Dietmaier Annette, Baumann Thomas
TUM School of Engineering and Design, Chair of Hydrogeology, Technical University Munich, Arcisstr. 21, Munich, 80333 Bavaria Germany.
Water Resour Manag (Dordr). 2023 May 16:1-18. doi: 10.1007/s11269-023-03529-6.
Deep groundwater aquifers are exploited for a variety of purposes. In general, impermeable rock layers protect these aquifers from anthropogenic influences. As such, they are a last resort for groundwater in a pre-industrial state, and a crucial resource in cases of emergency, such as floods contaminating shallow groundwater. The EU Water Framework Directive (WFD) provides the regulatory framework to protect its quality and quantity. Recent monitoring of the hydrochemical state of Upper Jurassic wells in Bavaria and Austria has shown fluctuations that were connected to new exploitation activities and might indicate an unsustainable development of the aquifer. We propose a new workflow in accordance with the WFD which uses clustering algorithms to assess these fluctuations. Our data consists of 5 to 42 hydrochemical analyses per well with yearly sampling intervals spanning up to 30 years. From the cluster analysis we derived thresholds for two corridors: Natural Range Corridor (NC) and Action Corridor (AC). While the NC represents a well-specific natural variation range, the AC hints towards unsustainable development and should trigger a detailed (re)assessment. To show the potential of the new method, the workflow was applied to two wells with different geological characteristics. Distinct fluctuation events were clearly recognized and can be used in the context of an early warning system, such that malign hydrochemical variations can be detected before they become legally problematic to well operators. Our workflow thus provides a novel, robust, and reproducible method to assess the grade of sustainability at which a well is exploited and ensures a good status of a unique and important resource.
The online version contains supplementary material available at 10.1007/s11269-023-03529-6.
深层地下含水层被用于各种目的。一般来说,不透水岩层保护这些含水层免受人为影响。因此,它们是处于工业化前状态的地下水的最后手段,也是在诸如洪水污染浅层地下水等紧急情况下的关键资源。欧盟水框架指令(WFD)提供了保护其质量和数量的监管框架。最近对巴伐利亚和奥地利上侏罗统井的水化学状态进行的监测显示,波动与新的开采活动有关,这可能表明含水层的开发不可持续。我们根据WFD提出了一种新的工作流程,该流程使用聚类算法来评估这些波动。我们的数据包括每口井5至42次水化学分析,每年采样一次,时间跨度长达30年。通过聚类分析,我们得出了两条走廊的阈值:自然范围走廊(NC)和行动走廊(AC)。虽然NC代表特定于井的自然变化范围,但AC暗示着不可持续的发展,应触发详细的(重新)评估。为了展示新方法的潜力,该工作流程被应用于两口具有不同地质特征的井。明显识别出了不同的波动事件,这些事件可用于预警系统,以便在对井运营商产生法律问题之前检测到有害的水化学变化。因此,我们的工作流程提供了一种新颖、稳健且可重复的方法来评估井的开采可持续性等级,并确保一种独特而重要资源的良好状态。
在线版本包含可在10.1007/s11269-023-03529-6获取的补充材料。