2014
DOI: 10.1080/10643389.2012.728522
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Reoxidation of Biogenic Reduced Uranium: A Challenge Toward Bioremediation

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Cited by 34 publications
(21 citation statements)
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“…Error bars indicate the standard deviation association of biogenic U(IV) with proteins and EPS, associated with the biomass, makes its unlikely to be transported as colloidal phases (Bargar et al 2008). However, after U bioreduction, Fe(III)hydroxide minerals as well as Fe sulfide minerals, reduced organic matter, electron shuttles could be controlling factors for the transport and long-term stability of bioreduced U (Singh et al 2014). Wang et al (2013) report mobile U(IV)-bearing colloids in a mining-impacted wetland demonstrating the presence of U(IV) in soil as a noncrystalline species bound to amorphous Al-P-Fe-Si aggregates, whereas in porewater, as a distinct species associated with Fe and organic matter colloids.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…Error bars indicate the standard deviation association of biogenic U(IV) with proteins and EPS, associated with the biomass, makes its unlikely to be transported as colloidal phases (Bargar et al 2008). However, after U bioreduction, Fe(III)hydroxide minerals as well as Fe sulfide minerals, reduced organic matter, electron shuttles could be controlling factors for the transport and long-term stability of bioreduced U (Singh et al 2014). Wang et al (2013) report mobile U(IV)-bearing colloids in a mining-impacted wetland demonstrating the presence of U(IV) in soil as a noncrystalline species bound to amorphous Al-P-Fe-Si aggregates, whereas in porewater, as a distinct species associated with Fe and organic matter colloids.…”
Section: Resultsmentioning
confidence: 99%
“…At least three different types of biogenic U(IV) have been observed: crystalline uraninite, nanoparticulate uraninite, and mononuclear U(IV) (Maleke et al 2015;Zhou et al 2014a, b;Singh etal.2014;Boyanov et al 2011;Fletcher et al 2010;Bernier-Latmani et al 2010). These reduced forms of U are prone to re-oxidation, raising questions regarding long-term U remediation and site stewardship (Singh et al 2014;Spycher et al 2011;Moonetal.2009;Beyenal et al 2004). Following the microbial reduction of U(VI) to U(IV), the second step in biogenic U(IV) formation entails the aggregation of the precipitated mineral.…”
Section: Introductionmentioning
confidence: 99%
“…Heavy metal and radioactive cations, of course, cannot be decomposed but have their solubility lowered or reduced, e.g. by a change in oxidation state and (Singh et al, 2013), so that they become less harmfully in the ground, or might be removed by phytoremediation or myco-remediation, which involves harvesting the fungus.…”
Section: Bioremediation Using Mushroommentioning
confidence: 99%
“…Heavy metal and radioactive cations, of course, cannot be decomposed but can be rendered into forms of low solubility, e.g. by a change in oxidation state, such as U (IV) (in UO 2 ) (Singh et al, 2014), so that they remain less harmfully in the ground, or might be physically removed by phytoremediation or mycoremediation, which involves harvesting the plant or fungus.…”
Section: The Issue Of Contaminated Landmentioning
confidence: 99%