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Influence of a Flood Event on Salinity and Nutrients in the Changshan Archipelago Area (Northern Yellow Sea)

查看全文 作  者:ZHANG [1]Guangtao;ZHAO [1]Zengxia;LIU [2]Changhua;LIU [1]Qun;REN [2]Jianming 高影响力作者 机构地区:[1]Jiaozhou Bay Marine Ecosystem Research Station,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;[2]The Yellow Sea Marine Observation Station,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China高影响力机构 出  处:《Journal of Ocean University of China》索引2012年第11卷第3期,共8页高影响力期刊 基  金:supported by the Knowledge Innovation Program of Chinese Academy of Sciences,the IOCAS-Zhangzidao Fishery Eco-Mariculture Joint Laboratory;the National Key Technology Research and Development Program (2008BAC42B01) 摘  要:River discharge can deliver nutrients to the coastal zone and change the hydrologic properties of the water column. Soon after a flash flood from the Yalu River (Northeast China) in August 2010, we investigated the salinity and nutrient concentrations, as well as other environmental conditions in the Changshan Archipelago area, located approximately 100 km west of the river mouth in the northern Yellow Sea. Diluted water was mainly observed in the upper layers shallower than 15 m, with surface salinity between 18.13 and 30.44 in the eastern study area and between 28.16 and 29.72 in the western area. Surface salinity showed a significant negative correlation with concentrations of dissolved nutrients (P < 0.05), but not with that of Chlorophyll-a (Chl-a), dissolved oxygen (DO), particulate materials or pH. The average concentrations of nitrite, nitrate, and silicic acid decreased from the surface layer to bottom layer and were significantly higher in the east area than in the west area (P < 0.05). In contrast, average ammonium and phosphate concentrations were highest in the bottom layer of both areas, with no significant spatial differences. DO varied between 6.06 and 8.25 mg L-1 in the surface layer, and was significantly higher in the eastern area than in the western area in the surface and middle layers. Chl-a concentration was constantly below 4.09 μg L-1. Our work demonstrated the strong influences of Yalu River on proportions of various nutrient components in the Changshan Archipelago area. Silicic acid and total inorganic nitrogen levels were significantly elevated comparing to phosphate in the eastern area. Such changes can potentially induce phosphate limit to phytoplankton growth. 关 键 词:长山群岛 黄海北部 营养盐 盐度 洪水事件 叶绿素A浓度 西部地区 东部地区
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