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首页> 外文期刊>Journal of the American Water Resources Association >EVALUATION OF A STREAM AQUIFER ANALYSIS TEST USING ANALYTICAL SOLUTIONS AND FIELD DATA
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EVALUATION OF A STREAM AQUIFER ANALYSIS TEST USING ANALYTICAL SOLUTIONS AND FIELD DATA

机译:利用分析解决方案和现场数据评估流域含水层分析测试

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Considerable advancements have been made in the development of analytical solutions for predicting the effects of pumping wells on adjacent streams and rivers. However, these solutions have not been sufficiently evaluated against field data. The objective of this research is to evaluate the predictive performance of recently proposed analytical solutions for unsteady stream depletion using field data collected during a stream/aquifer analysis test at the Tamarack State Wildlife Area in eastern Colorado. Two primary stream/aquifer interactions exist at the Tamarack site: (1) between the South Platte River and the alluvial aquifer and (2) between a backwater stream and the alluvial aquifer. A pumping test is performed next to the backwater stream channel. Drawdown measured in observation wells is matched to predictions by recently proposed analytical solutions to derive estimates of aquifer and streambed parameters. These estimates are compared to documented aquifer properties and field measured streambed conductivity. The analytical solutions are capable of estimating reasonable values of both aquifer and streambed parameters with one solution capable of simultaneously estimating delayed aquifer yield and stream flow recharge. However, for long term water management, it is reasonable to use simplified analytical solutions not concerned with early-time delayed yield effects. For this site, changes in the water level in the stream during the test and a varying water level profile at the beginning of the pumping test influence the application of the analytical solutions.
机译:在开发用于预测抽水井对邻近河流和河流的影响的分析解决方案方面已取得了相当大的进步。但是,尚未针对现场数据充分评估这些解决方案。这项研究的目的是使用在科罗拉多州东部塔玛拉克州野生动物保护区进行的河流/含水层分析测试期间收集的现场数据,评估最近提出的非恒定流耗竭分析解决方案的预测性能。塔玛拉克(Tamarack)站点存在两种主要的水流/含水层相互作用:(1)南普拉特河和冲积层之间,以及(2)回水流和冲积层之间。在回水流道旁边进行抽水测试。通过最近提出的分析解决方案,在观测井中测得的压降与预测值相匹配,以得出含水层和流床参数的估计值。将这些估计值与记录的含水层特性和现场测量的流化床电导率进行比较。该分析解决方案能够估算含水层参数和流床参数的合理值,而一种解决方案则能够同时估算延迟的含水层产量和水流补给量。但是,对于长期的水管理,使用与早期延迟产量影响无关的简化分析解决方案是合理的。对于此站点,测试过程中溪流中水位的变化以及抽水测试开始时水位曲线的变化会影响分析溶液的应用。

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