Tang Yong, Sun Yu-Yan, Shi Xiao-Yong, Han Xiu-Rong, Su Rong-Guo
College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 261000, China.
Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 261000, China.
Huan Jing Ke Xue. 2017 Nov 8;38(11):4501-4512. doi: 10.13227/j.hjkx.201703183.
Water samples were collected from the Yellow and Bohai seas during November 2013 and the chromophoric dissolved organic matter (CDOM) and nutrients concentrations were investigated, including their composition, source and distribution characteristics. CDOM was analyzed by excitation-emission matrix spectroscopy (EEMS) in combination with a parallel factor analysis (PARAFAC). Three terrestrial humic-like substances (C1, C2, and C3) and one protein-like (C4) substances were identified. The three terrestrial humic-like components had a similar horizontal distribution, decreasing from inshore to offshore. The protein-like component, showed higher values for both inshore and offshore areas in the Yellow Sea at the surface layer and the middle layer of the Bohai Sea, while in other layers it had a similar distribution pattern as the terrestrial humic-like components. In the Bohai Sea, the dissolved inorganic nitrogen (DIN) concentration showed a decreasing trend from inshore to offshore areas and the concentration of dissolved inorganic phosphorus (DIP) gradually decreased from the Caofeidian coastal and central areas to other adjacent areas. The dissolved organic nitrogen (DON) showed an increasing from inshore to the central area of the Bohai Sea. DIN and DON were higher in surface layer than in the bottom layer and for DIP this was the opposite in the Bohai Sea. In the Yellow Sea, DON concentrations showed a decreasing trend from inshore to offshore areas. DIN and DIP had higher concentrations at inshore areas in the surface and middle layers, while in the bottom layer they had higher concentrations in offshore areas. The vertical distribution of the DIN and DIP showed higher values in the bottom layer than surface layers and for DON this was the opposite. These results also showed that the concentrations of DIN, DON, and DIP in the Bohai sea were overall higher than the Yellow Sea. A discriminant analysis was performed through redundancy analysis (RAD) of these water quality parameters, including the four fluorescent components, an absorption coefficient (), chlorophyll a concentration, conductivity, dissolved oxygen (DO), dissolved organic carbon (DOC), DIN, DON, and DIP. The RDA indicated that the four fluorescent components are mainly affected by terrestrial inputs. DOC was affected by both terrestrial and marine sources but terrestrial inputs were the major contributor. It was also indicated that the DIN concentration was affected by terrestrial inputs in the Bohai Sea area and by both terrestrial and marine sources in the Yellow Sea. DON concentrations were mainly affected by marine sources in the Bohai Sea and terrestrial inputs in the Yellow Sea. DIP concentrations were affected by both terrestrial and marine sources in the studied areas.
2013年11月,在黄海和渤海采集了水样,对其中的发色溶解有机物(CDOM)和营养盐浓度进行了调查,包括它们的组成、来源和分布特征。采用激发发射矩阵光谱法(EEMS)结合平行因子分析(PARAFAC)对CDOM进行分析。识别出三种陆地腐殖质类物质(C1、C2和C3)和一种蛋白质类物质(C4)。三种陆地腐殖质类成分具有相似的水平分布,从近岸向离岸逐渐降低。蛋白质类成分在黄海表层和渤海中层的近岸和离岸区域均表现出较高的值,而在其他水层中,其分布模式与陆地腐殖质类成分相似。在渤海,溶解无机氮(DIN)浓度从近岸向离岸区域呈下降趋势,溶解无机磷(DIP)浓度从曹妃甸沿海和中部地区向其他相邻区域逐渐降低。溶解有机氮(DON)在渤海从近岸向中部区域呈增加趋势。DIN和DON在表层高于底层,而DIP在渤海则相反。在黄海,DON浓度从近岸向离岸区域呈下降趋势。DIN和DIP在表层和中层的近岸区域浓度较高,而在底层则在离岸区域浓度较高。DIN和DIP的垂直分布在底层高于表层,而DON则相反。这些结果还表明,渤海中DIN、DON和DIP的浓度总体高于黄海。通过对这些水质参数进行冗余分析(RAD)进行判别分析,这些参数包括四种荧光成分、吸收系数()、叶绿素 a 浓度、电导率、溶解氧(DO)、溶解有机碳(DOC)、DIN、DON和DIP。冗余分析表明,四种荧光成分主要受陆地输入的影响。DOC受陆地和海洋来源的共同影响,但陆地输入是主要贡献者。还表明,DIN浓度在渤海海域受陆地输入的影响,在黄海受陆地和海洋来源的共同影响。DON浓度在渤海主要受海洋来源的影响,在黄海受陆地输入的影响。DIP浓度在研究区域受陆地和海洋来源的共同影响。