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Tracing and quantifying groundwater inflow into lakes using a simple method for radon 222 analysis

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Figure

Table 1. Different analytical methods and their detection limit. Counting times are typical values for the respective methods and are in partlimited by the increasing background from the drying medium, except if a water trap is used
Fig. 2.Figure 2: Test of the tightness of the sampling buckets. Several buckets were filled with the same water and then stored
Fig. 3.Rad H2 Comparison of the new method, called Rad Aqua Plus, withFigure 3: Comparison of the new method, called Rad Aqua Plus, with Rad HO measurements at different activites.2O measurements
Fig. 5. Summary of vertical radon profiles in the middle of LakeWillersinnweiher at station L2 (full symbols) and horizontal tran-sects including all stations in the main basin (open symbols), takenat different dates during the summer stratification period
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