Ibrahim S A, Whicker F W, Simon S L
Department of Radiology and Radiation Biology, Colorado State University, Fort Collins 80523.
Health Phys. 1990 Mar;58(3):321-8. doi: 10.1097/00004032-199003000-00010.
Ground concentrations of 226Ra and total alpha activity as a function of soil depth and distance from an acidic U mill tailings pile were measured, as well as soil pH, sulfate, chloride, and conductivity. Contamination decreased with increasing soil depth and distance from the source. Most of the measured parameters were indistinguishable from background after a distance of 3.3 km from the tailings impoundment. The highest concentrations of all contaminants were contained in the particles less than 0.045 mm in diameter at the soil surface (0-0.6 cm). This fraction represents only 4% to 10% of the total soil mass. Surface soil particles greater than 2.0 mm contained higher concentrations of all contaminants than the intermediate-size (0.045-2.0 mm) fraction. Aggregate formation of the greater than 2.0-mm fraction from small particles or preferential erosion and transport of the tailings sand fractions were proposed as possible explanations. The significant correlations between various measurements were soil 226Ra vs. total alpha activity, sulfate concentration, and conductivity. The latter two parameters are indicative of sulfuric acid leached tailings. The sulfate concentration appeared to be a sensitive and easily measured indicator of tailings contamination and migration into the soil profile. Furthermore, sulfate may be used to delineate acidic U tailings from other sources of contamination (U ore dust, yellowcake, naturally elevated U and Ra) in the environment. Actual site measurements for surface 226Ra concentration were approximately twice the MILDOS computer code prediction.
