Investigating Primary Marine Aerosol Properties: CCN Activity of Sea Salt and Mixed Inorganic–Organic Particles
Author(s) -
S. M. King,
A. C. Butcher,
T. Rosenoern,
Esther Coz,
K. Lieke,
Gerrit de Leeuw,
E. D. Nilsson,
Merete Bilde
Publication year - 2012
Publication title -
environmental science and technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.851
H-Index - 397
eISSN - 1520-5851
pISSN - 0013-936X
DOI - 10.1021/es300574u
Subject(s) - seawater , sea spray , artificial seawater , cloud condensation nuclei , aeration , sea salt , diffuser (optics) , aerosol , chemistry , particle (ecology) , particle size , organic matter , jet (fluid) , environmental chemistry , chemical engineering , oceanography , organic chemistry , physics , light source , engineering , optics , thermodynamics , geology
Sea spray particles ejected as a result of bubbles bursting from artificial seawater containing salt and organic matter in a stainless steel tank were sampled for size distribution, morphology, and cloud condensation nucleus (CCN) activity. Bubbles were generated either by aeration through a diffuser or by water jet impingement on the seawater surface. Three objectives were addressed in this study. First, CCN activities of NaCl and two types of artificial sea salt containing only inorganic components were measured to establish a baseline for further measurements of mixed organic-inorganic particles. Second, the effect of varying bubble residence time in the bulk seawater solution on particle size and CCN activity was investigated and was found to be insignificant for the organic compounds studied. Finally, CCN activities of particles produced from jet impingement were compared with those produced from diffuser aeration. Analyses indicate a considerable amount of organic enrichment in the jet-produced particles relative to the bulk seawater composition when sodium laurate, an organic surfactant, is present in the seawater. In this case, the production of a thick foam layer during impingement may explain the difference in activation and supports hypotheses that particle production from the two methods of generating bubbles is not equal.
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