4.8 Article

The effect of acid-base clustering and ions on the growth of atmospheric nano-particles

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NATURE COMMUNICATIONS
卷 7, 期 -, 页码 -

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NATURE PUBLISHING GROUP
DOI: 10.1038/ncomms11594

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资金

  1. CERN
  2. European Union [656994]
  3. German Federal Ministry of Education and Research [01LK0902A, 01LK1222A]
  4. Swiss National Science Foundation [206621_125025, 206620_130527]
  5. Academy of Finland [251427, 1133872, 138951]
  6. Academy of Finland Center of Excellence program [1118615, 272041]
  7. Austrian Science Fund (FWF) [P19546, L593]
  8. Portuguese Foundation for Science and Technology [CERN/FP/116387/2010]
  9. Swedish Research Council [2011-5120]
  10. Russian Foundation for Basic Research [N08-02-91006-CERN]
  11. US National Science Foundation [AGS1136479, CHE1012293]
  12. US Department of Energy [DE-SC00014469]
  13. Vaisala foundation
  14. EC Seventh Framework Programme (Marie Curie Initial Training Network 'CLOUD-ITN') [215072]
  15. EC Seventh Framework Programme (Marie Curie Initial Training Network 'CLOUD-TRAIN') [316662]
  16. EC Seventh Framework Programme (ERC grant 'ATMOGAIN') [278277]
  17. EC Seventh Framework Programme (ERC grant 'MOCAPAF' [257360]
  18. EC Seventh Framework Programme (ERC grant 'NANODYNAMITE') [616075]
  19. EC Seventh Framework Programme (ERC grant 'ATMNUCLE') [227463]
  20. EC [FP7-ENV-2010-265148]
  21. Swiss National Science Foundation (SNF) [206621_125025] Funding Source: Swiss National Science Foundation (SNF)
  22. Academy of Finland (AKA) [138951, 138951] Funding Source: Academy of Finland (AKA)

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The growth of freshly formed aerosol particles can be the bottleneck in their survival to cloud condensation nuclei. It is therefore crucial to understand how particles grow in the atmosphere. Insufficient experimental data has impeded a profound understanding of nano-particle growth under atmospheric conditions. Here we study nano-particle growth in the CLOUD (Cosmics Leaving OUtdoors Droplets) chamber, starting from the formation of molecular clusters. We present measured growth rates at sub-3 nm sizes with different atmospherically relevant concentrations of sulphuric acid, water, ammonia and dimethylamine. We find that atmospheric ions and small acid-base clusters, which are not generally accounted for in the measurement of sulphuric acid vapour, can participate in the growth process, leading to enhanced growth rates. The availability of compounds capable of stabilizing sulphuric acid clusters governs the magnitude of these effects and thus the exact growth mechanism. We bring these observations into a coherent framework and discuss their significance in the atmosphere.

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