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On the formation, growth and composition of nucleation mode particles
Open accessAbstract
Taking advantage of only the measured aerosol particles spectral evolution as a function of time, a new analytical tool is developed to derive formation and growth properties of nucleation mode aerosols. This method, when used with hygroscopic growth-factors, can also estimate basic composition properties of these recently-formed particles. From size spectra the diameter growth-rate can be obtained, and aerosol condensation and coagulation sinks can be calculated. Using this growth-rate and condensation sink, the concentration of condensable vapours and their source rate can be estimated. Then, combining the coagulation sink together with measured number concentrations and apparent source rates of 3 nm particles, 1 nm particle nucleation rates and concentration can be estimated. To estimate nucleation rates and vapour concentration source rates producing new particle bursts over the Boreal forest regions, three cases from the BIOFOR project were examined using this analytical tool. In this environment, the nucleation mode growth-rate was observed to be 2–3 nm hour−1, which required a condensable vapour concentration of 2.5–4×107 cm−3 and a source rate of approximately 7.5–11×104 cm−3 s−1 to be sustained. The formation rate of 3 nm particles was =1 particle cm−3 s−1 in all three cases. The estimated formation rate of 1 nm particles was 10–100 particles cm−3 s−1, while their concentration was estimated to be between 10,000 and 100,000 particles cm−3. Using hygroscopicity data and mass flux expressions, the mass flux of insoluble vapour is estimated to be of the same order of magnitude as that of soluble vapour, with a soluble to insoluble vapour flux ratio ranging from 0.7 to 1.4 during these nucleation events.
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Citations
Cited by
Measurement of the nucleation of atmospheric aerosol particles
Kulmala, M., Petäjä, T., Nieminen, T., Sipilä, M., Manninen, H. E., Lehtipalo, K., Dal Maso, M., Aalto, P. P., Junninen, H., Paasonen, P., et al. (2012) · Nature Protocols · doi:10.1038/nprot.2012.091 · Cited by 678
Self-citationKerminen, V.-M., & Kulmala, M. (2002) · Journal of Aerosol Science · doi:10.1016/s0021-8502(01)00194-x · Cited by 375
Self-citationA review of the anthropogenic influence on biogenic secondary organic aerosol
Hoyle, C. R., Boy, M., Donahue, N. M., Fry, J. L., Glasius, M., Guenther, A., Hallar, A. G., Huff Hartz, K., Petters, M. D., Petäjä, T., et al. (2011) · Atmospheric Chemistry and Physics · doi:10.5194/acp-11-321-2011 · Cited by 306
Pan-Arctic aerosol number size distributions: seasonality and transport patterns
Freud, E., Krejci, R., Tunved, P., Leaitch, R., Nguyen, Q. T., Massling, A., Skov, H., & Barrie, L. (2017) · Atmospheric Chemistry and Physics · doi:10.5194/acp-17-8101-2017 · Cited by 169
Aerosol size distribution seasonal characteristics measured in Tiksi, Russian Arctic
Asmi, E., Kondratyev, V., Brus, D., Laurila, T., Lihavainen, H., Backman, J., Vakkari, V., Aurela, M., Hatakka, J., Viisanen, Y., et al. (2016) · Atmospheric Chemistry and Physics · doi:10.5194/acp-16-1271-2016 · Cited by 133
Metadata
- Authors
- Kulmala, M., Maso, M. D., Mäkela, J. M., Pirjola, L., Väkevä, M., Aalto, P., Miikkulainen, P., Hämeri, K., & O’dowd, C. D.
- Venue
- Tellus B: Chemical and Physical Meteorology
- Publisher
- Stockholm University Press
- Published
- 2001-01-01
- Volume
- 53
- Issue
- 4
- Pages
- 479
- ISSN
- 0280-6509 (ISSN-L)
- 1600-0889
- OpenAlex
- W2038178482
- Cited by
- 528
- References
- 0
- FWCI
- 12.62
- Type
- journal article
- Language
- en
- Open access
- bronze
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- Kulmala, M., Maso, M. D., Mäkela, J. M., Pirjola, L., Väkevä, M., Aalto, P., Miikkulainen, P., Hämeri, K., & O’dowd, C. D. (2001). On the formation, growth and composition of nucleation mode particles. Tellus B: Chemical and Physical Meteorology. https://doi.org/10.3402/tellusb.v53i4.16622
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