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Spatial distribution of anthropogenic inputs into groundwater: a case study

机译:人为进入地下水的空间分布 - 以案例研究

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摘要

At the Hardwald study site, Switzerland, 15million cubic metres per year of drinking water is being pumped. Chlorinated compounds, however, have been detected in the groundwater. Wepresent results from field sampling and lab analyses to determine thespatial distribution of chlorinated organic compounds, stable water isotopes (O-18 und D-2), major ions as well as selectedmicropollutants, which enter the groundwater by artificial recharge. Wedemonstrate that artificial groundwater recharge is essential forwater security and that the pumped groundwater has aclose chemical signature to that of the recharged river water. However, due to the heterogeneousinfiltration, Muschelkalk water from the regional flow system is mixed with therecently infiltrated water in the south-west.This interpretation is basedon the spatial distribution of chlorinated organic compounds, stable water isotopes, major ions as well as selected micropollutants.Despite the complex boundary conditions, the interaction betweenartificial recharge and pumping provides asecure drinking watersupply.
机译:在瑞士的Hardwald学习网站,每年1500万立方米正在泵送。然而,已经在地下水中检测到氯化化合物。来自现场采样和实验室分析的Wepresent结果,以确定氯化有机化合物,稳定的水同位素(O-18和D-2),主要离子以及选择的霉菌蛋解物,通过人工补给进入地下水的缺血性。威尔斯汀认为人造地下水充电是必不可少的措施安全性,并且泵浦地下水对充电河水的泵送了化学签名。然而,由于异源素,来自区域流动系统的Muschelkalk水与西南部的渗透水混合。这一解释是系,氯化有机化合物,稳定的水同位素,主要离子以及所选微孔的空间分布。尽管存在复杂的边界条件,但互动之间的互补和泵送提供了不可饮用水饮料。

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