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chemical thermodynamics of neptunium and plutonium - U.S. ...

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324 17. Plutonium oxygen <strong>and</strong> hydrogen compounds <strong>and</strong> complexesvalue, <strong>and</strong> the remaining spread <strong>of</strong> almost three orders <strong>of</strong> magnitude is possibly withinthe experimental uncertainties.The Gibbs energies <strong>of</strong> reaction <strong>of</strong> M 4+ ions (M = U, Np, Pu) with water to formthe corresponding MO 2 crystalline oxides (26.1, 55.7 <strong>and</strong> 45.8 kJ·mol −1 , respectively),show a large variation that is much greater than the accepted uncertainties. This variationis reflected in the values <strong>of</strong> log 10 K for the reactionMO 2 (cr) + 2H 2 O(l) Å M(OH) 4 (aq)Values for M = U, Np <strong>and</strong> Pu are −9.4 [92GRE/FUG] (or−13.4 estimated from[90RAI/FEL]), −19.6 (cf. Table 3.1) <strong>and</strong>−14.9 respectively. It would be expectedthat this same variation <strong>of</strong> 5-10 orders <strong>of</strong> magnitude should be reflected in actinide(IV)“solubilities” measured in near-neutral, reducing solutions over “amorphous” or “hydrated”MO 2 (cf. Sections 8.2.5.2 <strong>and</strong> 17.6). The observed restricted range <strong>of</strong> solubilityvalues (or similar “solubility limits”, e.g.,[85RAI/RYA], [90RAI/FEL] <strong>and</strong> also the recentlypublished [99RAI/HES2]) is most likely due to inadequate detection limits, butis also possibly due to the differences in important experimental variables, one <strong>of</strong> whichcould be the nature <strong>of</strong> the solid phases.

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