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Towards improved instrumentation for assessing river-groundwater interactions in a restored river corridor

机译:致力于改进仪器,以评估恢复后的河道中的河水相互作用

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River restoration projects have been launched over the last two decades toimprove the ecological status and water quality of regulated rivers. As mostrestored rivers are not monitored at all, it is difficult to predictconsequences of restoration projects or analyze why restorations fail or aresuccessful. It is thus necessary to implement efficient field assessmentstrategies, for example by employing sensor networks that continuouslymeasure physical parameters at high spatial and temporal resolution. Thispaper focuses on the design and implementation of an instrumentationstrategy for monitoring changes in bank filtration, hydrologicalconnectivity, groundwater travel time and quality due to river restoration.We specifically designed and instrumented a network of monitoring wells atthe Thur River (NE Switzerland), which is partly restored and has been mainlychannelized for more than 100 years. Our results show that bankfiltration – especially in a restored section with alternating riverbedmorphology – is variable in time and space. Consequently, our monitoring network has been adapted inresponse to that variability. Although not available at our test site, weconsider long-term measurements – ideally initiated before and continuedafter restoration – as a fundamental step towards predicting consequencesof river restoration for groundwater quality. As a result, process-basedmodels could be adapted and evaluated using these types of high-resolutiondata sets.
机译:在过去的二十年中,已经启动了河流修复项目,以改善受管制河流的生态状况和水质。由于根本没有对大多数恢复河流进行监控,因此很难预测恢复项目的后果或分析恢复失败或成功的原因。因此,有必要实施有效的现场评估策略,例如通过采用以高时空分辨率连续测量物理参数的传感器网络。本文着重于仪器仪表策略的设计和实施,以监测由于河流修复而引起的河岸过滤,水文连通性,地下水传播时间和水质的变化。我们专门设计并安装了图尔河(瑞士东北)的监测井网络已恢复,并已主要引导100多年。我们的结果表明,河床渗流(尤其是在河床形态交替的恢复区)在时间和空间上是可变的。因此,我们的监控网络已针对这种变化进行了调整。尽管无法在我们的测试现场进行,但我们考虑进行长期测量(理想情况下是在恢复之前进行并在恢复之后继续进行),这是预测河流恢复对地下水质量后果的基本步骤。结果,可以使用这些类型的高分辨率数据集来调整和评估基于过程的模型。

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