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Regional groundwater flow modeling in Zhangye Basin a of Heihe river watershed, China

机译:张掖盆地地区地下水流动造型海河流域,中国海河流域A

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Groundwater in Zhangye Basin accounts for a large amount of quantities during supplying water for Zhangye City. In order to find out the optimal groundwater development plan to achieve the sustainable development, a regional groundwater flow model was constructed for the study area. Hydrogeological parameters were calibrated against observed groundwater level hydrographs and flow field. Then, the model was used to analyze the flow system and the trend of groundwater levels changes. The modeling results show that total recharge was 1216×106m3/a and total discharge was 1365×106m3/a for the modeling period, i.e. 149 M m3/a of groundwater storage was over drafted. Ten year predictions show that groundwater level would continuously decline in the area under current groundwater exploitation schemes.
机译:张掖盆地地下水占张掖市供水期间的大量数量。 为了了解实现可持续发展的最佳地下水开发计划,为研究区建造了一个区域地下水流量模型。 对观察到的地下水位水平的水平和流场进行校准水文地质参数。 然后,该模型用于分析流量系统和地下水位变化的趋势。 建模结果表明,总充电总量为1216× 10 6 m 3 / a和总排出是1365× 10 6 m 用于建模时段的 3 / a,即149 m m 3 / sup> / a的地下水储存超过起草。 十年的预测表明,地下水位在当前地下水开采计划下的地区不断下降。

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