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Karst spring discharge modeling 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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摘要

The Shentou karst springs are representative of the 19 major karst springs in Shanxi, northern China. As the most important water supply source for Shuozhou City, Shanxi Province, the Shentou springs have an average discharge of 6.86 m3/s (between 1958 and 1999). 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 by 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 future should the rainfalls at Shentou keep comparatively high as in the middle of the 1990s and groundwater in Shuozhou not be excessively exploited.
机译:神头岩溶泉是中国北方山西19个主要岩溶泉的代表。作为山西省朔州市最重要的水源,神头泉的平均流量为6.86立方米/秒(1958年至1999年)。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。到1985年,神头泉的流量变化可分为两个阶段,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1985年之后的流量变化。预测变化趋势。对2000年至2004年之间流量变化的预测表明,如果神头县的雨水保持在1990年代中期相对较高的水平,朔州的地下水不被过度开发,则流量将遵循未来的增长趋势。

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