2015
DOI: 10.1016/j.chemgeo.2015.02.006
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Modeling plutonium sorption to kaolinite: Accounting for redox equilibria and the stability of surface species

Abstract:  Two pH-pe diagrams for Pu are drawn for (i) the solution and (ii) the surface. Pu sorption and redox speciation can be predicted. The redox potential is crucial information: it controls Pu overall sorption. This approach can be applied to other minerals and actinides.

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Cited by 26 publications
(28 citation statements)
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“…As previously inferred for actinide uptake on clays, the redox speciation of actinides is influenced by the formation of surface complexes [21][22][23]. The Pu(IV)/Pu(III) borderline at the illite surface (denoted as {Pu(IV)/Pu(III)} surf ) is expected to depend on the individual Pu(IV) and Pu(III) sorption behavior [22][23], and can be calculated for = 0.1, 1.0 and 3.2 m (Fig.…”
Section: Modeling Resultsmentioning
confidence: 83%
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“…As previously inferred for actinide uptake on clays, the redox speciation of actinides is influenced by the formation of surface complexes [21][22][23]. The Pu(IV)/Pu(III) borderline at the illite surface (denoted as {Pu(IV)/Pu(III)} surf ) is expected to depend on the individual Pu(IV) and Pu(III) sorption behavior [22][23], and can be calculated for = 0.1, 1.0 and 3.2 m (Fig.…”
Section: Modeling Resultsmentioning
confidence: 83%
“…When different Pu redox states coexist, the overall uptake of actinides on clays highly depends on pe [21][22][23]. As pointed out before, R d data scatter at acidic pH m , which might be due to slight variations in redox conditions in individual batch experiments.…”
Section: Modeling Resultsmentioning
confidence: 96%
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