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Quantification of Stream Depletion Due to Aquifer Pumping Using Adjoint Methodology: A Case Study

机译:伴随方法定量分析含水层抽水引起的水流枯竭:一个案例研究

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Water availability for humans and the environment faces increasing threats from expanding populations and potential reduction in supply due to changes in climactic patterns. In light of these threats, the need to minimize stream depletion, defined as the depletion of flows in streams and rivers caused by groundwater pumping, becomes paramount. Stream depletion associated with pumping wells has been quantified by both analytical and numerical approaches; however, methods for identifying the stream depletion caused by new wells remain inefficient and require separate simulations for each potential well location. In this work, we develop adjoint equations of a coupled groundwater and surface water system that can be solved to calculate stream depletion. We use MODFLOW with the stream package to solve the adjoint equations, and, unlike previous work, we allow the head and resulting flow in the river to change as a result of depletion. With only one simulation of the adjoint equations, stream depletion can be calculated for a well at any location in the aquifer, making it an efficient method for siting future wells. A case study is presented comparing the stream depletion calculated using adjoint methodology with that found using traditional methods.
机译:由于气候模式的变化,人口增长和潜在的供应减少将使人类和环境的水供应面临越来越多的威胁。鉴于这些威胁,将最小化河流枯竭的需求变得至关重要,这被定义为由地下水泵抽引起的河流和河流中的水流枯竭。与抽水井有关的水流枯竭已经通过分析和数值方法进行了量化。但是,用于识别由新井引起的流耗的方法仍然效率低下,并且需要对每个潜在的井位置进行单独的模拟。在这项工作中,我们开发了地下水和地表水耦合系统的伴随方程,可以求解该方程以计算水流耗竭。我们将MODFLOW与流程序包结合使用来求解伴随方程,并且与以前的工作不同,我们允许河流中的水头和所产生的水流由于枯竭而发生变化。仅需对伴随方程进行一次模拟,就可以计算出含水层中任意位置处的一口井的水流消耗,这使其成为定位未来井的有效方法。提出了一个案例研究,将使用伴随方法计算的流耗与使用传统方法发现的流耗进行了比较。

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