“…As a consequence, 222 Rn is normally in great radioactive disequilibrium with its parent 226 Ra nuclide in groundwater. The 222 Rn activity concentration in groundwater mostly varies in the broad interval between 1 Bq/dm 3 and 1000 Bq/dm 3 Kahlos, 1979, 1980;Bonotto, 2004;Dillon et al, 1991;Zhuo et al, 2001), but local concentrations up to 10 000 Bq/dm 3 or more have been reported in the literature (e.g. Brutsaert et al, 1981).…”