Leaching of depleted uranium in soil as determined by column experiments

The basic features of the leachability of depleted uranium (DU) projectiles in soil was investigated by using 12 projectiles (145–294 g DU) and 16 columns installed in an air-conditioned laboratory. Two soils widely distributed in Europe, a sandy-loamy cambisol and a silty-loamy luvisol, were filled into the columns (3.3 kg dry soil each). The effluents of all columns were collected weekly during the observation period of 1 year. In 648 samples, ²³⁵U and ²³⁸U were determined by inductively coupled plasma mass spectrometry. The leaching rates of ²³⁸U from natural uranium were in general about 0.01 μg week^-1 or smaller, while those of ²³⁸U from the DU munitions varied considerably and reached values of up to 100 μg week^-1, for the different columns. In total, about 0.3 μg natural uranium corresponding to 20 ppm of its inventory in the soil was leached during the observation period. From the projectiles, an average of about 50 μg DU were leached corresponding to 18 ppm of the corroded DU mass (about 1.6% of the mean initial DU mass of the projectiles). Assuming that corrosion and leaching continue as observed, the mobilisation of ²³⁸U from DU munitions will last, on an average, for thousands of years in the soils investigated, while the munitions themselves will have been corroded after a much shorter time. It is proposed to use, for the investigated soil types, the mean leaching rates of the six columns with projectiles for transport calculations of ²³⁸U to the groundwater and, thus, for a better risk assessment of the water-dependent uptake pathways of DU.