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Nutrient Dynamics in Jiaozhou Bay

机译:胶州湾的营养动态

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Three cruises were carried out in Jiaozhou Bay(JZB)in the neap tide in October 2002(fall)and in both neap and spring tides in May 2003(spring)to understand the relative importance of external nutrient inputs versus physical transport and internal biogeo-chemical processes.Nutrients(NO_3~-,NO_2~-,NH_4~+,PO_4~(3-),silicic acid,total dissolved nitrogen(TDN)and phosphorus(TDP),dissolved organic nitrogen(DON)and phosphorus(DOP))were measured.The concentrations of nutrients were higher in the northern part than in the southern part.High concentrations of NH_4~+ and DON in JZB demonstrated the anthropogenic input.Ambient nutrient ratios indicated that the potential limiting nutrients for phytoplankton growth were silicon,and then phosphorus.Nutrients showed an obvious tidal effect with low values at flood tide and high values at ebb tide.Nutrient elements were transported into JZB in the north and output in the south(i.e.,into the Yellow Sea),which varied with season,tidal cycle and investigation sites.Water exchange between JZB and the Yellow Sea exports NO_3~-,NH_4~+ and DON out of JZB,while it inputs PO_4~(3-),silicic acid and DOP into JZB.Nutrient budgets demonstrate that riverine input and wastewater discharge are major sources of nutrients,while residual flow is of minor importance in JZB ecosystem.JZB is a sink for the nutrient elements we studied except for DON.Stoichiometric calculations demonstrate that JZB is a net autotrophic system.
机译:在胶州湾(JZB)于2002年10月的潮汐(秋季)和2003年5月的春季和春季潮汐中进行了3次巡游,以了解外部营养输入与物理运输和内部生物地理相对的相对重要性。营养过程(NO_3〜-,NO_2〜-,NH_4〜+,PO_4〜(3-),硅酸,总溶解氮(TDN)和磷(TDP),溶解有机氮(DON)和磷(DOP)北部地区的养分含量高于南部地区.JZB中高浓度的NH_4〜+和DON证明了人为输入。环境养分比表明,浮游植物生长的潜在限制养分是硅,营养元素表现出明显的潮汐作用,潮汐值低,潮汐值高。养分元素从北部运入JZB,向南输出(即进入黄海),随季节变化,潮汐周期和调查JZB和黄海之间的水交换将J_BB中的NO_3〜-,NH_4〜+和DON排放到JZB中,同时将PO_4〜(3-),硅酸和DOP输入到JZB中。营养素预算表明河水输入和废水排泄物是养分的主要来源,而剩余流量在JZB生态系统中的重要性不高。JZB是我们研究的营养元素的汇,除了DON。化学计量计算表明JZB是净自养系统。

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