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3D hydraulic modeling of a complex alluvial aquifer for groundwater resource management

机译:3D地下水资源管理复合激发含水层的水力建模

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Many cities take nearby alluvial aquifers as their main resource of water supply. Therefore the aquifers, especially shallow aquifers, are always under either the influence of extreme hydrological events, or the threat of pollutants that are generated by the intense urban developments. To ensure an efficient management of water supply regarding both quantity and quality aspect, it requires a good knowledge of the dynamics of the aquifer. Characterizing the exchanges that could exist with free surface flow in associated rivers is one of the key issues. The most efficient way to understand the behaviour of the aquifer is to implement a 3D physically-based hydrodynamic model that can represent all physical processes. However, this approach, in order to become an operational tool, requests a structured methodology for data integration and validation. In this paper, a 3D hydraulic model of the Var lower valley is set up with FEFLOW modeling system. All the important hydrological processes such as precipitation, evapotranspiration, river-aquifer exchanges are considered. Despite a very complex and partially known geological structure, the results for a simulation of 1266 days demonstrate that the model is able to provide an accurate diagnostic on various hydraulic structures that are affecting the aquifer and may induced management difficulties. The proposed approach answers the current management demand and can provide efficient support within the underground resource exploitation.
机译:许多城市将附近的含水层作为其主要供水资源。因此,含水层,尤其是浅含水层,总是在极端水文事件的影响下,或强烈的城市发展产生的污染物的威胁。为了确保有关数量和质量方面的供水管理,需要良好地了解含水层的动态。在关联河流中使用自由表面流存在的交换表征是关键问题之一。理解含水层行为的最有效方法是实现可以代表所有物理过程的3D物理基础的流体动力学模型。但是,这种方法是为了成为操作工具,请求结构化方法进行数据集成和验证。本文使用Feflow建模系统建立了VAL下谷的3D水力模型。考虑了所有重要的水文过程,如沉淀,蒸散蒸腾,河流交换。尽管具有非常复杂和部分已知的地质结构,但模拟的结果为1266天,表明该模型能够在影响含水层的各种液压结构上提供准确的诊断,并且可能引起管理困难。建议的方法回答了当前的管理需求,可以在地下资源开发中提供有效的支持。

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