Distribution and partitioning of depleted uranium (DU) in soils at weapons test ranges - investigations combining the BCR extraction scheme and isotopic analysis

Depleted uranium (DU) has become a soil contaminant of considerable concern in many combat zones and weapons-testing sites around the world, including locations in Europe, the Middle East and the USA, arising from its dispersion via the application of DU-bearing munitions. Once DU is released into the environment its mobility and bioavailability will, like that of other contaminants, largely depend on the type of associations it forms in soil and on the nature of the soil components to which it binds. In this study we used the BCR sequential extraction scheme to determine the partitioning of DU amongst soil fractions of texturally varying soils from locations affected by weapons-testing activities. Isotopic analyses (MC-ICP-MS and alpha-spectrometry) were performed to verify the presence of DU in whole soils and soil fractions and to determine any preferential partitioning of the contaminant. Results identified soil organic matter as being consistently the most important component in terms of DU retention, accounting for 30-100% of DU observed in the soils examined. However, at greater distances from known contamination points, DU was also found to be largely associated with the exchangeable fraction, suggesting that DU can be mobilised and transported by surface and near-surface water and does remain in an exchangeable (and thus potentially bioavailable) form in soils.     

Comparative hersistence of chlorpyrifos in a mineral soil after granular and drench applications

Abstract

Lorsban 15G (15% chlorpyrifos) at 1.6 and 2.2 g a.i./10 m row, and Lorsban 4E (40.7% chlorpyrifos) at 2.0 g a.i./10 m row were applied respectively to a silt loam soil as a band treatment at seeding and as a drench after seeding. The rate of disappearance of chlorpyrifos [Q,Q‐diethyl Q‐(3,5,6‐trichloro‐2‐pyridinyl) phosphorothioate] was relatively fast in the first 15 days but slowed down considerably thereafter regardless of the methods of application and application rates; and there was a statistically significant (p=0.05) linear relationship between the natural logarithm of chlopyrifos concentration and time. Based on the linear regression equations, the calculated pseudo‐first‐order rate constants were 0.041 day^‐1 and 0.044 day^‐1 respectively for the band treatments at 1.6 and 2.2 g a.i./10 m row; and 0.040 day^‐1 for the drench. The calculated half‐lives for all three treatments were similar and they ranged frcm 15.8 days to 17.3 days. The degradation product 3,5,6‐trichloro‐2‐pyridinol (TP) was detected in soil but not 3,5_/6‐trichloro‐2‐methoxypyridine (TMP). The concentration of TP increased steadily to a peak and declined thereafter. The highest mean concentration of TP was 2.21 ppm (dry wt) detected 29 days after band treatment at the high rate. After 90 days the concentration of TP decreased to 0.43 ppm (dry wt).