Qu Li-mei, Yao De, Cong Pi-fu
Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China.
Huan Jing Ke Xue. 2006 Feb;27(2):263-7.
On basis of field data measured during 4 cruises from June to September in 2002, variation feature of inorganic nitrogen and phosphate in Liaodong Bay was analyzed. Regression analyses of NH4+(-)N, NO3-(-)N, NO2-(-)N and PO4(3-)-P versus pH as well as inorganic nitrogen and phosphate versus salinity were also conducted. Finally, potential eutrophication of Liaodong Bay was assessed. It is shown that inorganic nitrogen and phosphate in Liaodong Bay vary with different months and different locations. In coast areas inorganic nitrogen and phosphate are mainly affected by rivers, while in central areas of the bay, they are subject to marine biochemical process. Ratio of inorganic nitrogen to phosphate rises to 60.6 from 52.5 in early June, then drops to 39, all far above Redfield value 16. Inorganic nitrogen and phosphate versus pH as well as salinity show different correlation. For example, the correlation coefficient of NO2(-)-N and pH even reaches 0.93. During 4 cruises in Liaodong Bay the total inorganic nitrogen is 212.0 microg/L, phosphate 10.1 microg/L, N/P 50.77. Potential eutrophication assessment indicates that during the survey period Liaodong Bay can be classified as a phosphate-limiting moderate-level nutrient area.
根据2002年6月至9月4个航次的现场实测数据,分析了辽东湾无机氮和磷酸盐的变化特征。对NH4⁺-N、NO3⁻-N、NO2⁻-N和PO4³⁻-P与pH以及无机氮和磷酸盐与盐度进行了回归分析。最后,对辽东湾潜在富营养化状况进行了评价。结果表明,辽东湾无机氮和磷酸盐含量随月份和地点的不同而变化。在海岸地区,无机氮和磷酸盐主要受河流影响,而在海湾中部地区,则受海洋生化过程的影响。无机氮与磷酸盐的比值从6月初的52.5上升到60.6,然后降至39,均远高于雷德菲尔德值16。无机氮和磷酸盐与pH以及盐度呈现出不同的相关性。例如,NO2⁻-N与pH的相关系数甚至达到0.93。在辽东湾4个航次中,总无机氮为212.0微克/升,磷酸盐为10.1微克/升,N/P为50.77。潜在富营养化评价表明,在调查期间,辽东湾可被归类为磷限制型中度营养区。