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以上海市浦西地区第二承压含水层和第三承压含水层为例 ,利用实际资料以及部分插值的方法 ,建立了该区地下水系统完整三维数学模型 ,较好地解决了相对隔水层缺失区越流系数无法调试的问题 ,为上海市整个地下水含水系统建立完整三维水流模型以及沉降模型奠定了基础。
Taking the second confined aquifer and the third confined aquifer in Puxi area of Shanghai as an example, a complete three-dimensional mathematical model of the groundwater system in the area was established by using actual data and partial interpolation method, which solved the problem that the relative aquitard The problem of inability to debug the missing current flow coefficient can lay a foundation for the establishment of complete three-dimensional flow model and settlement model for the entire groundwater aquifer system in Shanghai.