ZHANG Jing, YANG Guipeng. Chemical properties of colored dissolved organic matter in the sea-surface microlayer and subsurface water of Jiaozhou Bay, China in autumn and winter[J]. Acta Oceanologica Sinica, 2013, 32(6): 26-39. doi: 10.1007/s13131-013-0306-4
Citation: ZHANG Jing, YANG Guipeng. Chemical properties of colored dissolved organic matter in the sea-surface microlayer and subsurface water of Jiaozhou Bay, China in autumn and winter[J]. Acta Oceanologica Sinica, 2013, 32(6): 26-39. doi: 10.1007/s13131-013-0306-4

Chemical properties of colored dissolved organic matter in the sea-surface microlayer and subsurface water of Jiaozhou Bay, China in autumn and winter

doi: 10.1007/s13131-013-0306-4
  • Received Date: 2011-12-14
  • Rev Recd Date: 2012-03-27
  • The distribution and chemical properties of chromophoric dissolved organic matter (CDOM) in the Jiaozhou Bay, China were examined during four cruises in 2010-2011. The influence of freshwater and industrial and municipal sewage along the eastern coast of the bay was clearly evident as CDOM levels (defined as a305), and dissolved organic carbon (DOC) concentrations were well correlated with salinity during all the cruises. Moreover, DOC concentrations were significantly correlated with chlorophyll a concentrations in the surface microlayer as well as in the subsurface water. The concentrations of DOC and CDOM displayed a gradually decreasing trend from the northwestern and eastern coast to the central bay, and the values and gradients of their concentrations on the eastern coast were generally higher than those on the western coast. In addition, CDOM and DOC levels were generally higher in the surface microlayer than in the subsurface water. In comparison with DOC, CDOM exhibited a greater extent of enrichment in the microlayer in each cruise, with average enrichment factor (EF) values of 1.38 and 1.84, respectively. Four fluorescent components were identified from the surface microlayer and subsurface water samples and could be distinguished as peak A, peak T, peak B and peak M. For all the cruises, peak A levels were higher in the surfacemicrolayer than in the subsurface water. This pattern of variationmight be attributed to the terrestrial input.
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      沈阳化工大学材料科学与工程学院 沈阳 110142

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