Spatial-temporal variation of dissolved inorganic nitrogen (DIN) and impacts of water mass on the reserves estimation of the total DIN content in the Yellow Sea
JIN Chun-jie1,2, ZHANG Chuan-song1,2, WANG Li-sha1,2, SHI Xiao-yong1,2,3, HAN Xiu-rong1,2, TANG Hong-jie1,2
1. College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China; 2. Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China; 3. National Marine Hazard Mitigation Service, Beijing 100194, China
Abstract：Based on the data of 4 curies in 2013~2016, the distribution of DIN in the Yellow Sea、nitrogen pool and its influencing factors have been studied. Results showed that the average concentrations of DIN in the Yellow Sea were (5.43±4.02) μmol/L in spring, (4.47±3.16) μmol/L in summer, (7.46±3.56) μmol/L in autumn, and (5.09±2.59) μmol/L in winter, among which DIN contents reached maximum in autumn and minimum in summer, respectively. DIN concentrations declined from coastal zones to the offshore area. The DIN-rich sites near the coast were mostly centralized in the north of the Yangtze River estuary, Shandong Peninsula and Liaodong Peninsula. The main affecting factors all the year except winter were terrigenous input and the growth of phytoplankton, as the resuspension of the riverine input and sediment were the main factors affecting the distribution of DIN in winter. There was an area with high concentration of DIN(>6μmol/L) in the central area, which was co-influenced by the Yellow Sea warm current and the Yellow Sea Cold Water Mass. Cluster analysis has been used to classified the Yellow Sea water into 5 water masses, including the Yellow Sea water masses (Y), Yellow Sea cold water mass (YC), Yellow Sea warm current water (YW), Coastal water mass (CW) and Yellow Sea-East China Sea mixed water mass (YE), which was the main water mass in the researching sea area. All these water masses except for Y were seasonal. The total DIN content in the research field showed no obvious difference in all year, and their range was 1.0×106~1.5×106t. The DIN content was slightly lower in spring and summer under the influence of phytoplankton assimilation. The total DIN contents were about 1.2×106t in spring, 1.0×106t in summer, 1.5×106t in autumn, and 1.3×106t in winter, respectively. The contributions of water masses to the total DIN content were different in the varying season. In autumn and winter, Y was dominant, while in summer and spring, YW and YC played the dominant roles, respectively.
金春洁, 张传松, 王丽莎, 石晓勇, 韩秀荣, 唐洪杰. 黄海溶解无机氮时空变化及其水团对DIN总量的影响[J]. 中国环境科学, 2021, 41(4): 1642-1654.
JIN Chun-jie, ZHANG Chuan-song, WANG Li-sha, SHI Xiao-yong, HAN Xiu-rong, TANG Hong-jie. Spatial-temporal variation of dissolved inorganic nitrogen (DIN) and impacts of water mass on the reserves estimation of the total DIN content in the Yellow Sea. CHINA ENVIRONMENTAL SCIENCECE, 2021, 41(4): 1642-1654.
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