The discharge of highly mineralised mine waters with
enhanced
226Ra and
228Ra activity concentrations has
affected creeks, rivers, sediments, soils, and plants along the
Lippe River and its tributaries.
226Ra activity concentrations were
elevated in all water samples receiving mine water, with
activity concentrations gradually decreasing with increased
distance from the colliery due to dilution and chemical
precipitation of radium with barium. Increased concentrations of
radium and radium decay products were also measured in sediments
and flood-affected soils. The sediments show an enrichment of
226Ra up to a factor of 750, while
the contaminated soils “only” reach a factor of 10. In aquatic
plants, a 4-fold increase in
226Ra activity concentrations was
measured downstream of the discharge points. The contamination
of the river banks and adjacent floodplain with radium is
responsible for enhanced gamma dose rates, which, along with the
incorporation of soil by playing children, provide potential
radiation exposure to the public.