Distribution and source analyses of particulate organic carbon in the Yellow Sea and Bohai Sea during summer, 2013

Zhang Haibo; Yang Luning; Wang Lisha; Pei Shaofeng; Shi Xiaoyong

doi:10.3969/j.issn.0253-4193.2016.08.003

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Zhang Haibo, Yang Luning, Wang Lisha, Pei Shaofeng, Shi Xiaoyong. Distribution and source analyses of particulate organic carbon in the Yellow Sea and Bohai Sea during summer, 2013[J]. Haiyang Xuebao, 2016, 38(8): 24-35. doi: 10.3969/j.issn.0253-4193.2016.08.003

Citation:

Zhang Haibo, Yang Luning, Wang Lisha, Pei Shaofeng, Shi Xiaoyong. Distribution and source analyses of particulate organic carbon in the Yellow Sea and Bohai Sea during summer, 2013[J]. Haiyang Xuebao, 2016, 38(8): 24-35. doi: 10.3969/j.issn.0253-4193.2016.08.003

Citation:

Zhang Haibo, Yang Luning, Wang Lisha, Pei Shaofeng, Shi Xiaoyong. Distribution and source analyses of particulate organic carbon in the Yellow Sea and Bohai Sea during summer, 2013[J]. Haiyang Xuebao, 2016, 38(8): 24-35. doi: 10.3969/j.issn.0253-4193.2016.08.003

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Distribution and source analyses of particulate organic carbon in the Yellow Sea and Bohai Sea during summer, 2013

doi: 10.3969/j.issn.0253-4193.2016.08.003

1.
College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China;Key Lab. of Coastal Wetland Biogeosciences, China Geological Survey, Qingdao 266071, China
2.
Yantai Oceanic Environmental Monitoring Central Station of State Oceanic Administration, Yantai 264006, China
3.
College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China
4.
Key Lab. of Coastal Wetland Biogeosciences, China Geological Survey, Qingdao 266071, China
5.
College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China;National Marine Hazard Mitigation Service, Beijing 100194, China

Received Date: 2015-10-15
Rev Recd Date: 2015-12-28

Abstract

Abstract

Based on the data of particulate organic carbon (POC), chlorophyll a(Chl a) and total suspended particles (TSP) as well as hydrological environment parameters collected during the summer of 2013 in the Yellow Sea and Bohai Sea.We examined the spatial and temporal distribution patterns of POC, and possible factors influencing POC contents and distributions in various water masses characterized by temperature and salinity. Results show that POC concentrations ranged from 102.3 μg/L to 1 850.0 μg/L, with an average of (383.7±269.6) μg/L, and declined from nearshore to offshore areas but increased from surface to bottom layers. The high concentration of POC appears at northern of Jiangsu Province because of the runoff input, mixing effect of longshore currents and enriched phytoplankton photosynthesis, and at the layers of both 10 m and bottom in the northeast area of the northern Yellow Sea. Influenced by ocean circulations, phytoplankton productivity was relatively lower in the middle of the southern Yellow Sea, and resulted in the lower POC concentrations in this regional area. Vertical distribution shows that POC concentrations were higher and mixed well in the nearshore area because of terrestrial input and resuspension. Controlled by ocean circulation and the Cold Water Mass, phytoplankton productivity was relatively lower in the middle of southern and northern Yellow Sea, and correspondingly decreased POC concentrations. In the water masses characterized by high temperature and low salinity, POC distributions were mainly influenced by phytoplankton primary production and resuspension. In the water masses characterized by moderate temperature and salinity, primary production of phytoplankton was the major source of POC. In the cold water mass of bottom layers, the main sources of POC were particle deposition and resuspension.
- particulate organic carbon,
- chlorophyll,
- Yellow Sea,
- Bohai Sea,
- water mass

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References(39)

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