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Numerical study on amelioration of water quality in Lakes Shinji and Nakaumi: a coastal brackish lagoon system

机译:沿海咸水泻湖系统改善真治湖和中海湖水质的数值研究

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Aiming at estimating the effect of an amelioration scheme for water quality in a highly eutrophicated and strongly enclosed estuary, especially placing emphasis on the alleviation of a oxygen-depleted water body, a three-dimensional (3-D) time-dependent coupled physical and ecological model was applied to Lakes Shinji and Nakaumi, a typical coastal brackish lagoon system in Japan. First, the model was run to reproduce the seasonal variation in water temperature, salinity, dissolved oxygen, and other ecological constituents during the period from April 1998 to March 1999. The daily change regimes of the observed sea surface winds, tidal elevation at the open boundary, river discharges, and meteorological parameters were incorporated into the forcing variables of the ecosystem model. Next, as a numerical experiment, a scenario simulation was carried out under four premises to alleviate the oxygen-depleted water body. The model results agreed fairly well with the field measurements obtained through the regular environmental monitoring in the lagoon system. It was found that an oxygen-depleted water body appears in the eastern part of Lake Nakaumi in early May and develops to cover the whole lagoon in midsummer to leave it almost anoxic. The scenario simulation revealed that each amelioration scheme has a considerable effect in alleviating this hypoxic water body. It was found from the model results and the additional flux analyses that the oxygen concentration will improve as a result of (1) change in the flow field by cutting the dikes built up during lake reclamation and (2) decrease in benthic oxygen consumption by filling up deep holes once created by dredging activities.
机译:旨在评估改善方案在高度富营养化和高度封闭的河口中对水质的影响,尤其着重于减少耗氧水体,三维(3-D)时变耦合物理和水生态模型被应用于日本典型的沿海咸淡水泻湖系统Shinji和Nakaumi。首先,运行该模型以重现1998年4月至1999年3月期间水温,盐度,溶解氧和其他生态成分的季节性变化。观测到的海表风的日变化态,露天的潮汐高程边界,河流流量和气象参数被纳入生态系统模型的强迫变量。接下来,作为数值实验,在四个前提下进行了情景模拟以减轻贫氧水体。模型结果与通过泻湖系统中的常规环境监测获得的现场测量结果非常吻合。人们发现,缺氧的水体在五月初出现在中尾湖的东部,并在仲夏发展为覆盖整个泻湖,几乎没有氧。情景模拟表明,每种改善方案在缓解这种低氧水体方面都具有相当大的作用。从模型结果和附加通量分析中发现,氧的浓度将由于以下原因而提高:(1)通过减少在填海过程中积聚的堤坝来改变流场,以及(2)通过填充减少底栖氧气消耗挖泥活动造成的深孔。

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