Effects of Progressive Anoxia on the Solubility of Technetium in Sediments

Citations Over TimeTop 10% of 2005 papers

Abstract

Technetium is a significant radioactive contaminant from nuclear fuel cycle operations. It is highly mobile in its oxic form (as Tc(VII)O4-) but is scavenged to sediments in its reduced forms (predominantly Tc(IV)). Here we examine the behavior of Tc at low concentrations and as microbial anoxia develops in sediment microcosms. A cascade of stable-element terminal-electron-accepting processes developed in microcosms due to indigenous microbial activity. TcO4- removal from solution occurred during active microbial Fe(III) reduction, which generated Fe(II) in the sediments and was complete before sulfate reduction began. Microbial community analysis revealed a similar and complex microbial population at all three sample sites. At the intermediate salinity site, PauII, a broad range of NO3-, Mn(IV), Fe(III), and SO4(2-) reducers were present in sediments including microbes with the potential to reduce Fe(III) to Fe(II), although no differences in the microbial population were discerned as anoxia developed. When sterilized sediments were incubated with pure cultures of NO3(-)-, Fe(III)-, and sulfate-reducing bacteria, TcO4- removal occurred during active Fe(III) reduction. X-ray absorption spectroscopy confirmed that TcO4- removal was due to reduction to hydrous Tc(IV)O2 in Fe(III)- and sulfate-reducing estuarine sediments.

Related Papers

• → Fate and Stereoselective Behavior of Benalaxyl in a Water–Sediment Microcosm(2015)23 cited
• → A latest review on the application of microcosm model in environmental research(2021)9 cited
• → Factors controlling the removal of sulfate and acidity from the waters of an acidified lake(1989)13 cited
• → Microcosms as potential screening tools for evaluating transport and effects of toxic substances(1980)20 cited
• → A Subsystem Microcosm Verification of the Microcosm N-System(2019)