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      Investigating Primary Marine Aerosol Properties: CCN Activity of Sea Salt and Mixed Inorganic–Organic Particles

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          Abstract

          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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          Production flux of sea spray aerosol

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            Optimal Power-Law Description of Oceanic Whitecap Coverage Dependence on Wind Speed

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              Scale dependence of bubble creation mechanisms in breaking waves.

              Breaking ocean waves entrain air bubbles that enhance air-sea gas flux, produce aerosols, generate ambient noise and scavenge biological surfactants. The size distribution of the entrained bubbles is the most important factor in controlling these processes, but little is known about bubble properties and formation mechanisms inside whitecaps. We have measured bubble size distributions inside breaking waves in the laboratory and in the open ocean, and provide a quantitative description of bubble formation mechanisms in the laboratory. We find two distinct mechanisms controlling the size distribution, depending on bubble size. For bubbles larger than about 1 mm, turbulent fragmentation determines bubble size distribution, resulting in a bubble density proportional to the bubble radius to the power of -10/3. Smaller bubbles are created by jet and drop impact on the wave face, with a -3/2 power-law scaling. The length scale separating these processes is the scale where turbulent fragmentation ceases, also known as the Hinze scale. Our results will have important implications for the study of air-sea gas transfer.
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                Author and article information

                Journal
                Environ Sci Technol
                Environ. Sci. Technol
                es
                esthag
                Environmental Science & Technology
                American Chemical Society
                0013-936X
                1520-5851
                18 July 2012
                02 October 2012
                : 46
                : 19 , Marine Boundary Layer: Ocean Atmospheric Interactions
                : 10405-10412
                Affiliations
                []Department of Chemistry, simpleUniversity of Copenhagen , DK-2100 Copenhagen, Denmark
                []Departamento de Medio Ambiente, simpleCIEMAT , E-28040 Madrid, Spain
                [§ ]Climate Change Unit, simpleFinnish Meteorological Institute , FI-00560 Helsinki, Finland
                []Department of Physics, simpleUniversity of Helsinki , FI-00560 Helsinki, Finland
                []Department of Air Quality and Climate, simpleTNO Built Environment and Geosciences , NL-3508 TA Utrecht, Netherlands
                [# ]Department of Applied Environmental Science, simpleStockholm University , SE-11418 Stockholm, Sweden
                Author notes
                [* ]Phone: +45 35320329. E-mail: mbilde@ 123456chem.ku.dk .
                Article
                10.1021/es300574u
                3462475
                22809370
                6e82ac35-bb8d-406e-9a8a-893f03112513
                Copyright © 2012 American Chemical Society

                This is an open-access article distributed under the ACS AuthorChoice Terms & Conditions. Any use of this article, must conform to the terms of that license which are available at http://pubs.acs.org.

                History
                : 10 February 2012
                : 18 July 2012
                : 13 July 2012
                Categories
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                Custom metadata
                es300574u
                es-2012-00574u

                General environmental science
                General environmental science

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