Primary submicron marine aerosol dominated by insoluble organic colloids and aggregates

M. C. Facchini(Institute of Atmospheric Sciences and Climate), Matteo Rinaldi(Institute of Atmospheric Sciences and Climate), Stefano Decesari(Institute of Atmospheric Sciences and Climate), Claudio Carbone(Institute of Atmospheric Sciences and Climate), E. Finessi(Institute of Atmospheric Sciences and Climate), Mihaela Mircea(Institute of Atmospheric Sciences and Climate), S. Fuzzi(Institute of Atmospheric Sciences and Climate), Darius Čeburnis(Ollscoil na Gaillimhe – University of Galway), Robert J. Flanagan(Ollscoil na Gaillimhe – University of Galway), E. D. Nilsson(Stockholm University), Gerrit de Leeuw(Finnish Meteorological Institute), Manuela Martino(University of East Anglia), Janina Woeltjen(University of East Anglia), Colin O’Dowd(Ollscoil na Gaillimhe – University of Galway)
Geophysical Research Letters
September 1, 2008
Cited by 543Open Access
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Abstract

The chemical properties of sea‐spray aerosol particles produced by artificially generated bubbles using oceanic waters were investigated during a phytoplankton bloom in the North Atlantic. Spray particles exhibited a progressive increase in the organic matter (OM) content from 3 ± 0.4% up to 77 ± 5% with decreasing particle diameter from 8 to 0.125 μ m. Submicron OM was almost entirely water insoluble (WIOM) and consisted of colloids and aggregates exuded by phytoplankton. Our observations indicate that size dependent transfer of sea water organic material to primary marine particles is mainly controlled by the solubility and surface tension properties of marine OM. The pattern of WIOM and sea‐salt content in the different size intervals observed in bubble bursting experiments is similar to that measured in atmospheric marine aerosol samples collected during periods of high biological activity. The results point to a WIOM/sea‐salt fingerprint associated with submicron primary marine aerosol production in biologically rich waters.


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