首页> 外文会议>Third International Conference on Environmental Problems in Coastal Regions, 2000 >3D model system for hydrodynamics, eutrophication and nutrient transport
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3D model system for hydrodynamics, eutrophication and nutrient transport

机译:流体动力学,富营养化和营养物输送的3D模型系统

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The existing MIKE 3 model system consisting of modules for hydrodynamics and eutrophication has been improved to include a description of exchangeable pools of nitrogen (N) and phosphorus (P) in the sediment. It is now possible to make a complete mass balance for N and P in a model area and to make calculations of the transport of nutrients across sections in the model. Besides the new feature the model system is also able to simulate water levels, current fields, concentrations of nutrients, chlorophyll, dissolved oxygen, biomass of eelgrass and benthic macroalgae. The model system has been calibrated (1998) and validated (1997) on a temperate shallow Danish fjord, (Odense Fjord, Funen). The fjord, which covers 64 km~2 and has an average depth of 2.5 m, is connected to the sea through a narrow entrance. The hydrodynamic module was able to reproduce the water levels and the salinity satisfactorily at three stations in the fjord for both years. At two stations weekly data of water chemical parameters, such as total P & N and inorganic nutrients, were available for the calibration and validation of the eutrophication module. Based on model results a nutrient budget was set up for 1997 and 1998. Due to low precipitation the 1997 load of N and P was about 60 % lower than in 1998. The yearly retention of N for the two years was 35 % and 15 % and was caused by the burial of N in the sediment and denitrification. The yearly retention of P was negative,-121% and -28 %, for the two years due to the release of P from the sediment. This is consistent with the implementation of the nutrient treatment of domestic sewage in the early 1990's.
机译:现有的由流体动力学和富营养化模块组成的MIKE 3模型系统已得到改进,以包括对沉积物中氮(N)和磷(P)可交换池的描述。现在,可以在模型区域中实现N和P的完全质量平衡,并计算模型中各个部分的养分迁移率。除了新功能外,该模型系统还能够模拟水位,当前场,养分浓度,叶绿素,溶解氧,鳗gra生物和底栖大型藻类。该模型系统已在温带浅层丹麦峡湾(Odense峡湾,Funen)上进行了校准(1998年)和验证(1997年)。峡湾全长64 km〜2,平均深度为2.5 m,通过狭窄的入口与大海相连。两年来,流体动力学模块能够令人满意地再现峡湾三个站的水位和盐度。在两个站点,每周的水化学参数数据(例如总P&N和无机养分)可用于富营养化模块的校准和验证。根据模型结果,制定了1997年和1998年的养分预算。由于降水量少,1997年的N和P含量比1998年低约60%。两年中N的年保留量分别为35%和15%并且是由于沉积物中的氮埋藏和反硝化所致。由于沉积物中P的释放,两年中P的年保留量分别为负,-121%和-28%。这与1990年代初期对生活污水进行养分处理是一致的。

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