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A numerical modelling and neural network approach to estimate the impact of groundwater abstractions on river flows

机译:估算地下水抽取对河流流量影响的数值建模和神经网络方法

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Evaluation of the impacts of groundwater abstractions on surface water systems is a necessary task in integrated water resources management. A range of hydrological, hydrogeological, and geomorphological factors influence the complex processes of interaction between groundwater and rivers. This paper presents an approach which uses numerical modeling of generic river-aquifer systems to represent the interaction processes, and neural networks to capture the impacts of the different controlling factors. The generic models describe hydrogeotogical settings representing most river-aquifer systems in England and Wales: high diffusivity (e.g. Chalk) and tow diffusivity (e.g. Triassic Sandstone) aquifers with flow to rivers mediated by alluvial gravels; the same aquifers where they are in direct connection with the river; and shallow alluvial aquifers which are disconnected from regional aquifers. Numerical model simulations using the SHETRAN integrated catchment modeling system provided outputs inctuding time-series and spatial variations in river flow depletion, and spatiatty distributed groundwater levels. Artificial neural network models were trained using input parameters describing the controlling factors and the outputs from the numerical model simulations, providing an efficient tool for representing the impacts of groundwater abstractions across a wide range of conditions. There are very few field data sets of accurately quantified river flow depletion as a result of groundwater abstraction under controlled conditions. One such data set from an experimental study carried out in 1967 on the Winterbourne stream in the Lambourne catchment over a Chalk aquifer was used successfully to test the modeling tool. This modeling approach provides a general methodology for rapid simulations of complex hydrogeological systems which preserves the physical consistency between multiple and diverse model outputs. (c) 2007 Published by Elsevier B.V.
机译:评估地下水提取对地表水系统的影响是水资源综合管理中的一项必要任务。一系列水文,水文地质和地貌因素影响着地下水与河流相互作用的复杂过程。本文提出了一种方法,该方法使用通用河水含水层系统的数值模型来表示相互作用过程,并使用神经网络来捕获不同控制因素的影响。通用模型描述了代表英格兰和威尔士大多数河流-含水层系统的水文地质背景:高扩散性(例如粉笔)和丝束扩散性(例如三叠纪砂岩)含水层,并由冲积砾石介导流向河流;与河直接相连的相同的含水层;和与区域含水层断开连接的浅冲积含水层。使用SHETRAN集成集水区建模系统进行的数值模型仿真提供了输出,包括河流流量枯竭的时间序列和空间变化,以及分布的地下水位。使用描述控制因素的输入参数和数值模型模拟的输出对人工神经网络模型进行了训练,从而提供了一种表示广泛条件下地下水抽取影响的有效工具。在受控条件下,由于抽取了地下水,因此很少有能准确量化河流流量枯竭的现场数据集。 1967年在Lambourne集水区Chalk含水层上的Winterbourne河上进行的一项实验研究获得的此类数据集已成功用于测试建模工具。这种建模方法为复杂水文地质系统的快速仿真提供了一种通用方法,该方法保留了多种模型输出之间的物理一致性。 (c)2007年由Elsevier B.V.

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