2010
DOI: 10.5516/net.2010.42.5.552
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Effect of Carbonate on the Solubility of Neptunium in Natural Granitic Groundwater

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Cited by 8 publications
(7 citation statements)
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“…Interestingly, this lower solubility coincides with a higher static order as reflected by lower Debye–Waller factor of the Np-Np paths as compared to the 1 day sample (Table ). Even addition of a high concentration of carbonate (0.1 M) had only a relatively small influence on Np retention, in line with previous results. , …”
Section: Environmental Implicationssupporting
confidence: 92%
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“…Interestingly, this lower solubility coincides with a higher static order as reflected by lower Debye–Waller factor of the Np-Np paths as compared to the 1 day sample (Table ). Even addition of a high concentration of carbonate (0.1 M) had only a relatively small influence on Np retention, in line with previous results. , …”
Section: Environmental Implicationssupporting
confidence: 92%
“…Even addition of a high concentration of carbonate (0.1 M) had only a relatively small influence on Np retention, in line with previous results. 58,59 The observed high retention of Np by siderite across a relatively wide pH range is encouraging. However, the potential mobilization of the formed NpO 2 −like nanoparticles as colloids may significantly raise the risk of Np migration away from the waste disposal site.…”
Section: ■ Environmental Implicationsmentioning
confidence: 74%
“…It remains unclear in these low Np microcosm studies whether Np(V) removal is linked to microbial metabolism or the result of abiotic reaction with Mn(II/III) minerals produced during microbial Mn(IV) reduction. The formation of Np-carbonatohydroxo complexes has been shown to increase the solubility of Np(IV) (Kitamura and Kohara, 2002;Kim et al, 2010). However, in these systems under end point sulfate reducing conditions (pE -4), and taking into account the increase in inorganic carbon expected from acetate utilization (2 mM), solution modelling in PHREEQC-2 (SIT database) predicted that Np would be speciated as Np(OH)4 (see supporting information S2).…”
Section: Neptunium Behaviour During Progressive Bioreductionmentioning
confidence: 99%
“…The H 2 O 2 decomposition mechanism is dependent on U oxidation and so can also be investigated using U 3 O 8 for comparison with UO 2 . The concentration of bicarbonate in groundwater is dependent on the location of the deep geological repository, and can range from ∼10 −4 M (Tono, Japan), 24 to ∼10 −3 M (Daejeon, South Korea), 25,26 to ∼10 −2 M (Forsmark, Sweden) 27 and so it is necessary to understand U dissolution and H 2 O 2 decomposition at uranium oxide surfaces over a range of bicarbonate concentrations.…”
Section: Introductionmentioning
confidence: 99%