| Literature DB >> 25288761 |
Andreas Kürten1, Tuija Jokinen2, Mario Simon3, Mikko Sipilä4, Nina Sarnela2, Heikki Junninen2, Alexey Adamov2, João Almeida5, Antonio Amorim6, Federico Bianchi7, Martin Breitenlechner8, Josef Dommen7, Neil M Donahue9, Jonathan Duplissy10, Sebastian Ehrhart5, Richard C Flagan11, Alessandro Franchin2, Jani Hakala2, Armin Hansel8, Martin Heinritzi12, Manuel Hutterli13, Juha Kangasluoma2, Jasper Kirkby5, Ari Laaksonen14, Katrianne Lehtipalo15, Markus Leiminger3, Vladimir Makhmutov16, Serge Mathot17, Antti Onnela17, Tuukka Petäjä2, Arnaud P Praplan2, Francesco Riccobono7, Matti P Rissanen2, Linda Rondo3, Siegfried Schobesberger2, John H Seinfeld11, Gerhard Steiner18, António Tomé6, Jasmin Tröstl7, Paul M Winkler19, Christina Williamson3, Daniela Wimmer20, Penglin Ye9, Urs Baltensperger7, Kenneth S Carslaw21, Markku Kulmala4, Douglas R Worsnop22, Joachim Curtius3.
Abstract
For atmospheric sulfuric acid (SA) concentrations the presence of dimethylamine (DMA) at mixing ratios of several parts per trillion by volume can explain observed boundary layer new particle formation rates. However, the concentration and molecular composition of the neutral (uncharged) clusters have not been reported so far due to the lack of suitable instrumentation. Here we report on experiments from the Cosmics Leaving Outdoor Droplets chamber at the European Organization for Nuclear Research revealing the formation of neutral particles containing up to 14 SA and 16 DMA molecules, corresponding to a mobility diameter of about 2 nm, under atmospherically relevant conditions. These measurements bridge the gap between the molecular and particle perspectives of nucleation, revealing the fundamental processes involved in particle formation and growth. The neutral clusters are found to form at or close to the kinetic limit where particle formation is limited only by the collision rate of SA molecules. Even though the neutral particles are stable against evaporation from the SA dimer onward, the formation rates of particles at 1.7-nm size, which contain about 10 SA molecules, are up to 4 orders of magnitude smaller compared with those of the dimer due to coagulation and wall loss of particles before they reach 1.7 nm in diameter. This demonstrates that neither the atmospheric particle formation rate nor its dependence on SA can simply be interpreted in terms of cluster evaporation or the molecular composition of a critical nucleus.Entities:
Keywords: aerosol particles; atmospheric chemistry; atmospheric nucleation; mass spectrometry
Year: 2014 PMID: 25288761 PMCID: PMC4210346 DOI: 10.1073/pnas.1404853111
Source DB: PubMed Journal: Proc Natl Acad Sci U S A ISSN: 0027-8424 Impact factor: 11.205