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Modelling the spatial distribution of phytoplankton and inorganic nitrogen in Narva Bay, southeastern Gulf of Finland, in the biologically active period

机译:在生物活性期模拟芬兰东南海湾纳尔瓦湾浮游植物和无机氮的空间分布

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The mean spatial distributions of phytoplankton and inorganic nitrogen (IN) in Narva Bay (southeastern Gulf of Finland) during a single biologically active period were studied by means of numerical modelling. The model implemented is three-dimensional ecohydrodynamic model MIKE 3. Model validation gave reasonable justification for studying the mean spatial distributions of IN and phytoplankton in Narva Bay. Results showed that mean inorganic nitrogen concentration in Narva Bay was highest near the river mouth (0.015 to about 0.03 gN/m(3)), while phytoplankton concentration was relatively low there. Another area of elevated IN concentration was found at the southern coast of Narva Bay some 30 km to the west from the river mouth, where high phytoplankton concentration persisted during summer. In general, coastal waters enriched with inorganic nitrogen (IN > 0.006 gN/m(3)) formed a narrow belt of approximately 3-8 km wide that extended from the middle of the eastern coast and along the entire southern coast of Narva Bay. According to phytoplankton distribution the coastal waters can be characterized with concentrations exceeding OAS gC/m(3). The results allow to the separation of the Narva Bay coastal area into zones with different trophic status and nutrients origin: (a) the river mouth area with high IN and low phytoplankton concentration due to intensive hydrodynamic processes, (b) the area to the right of the river mouth with high phytoplankton concentration due to river IN discharge, (c) the southwestern coastal part of the bay enriched with nutrients due to upwelling, and (d) the area between upwelling zone and the river mouth influenced by both upwelling and river discharge. (c) 2006 Elsevier B.V. All rights reserved.
机译:通过数值模拟研究了纳瓦湾(芬兰东南海湾)​​在单个生物活跃期内浮游植物和无机氮(IN)的平均空间分布。实施的模型是三维生态水动力模型MIKE3。模型验证为研究纳尔瓦湾IN和浮游植物的平均空间分布提供了合理的理由。结果表明,纳尔瓦湾的平均无机氮浓度在河口附近最高(0.015至约0.03 gN / m(3)),而那里的浮游植物浓度相对较低。在纳尔瓦湾的南海岸,距河口以西约30公里处,发现了另一个IN浓度升高的区域,夏季期间,浮游植物的高浓度持续存在。一般而言,富含无机氮的沿海水域(IN> 0.006 gN / m(3))形成了一条约3-8公里宽的窄带,从东部海岸的中部延伸至整个纳尔瓦湾的整个南部海岸。根据浮游植物的分布,沿海水域的浓度可以超过OAS gC / m(3)。结果可将纳尔瓦湾沿岸地区分为营养状态和营养来源不同的区域:(a)由于密集的水动力过程而导致的高IN和低浮游植物浓度的河口区域,(b)右侧区域河流IN排放引起的浮游植物浓度高的河口的变化;(c)由于上升流而使海湾西南沿海地区富含营养的物质;(d)受上升流和河流影响的上升流区与河口之间的区域卸货。 (c)2006 Elsevier B.V.保留所有权利。

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