2011
DOI: 10.1016/j.gca.2010.10.011
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Formation of uranium(IV)-silica colloids at near-neutral pH

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Cited by 61 publications
(94 citation statements)
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References 79 publications
(96 reference statements)
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“…To explain their results, they speculated that U(IV) colloids enhanced the observed U(IV) solubility in experiments with groundwater from granitic bedrock, a uranium ore deposit or porewater from Boom Clay, respectively. While U(VI) mobility in association with colloids has been documented in the field [23][24][25] , and recent laboratory studies evidenced the formation of U(IV) silicate colloids r20 nm in size 26 and that of U IV O 2 colloids 27 , this study is the first to demonstrate the association of U(IV) with colloids in natural environments and its resulting increased mobility.…”
Section: Discussionmentioning
confidence: 59%
“…To explain their results, they speculated that U(IV) colloids enhanced the observed U(IV) solubility in experiments with groundwater from granitic bedrock, a uranium ore deposit or porewater from Boom Clay, respectively. While U(VI) mobility in association with colloids has been documented in the field [23][24][25] , and recent laboratory studies evidenced the formation of U(IV) silicate colloids r20 nm in size 26 and that of U IV O 2 colloids 27 , this study is the first to demonstrate the association of U(IV) with colloids in natural environments and its resulting increased mobility.…”
Section: Discussionmentioning
confidence: 59%
“…The autocorrelation functions, C ( τ ), were calculated from the fluctuations of the scattered light intensity to estimate the hydrodynamic radii (i.e., Stokes radii) of the particles in the samples 18. The Cumulant expansion and the CONTIN analysis were employed to derive the particle size information based on the obtained C ( τ ) 41. For the measurements of aging effect, the samples were triply sealed in a glass cuvette and stored in a N 2 ‐filled inert glove box between the measurements, to avoid possible penetration of air into the samples.…”
Section: Methodsmentioning
confidence: 99%
“…Furthermore: (a) the precipitation of U VI ? U IV depending on concentration of silicates in sediments may caused the formation of U IV -silica colloids (Dreissig et al 2011). The U-O-Si bond formation has been observed in those forms, where the coordination environment has been found comparable to coffinite (USiO 4 ); and (b) study of the uranium distribution in sediments in the environmental area near to nuclear waste storage has been shown that the uranium mobility curtailed via the precipitation of silicates and phosphates (Um et al 2010).…”
Section: Introductionmentioning
confidence: 97%