Quantifying technetium and strontium bioremediation potential in flowing sediment columns.

摘要

The high-yield fission products Tc and Sr are found as problematic radioactive contaminants in groundwater at nuclear sites. Treatment options for radioactively contaminated land include bioreduction approaches and this paper explores mTc and Sr behaviour and stability under a range of biogeochemical conditions stimulated by electron donor addition methods. Dynamic column experiments with sediment from the Sellafield nuclear facility, completed at site relevant flow conditions, demonstrated that Fe(III)-reducing conditions had developed by 60 days. Sediment reactivity towards Tc was then probed using a Tc(VII) tracer at <10 mol L and gamma camera imaging showed full retention of Tc in acetate amended systems. Sediment columns were then exposed to selected treatments to examine the effects of different acetate amendment regimes and reoxidation scenarios over 55 days when they were again imaged with Tc. Here, partially oxidized sediments with no further electron donor additions remained reactive towards 99mTc under relevant groundwater O and NO concentrations over 55 days. Immobilization of Tc was highest where continuous acetate amendment had resulted in sulfate-reducing conditions. Interestingly, the sulfate reducing system showed enhanced Sr retention when stable Sr was added continuously as a proxy for Sr. Overall, sediment reactivity was non-destructively imaged over an extended period to provide new information about dynamic iron and radionuclide biogeochemistry throughout realistic sediment redox cycling regimes.