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Tracing mineral water in the artesian karst aquifer of Stuttgart (SW Germany)

机译:在斯图加特(德国西南部)的自流喀斯特喀斯特含水层中追踪矿泉水

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The artesian mineral springs in the city of Stuttgart are discharged from a complex regional karst system in Triassic carbonate rocks. The mineral water had already been used in Roman times and is still used today for cures and in three leisure pools. Since 1984, contamination with chlorinated solvents in very low concentrations has been observed in some springs. Within the framework of a long-term research program, two multi tracer tests were carried out in the catchment of the springs in order to investigate the hydraulic properties of the karst aquifer and the mechanisms of contaminant transport. The fluorescent dyes Naphthionate, Eosine and Pyranine as well as microspheres and Lycopodium spores were used as tracers. The best results were obtained with Naphthionate while Pyranine was completely decayed in the groundwa-ter. The results of the tracer tests are essential both for risk assessment and for developing protection strategies.
机译:斯图加特市的自流矿物泉是从三叠纪碳酸盐岩中复杂的区域岩溶系统中排出的。矿泉水已经在罗马时代使用过,如今仍用于治疗和用于三个休闲泳池。自1984年以来,在某些温泉中已观察到低浓度氯化溶剂的污染。在长期研究计划的框架内,对泉水进行了两次多示踪剂测试,以研究岩溶含水层的水力特性和污染物运移的机理。荧光染料萘硫酸盐,曙红和吡喃以及微球和石蒜孢子被用作示踪剂。用萘硫酮获得最好的结果,而吡喃胺在地下水中完全被腐烂。示踪剂测试的结果对于风险评估和制定保护策略都是必不可少的。

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