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Integrating Bayesian Groundwater Mixing Modeling With On-Site Helium Analysis to Identify Unknown Water Sources

机译:结合贝叶斯地下水混合模型和现场氦气分析来识别未知水源

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Analyzing groundwater mixing ratios is crucial for many groundwater management tasks such as assessing sources of groundwater recharge and flow paths. However, estimating groundwater mixing ratios is affected by various uncertainties, which are related to analytical and measurement errors of tracers, the selection of end-members, and finding the most suitable set of tracers. Although these uncertainties are well recognized, it is still not common practice to account for them. We address this issue by using a new set of tracers in combination with a Bayesian modeling approach, which explicitly considers the possibility of unknown end-members while fully accounting for tracer uncertainties. We apply the Bayesian model we developed to a tracer set, which includes helium (He-4) analyzed on site to determine mixing ratios in groundwater. Thereby, we identify an unknown end-member that contributes up to 84 +/- 9% to the water mixture observed at our study site. For the He-4 analysis, we use a newly developed Gas Equilibrium Membrane Inlet Mass Spectrometer (GE-MIMS), operated in the field. To test the reliability of on-site He-4 analysis, we compare results obtained with the GE-MIMS to the conventional lab-based method, which is comparatively expensive and labor intensive. Our work demonstrates that (i) tracer-aided Bayesian mixing modeling can detect unknown water sources, thereby revealing valuable insights into the conceptual understanding of the groundwater system studied, and (ii) on-site He-4 analysis with the GE-MIMS system is an accurate and reliable alternative to the lab-based analysis.
机译:分析地下水混合比对于许多地下水管理任务至关重要,例如评估地下水的补给和流动路径。但是,估算地下水混合比会受到各种不确定性的影响,这些不确定性与示踪剂的分析和测量误差,末端成员的选择以及寻找最合适的示踪剂有关。尽管这些不确定性已得到公认,但仍无法解决这些不确定性。我们通过使用一组新的示踪剂与贝叶斯建模方法相结合来解决此问题,该方法明确考虑了未知最终成员的可能性,同时充分考虑了示踪剂的不确定性。我们将开发的贝叶斯模型应用于示踪剂组,该示踪剂组包括现场分析的氦气(He-4),以确定地下水中的混合比。因此,我们确定了一个未知的最终成员,该成员对我们研究现场观察到的水混合物的贡献高达84 +/- 9%。对于He-4分析,我们使用了在现场运行的新开发的气体平衡膜进气质谱仪(GE-MIMS)。为了测试现场He-4分析的可靠性,我们将GE-MIMS获得的结果与传统的基于实验室的方法进行比较,该方法相对昂贵且劳动强度大。我们的工作表明,(i)示踪剂辅助的贝叶斯混合模型可以检测未知的水源,从而揭示了对所研究的地下水系统的概念理解的宝贵见解,以及(ii)使用GE-MIMS系统进行的He-4现场分析是基于实验室的分析的准确而可靠的替代方法。

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