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Karst spring discharge modelling based on grey system theory:A case study at Shentou, northern China

机译:基于灰色系统理论的岩溶泉水涌流模拟-以华北神头为例

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As the most important water supply source for Shuozhou City of northern China, the Shentou springs have an average annual discharge of 6.86 nrVs. However, the discharge of the springs has been reducing since the early 1960s. Grey system theory is applied to simulate and predict the change in discharge of the Shentou springs with time. The change in the discharge of the Shentou springs can be divided into two phases: before and after 1985. The GM (1,1) model is used to fit the discharge change process before 1985, and grey prediction-amending model to simulate the process after 1985 and to predict the trend of the change. The prediction of discharge change between 2000 and 2004 shows that the discharge would follow the trend of increasing in the future should the rainfalls at Shentou continue to be comparatively high, as in the middle of the 1990s, and groundwater in Shuozhou is not excessively exploited.
机译:作为华北朔州市最重要的水源,神头泉的年平均排放量为6.86 nrVs。但是,自1960年代初以来,弹簧的排出量一直在减少。应用灰色系统理论对神头泉水流量随时间的变化进行模拟和预测。神头泉水流量的变化可分为两个阶段:1985年之前和之后。GM(1,1)模型用于拟合1985年之前的流量变化过程,灰色预测修正模型用于模拟该过程。并在1985年以后预测了变化的趋势。对2000年至2004年之间流量变化的预测表明,如果1990年代中期神头的降雨继续保持较高水平,并且朔州的地下水没有被过度开采,流量将遵循未来增加的趋势。

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