(85) Å for the HF, HCl, and HBr complexes, respectively, and in all three systems the out-of-plane distortion of the SO3 is negligible. In HF-SO3, the hydrogen points away from the SO3 and hyperfine structure in the DF complex gives an average angle of 47.7 degrees with respect to the vibrationally averaged C3 axis of the complex. In the HCl and HBr complexes, however, the HX unit is nearly parallel to the SO3 plane. In HCl-SO3, the HCl forms a 72.8 degrees angle with the average C3 axis of the complex, with the proton tilting slightly toward the SO3. In HBr-SO3, the average orientation of the HBr is 73.0 degrees off the symmetry axis of the complex, but the direction of the tilt (toward or away from the SO3) is not determined. Although the hydrogen halides react with SO3 in bulk to produce halosulfuric acids, these gas-phase complexes are much like weakly bound dimers. Copyright 1998 Academic Press.
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Affiliation(s)
- M Canagaratna
- Department of Chemistry, University of Minnesota, 207 Pleasant St., SE, Minneapolis, MN, 55455
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