Journal article

Aerosol dynamics simulations on the connection of sulphuric acid and new particle formation

Sihto S, Vuollekoski H, Leppa J, Riipinen I, Kerminen V, Korhonen H, Lehtinen K, Boy M, Kulmala M ...see all

Atmospheric Chemistry and Physics, vol. 9, issue 9 (2009) pp. 2933-2947

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We have performed a series of simulations with an aerosol dynamics box model to study the connection between new particle formation and sulphuric acid concentration. For nucleation either activation mechanism with a linear dependence on the sulphuric acid concentration, kinetic mechanism with a squared dependence on the sulphuric acid concentration or ternary H(2)O-H(2)SO(4)-NH(3) nucleation was assumed. The aim was to study the factors that affect the sulphuric acid dependence during the early stages of particle growth, and specifically to find conditions which would yield the linear dependence between the particle number concentration at 3-6 nm and sulphuric acid, as observed in field experiments. The simulations showed that the correlation with sulphuric acid may change during the growth from nucleation size to 3-6 nm size range, the main reason being the size dependent growth rate between 1 and 3 nm. In addition, the assumed size for the nucleated clusters had a crucial impact on the sulphuric acid dependence at 3 nm. A linear dependence between the particle number concentration at 3 nm and sulphuric acid was achieved, when activation nucleation mechanism was used with a low saturation vapour pressure for the condensable organic vapour, or with nucleation taking place at similar to 2 nm instead of similar to 1 nm. Simulations with activation, kinetic and ternary nucleation showed that ternary nucleation reproduces too steep dependence on sulphuric acid as compared to the linear or square dependence observed in field measurements.

Author-supplied keywords

  • atmospheric nucleation
  • boreal forest
  • climate
  • growth-rates
  • model
  • nanoparticles
  • parameterization
  • size
  • ternary nucleation
  • water

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  • S L Sihto

  • H Vuollekoski

  • J Leppa

  • I Riipinen

  • V M Kerminen

  • H Korhonen

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