Articles | Volume 13, issue 5
https://doi.org/10.5194/os-13-633-2017
https://doi.org/10.5194/os-13-633-2017
Research article
 | 
31 Aug 2017
Research article |  | 31 Aug 2017

Study on organic matter fractions in the surface microlayer in the Baltic Sea by spectrophotometric and spectrofluorometric methods

Violetta Drozdowska, Iwona Wrobel, Piotr Markuszewski, Przemysław Makuch, Anna Raczkowska, and Piotr Kowalczuk

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Cited articles

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Boehme, J. and Wells, M.: Fluorescence variability of marine and terrestrial colloids: Examining size fractions of chromophoric dissolved organic matter in the Damariscotta River estuary, Mar. Chem., 101, 95–103, https://doi.org/10.1016/j.marchem.2006.02.001, 2006.
Bracchini, L., Cózar, A., Dattilo, A. M., Loiselle, S. A., Tognazzi, A., Azza, N., and Rossi, C.: The role of wetlands in the chromophoric dissolved organic matter release and its relation to aquatic ecosystems optical properties. A case of study: Katonga and Bunjako Bays (Victoria Lake, Uganda), Chemosphere, 63, 1170–1178, https://doi.org/10.1016/j.chemosphere.2005.09.045, 2006.
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Short summary
The studies on the absorption and fluorescence properties of the organic molecules included in surface microlayer (SML) and subsurface (SS) waters confirm that (i) the process of the structural changes in molecules of HMW to LMW, due to effects of photo- and biodegradation, occurs faster in the SML than in the SS; (ii) the organic molecules contained in the SML have a smaller molecular mass than in the SS. Hence, SML can specifically modify the physical processes associated with the sea surface.