The Swiss Federal Institute of Aquatic Science and Technology (Eawag) and their partners at CHYN and Rhesi used a miniRUEDI to track the groundwater flow near a large channelized river. The river bed was excavated to simulate a natural erosion event, as it might occur after river revitalisation. Different groundwater flow paths were artificially spiked with different noble gases, and their break-through curves at a nearby pumping well were monitored with a miniRUEDI. The spiking was repeated several times over a period of one year. These measurements show how the river/groundwater exchange evolves in response to the excavation and to the «healing» of the eroded river bed. This new tracer tool and the resulting insights will be important for groundwater management and drinking water production near revitalised river systems.
