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采用 H/He 表观年龄与现场氦分析相结合的方法,识别城市地区地下水流动过程和全氯乙烯(PCE)的迁移。

Combined method of H/He apparent age and on-site helium analysis to identify groundwater flow processes and transport of perchloroethylene (PCE) in an urban area.

机构信息

Department of Water Resources and Drinking Water, Eawag, Swiss Federal Institute of Aquatic Science and Technology, Dübendorf, Switzerland.

Department of Water Resources and Drinking Water, Eawag, Swiss Federal Institute of Aquatic Science and Technology, Dübendorf, Switzerland; Department of Environmental Systems Science, ETH Zurich, Zurich, Switzerland.

出版信息

J Contam Hydrol. 2021 Mar;238:103773. doi: 10.1016/j.jconhyd.2021.103773. Epub 2021 Jan 22.

DOI:10.1016/j.jconhyd.2021.103773
PMID:33540239
Abstract

Urban groundwater management requires a thorough and robust scientific understanding of flow and transport processes. H/He apparent ages have been shown to efficiently help provide important groundwater-related information. However, this type of analysis is expensive as well as labor- and time-intensive, and hence limits the number of potential sampling locations. To overcome this limitation, we established an inter-relationship between H/He apparent groundwater ages and He concentrations analyzed in the field with a newly developed portable gas equilibrium membrane inlet mass spectrometer (GE-MIMS) system, and demonstrated that the results of the simpler GE-MIMS system are an accurate and reliable alternative to sophisticated laboratory based analyses. The combined use of H/He lab-based ages and predicted ages from the H/He-He age relationship opens new opportunities for site characterization, and reveals insights into the conceptual understanding of groundwater systems. For our study site, we combined groundwater ages with hydrochemical data, water isotopes (O and H), and perchloroethylene (PCE) concentrations (1) to identify spatial inter-aquifer mixing between artificially infiltrated groundwater and water originating from regional flow paths and (2) to explain the spatial differences in PCE contamination within the observed groundwater system. Overall, low PCE concentrations and young ages occur when the fraction of artificially infiltrated water is high. The results obtained from the age distribution analysis are strongly supported by the information gained from the isotopic and hydrochemical data. Moreover, for some wells, fault-induced aquifer connectivity is identified as a preferential flow path for the transport of older groundwater, leading to elevated PCE concentrations.

摘要

城市地下水管理需要对流动和传输过程有透彻而强大的科学理解。氚/氦表观年龄已被证明可以有效地提供有关地下水的重要信息。然而,这种分析既昂贵又耗费大量的人力和时间,因此限制了潜在采样点的数量。为了克服这一限制,我们建立了氚/氦表观地下水年龄与现场分析的氦浓度之间的关系,利用新开发的便携式气体平衡膜进样质谱仪(GE-MIMS)系统,证明了更简单的 GE-MIMS 系统的结果是一种准确可靠的替代复杂实验室分析的方法。氚/氦实验室年龄与氚/氦-氦年龄关系预测年龄的结合使用为场地特征化开辟了新的机会,并深入了解了地下水系统的概念理解。在我们的研究地点,我们将地下水年龄与水文化学数据、水同位素(O 和 H)和全氯乙烯(PCE)浓度(1)相结合,以识别人工渗透地下水与源自区域流径的水之间的空间含水层间混合,(2)解释观测地下水系统中 PCE 污染的空间差异。总体而言,当人工渗透水的比例较高时,PCE 浓度较低且年龄较小。年龄分布分析的结果得到了同位素和水文化学数据信息的有力支持。此外,对于一些井,断层诱导的含水层连通性被确定为输送旧地下水的优先流径,导致 PCE 浓度升高。

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