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中国玄武湖调水与水质关系研究。

Research on the Relationship between Water Diversion and Water Quality of Xuanwu Lake, China.

机构信息

College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China.

College of Environment, Hohai University, Nanjing 210098, China.

出版信息

Int J Environ Res Public Health. 2018 Jun 14;15(6):1262. doi: 10.3390/ijerph15061262.

Abstract

Water diversion is often used to improve water quality to reach the standard of China in the short term. However, this large amount of water diversion can not only improve the water quality, but also lead to a decline in the water quality (total phosphorus, total nitrogen) of Xuanwu Lake. Through theoretical analysis, the relationship between water quality and water diversion is established. We also found that the multiplication of the pollutant degradation coefficient () and the water residence time () is a constant (), K⋅T=N. The water quality changed better at first, with the increase of inflow discharge, and then became worse, and the optimal water quality inflow discharge is 180,000 m³/day. By constructing two-dimensional hydrodynamic and water quality models, the optimal diversion water plan is calculated. Through model calculations, it can be seen that reducing the inflow discharge makes the water residence time longer (15.3 days changed to 23.8 days). Thereby, increasing the degradation of pollutants, and thus improving water quality. Compared with other wind directions, the southwest wind makes the water quality of Xuanwu Lake the most uniform. The concentration of water quality first became smaller and then became larger, as the wind speed increased, and eventually became constant. Implementing these results for water quality improvement in small and medium lakes will significantly reduce the cost of water diversion.

摘要

引水通常用于在短期内将水质提高到中国的标准。然而,这种大量的引水不仅可以改善水质,还会导致玄武湖水质(总磷、总氮)下降。通过理论分析,建立了水质与引水的关系。我们还发现,污染物降解系数 () 和水停留时间 () 的乘积是一个常数 (),K&Tdot;T=N。随着入流流量的增加,水质先变好,然后变差,最佳入流水量为 180,000 立方米/天。通过构建二维水动力和水质模型,计算出最佳引水方案。通过模型计算,可以看出减少入流流量会使水停留时间更长(从 15.3 天变为 23.8 天)。从而增加污染物的降解,从而改善水质。与其他风向相比,西南风使玄武湖的水质最均匀。随着风速的增加,水质的浓度先变小后变大,最终变得恒定。将这些结果应用于中小湖泊的水质改善,将显著降低引水成本。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/de56/6025549/ad0205f6062b/ijerph-15-01262-g001.jpg

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