4.8 Article

Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions

Publisher

NATL ACAD SCIENCES
DOI: 10.1073/pnas.1404853111

Keywords

aerosol particles; atmospheric nucleation; atmospheric chemistry; mass spectrometry

Funding

  1. European Center for Nuclear Research (CERN)
  2. European Commission [215072, 316662]
  3. European Research Council (ERC)-Starting MOCAPAF Grant [57360]
  4. ERC-Advanced ATMNUCLE Grant [227463]
  5. German Federal Ministry of Education and Research [01LK0902A, 01LK1222A]
  6. Swiss National Science Foundation [200020 135307, 206620 141278]
  7. Academy of Finland [135054, 133872, 251427, 139656, 139995, 137749, 141217, 141451, 1118615]
  8. Finnish Funding Agency for Technology and Innovation
  9. Vaisala Foundation
  10. Nessling Foundation
  11. Austrian Science Fund [J3198-N21]
  12. Portuguese Foundation for Science and Technology [CERN/FP/116387/2010]
  13. Swedish Research Council
  14. Vetenskapsradet [2011-5120]
  15. Presidium of the Russian Academy of Sciences
  16. Russian Foundation for Basic Research [08-02-91006-CERN, 12-02-91522-CERN]
  17. US National Science Foundation [AGS1136479, CHE1012293]
  18. Pan-European Gas-Aerosols-Climate Interaction Study project - European Commission under the Framework Program 7 [FP7-ENV-2010-265148]
  19. Davidow Foundation
  20. Swiss National Science Foundation (SNF) [206620_141278] Funding Source: Swiss National Science Foundation (SNF)

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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.

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