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The phosphorus cycle in the Sanggou Bay

机译:桑沟湾的磷循环

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摘要

The phosphorus cycle is studied during 2013–2014 in the Sanggou Bay (SGB), which is a typical aquaculture area in northern China. The forms of measured phosphorus include dissolved inorganic phosphorus (DIP), dissolved organic phosphorus (DOP), particulate inorganic phosphorus (PIP), and particulate organic phosphorus (POP). DIP and PIP are the major forms of total dissolved phosphorus (TDP) and total particulate phosphorus (TPP), representing 51%–75% and 53%–80%, respectively. The concentrations and distributions of phosphorus forms vary among seasons relative to aquaculture cycles, fluvial input, and hydrodynamic conditions. In autumn the concentration of DIP is significantly higher than in other seasons (P<0.01), and higher concentrations are found in the west of the bay. In winter and spring the phosphorus concentrations are higher in the east of the bay than in the west. In summer, the distributions of phosphorus forms are uniform. A preliminary phosphorus budget is developed, and shows that SGB is a net sink of phosphorus. A total of 1.80×107 mol/a phosphorus is transported into the bay. The Yellow Sea is the major source of net input of phosphorus (61%), followed by submarine groundwater discharge (SGD) (27%), river input (11%), and atmospheric deposition (1%). The main phosphorus sink is the harvest of seaweeds (Saccharina japonica andGracilaria lemaneiformis), bivalves (Chlamys farreri), and oysters (Crassostrea gigas), accounting for a total of 1.12×107 mol/a. Burial of phosphorus in sediment is another important sink, accounting for 7.00×106 mol/a. Biodeposition by bivalves is the major source of phosphorus in sediment, accounting for 54% of the total.
机译:在中国北方地区典型的水产养殖区桑沟湾(SGB),研究了2013-2014年的磷循环。被测磷的形式包括溶解无机磷(DIP),溶解有机磷(DOP),颗粒无机磷(PIP)和颗粒有机磷(POP)。 DIP和PIP是总溶解磷(TDP)和总颗粒磷(TPP)的主要形式,分别占51%–75%和53%–80%。磷的浓度和分布随季节的变化而变化,这取决于水产养殖周期,河流输入和水动力条件。秋季,DIP的浓度明显高于其他季节(P <0.01),并且在海湾西部发现浓度较高。在冬季和春季,海湾东部的磷含量高于西部。夏季,磷的形态分布均匀。初步的磷预算已经制定,表明SGB是磷的净汇。总共1.80×107 mol / a的磷被输送到海湾中。黄海是磷净输入的主要来源(61%),其次是海底地下水排放(SGD)(27%),河流输入(11%)和大气沉积(1%)。主要的磷汇是海藻(Saccharina japonica和Gracilaria lemaneiformis),双壳类(Chlamys farreri)和牡蛎(Crassostrea gigas)的收获,占1.12×107 mol / a。沉积物中的磷埋葬是另一个重要的汇,占7.00×106 mol / a。双壳类生物沉积是沉积物中磷的主要来源,占总量的54%。

著录项

  • 来源
    《海洋学报(英文版)》 |2017年第1期|90-100|共11页
  • 作者单位

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, 0cean University of China/Qingdao Collaborative Innovation Center of Marine Science and Technology, Qingdao 266100, China;

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, 0cean University of China/Qingdao Collaborative Innovation Center of Marine Science and Technology, Qingdao 266100, China;

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, 0cean University of China/Qingdao Collaborative Innovation Center of Marine Science and Technology, Qingdao 266100, China;

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, 0cean University of China/Qingdao Collaborative Innovation Center of Marine Science and Technology, Qingdao 266100, China;

    Department of Mariculture Ecology and Carrying Capacity Laboratory, Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266100, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
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