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

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322 17. Plutonium oxygen <strong>and</strong> hydrogen compounds <strong>and</strong> complexes17.1.3 Plutonium(IV) hydroxide complexesThere have been a number <strong>of</strong> potentiometric [51RAB/LEM, 57RAB], solubility[90PAZ/KUD], extraction [74SOL, 76MET/GUI] <strong>and</strong> spectroscopic[50KRA/NEL, 60RAB/KLI, 96NIT/SIL] studies <strong>of</strong> the first hydrolysis constant <strong>of</strong>Pu(IV). These are discussed in Appendix A. Measured values may be time dependentbecause <strong>of</strong> slow oxidation, disproportionation, radiolysis, or polymerization reactions.Therefore, the hydrolysis constant can be found only from studies in which theelectro<strong>chemical</strong> potential was carefully controlled, or in which the equilibrium total<strong>plutonium</strong>(IV) in solution was measured, or the measurements were carried outrapidly.The values <strong>of</strong> ∗ β 1 for reaction:Pu 4+ + H 2 O(l) Å PuOH 3+ + H + (17.2)reported from the two extraction studies [74SOL, 76MET/GUI], are in relatively goodagreement, but the source <strong>of</strong> Solovkin’s values [74SOL] is not clear (see Appendix A).Metivier <strong>and</strong> Guillaumont’s value [76MET/GUI] differs by an order <strong>of</strong> magnitudefrom the value found potentiometrically in a similar medium [51RAB/LEM]. Conversely,the spectrophotometric results <strong>of</strong> Rabideau <strong>and</strong> Kline [60RAB/KLI] arealmosthalf an order <strong>of</strong> magnitude larger than the value reported from potential measurementsby Rabideau [57RAB]. In this complicated system, spectrophotometric measurementsare probably less prone than extraction or potentiometric measurements tosome <strong>of</strong> the possible systematic errors that can originate from slow disproportionation<strong>of</strong> Pu(IV). There is only one study in chloride solution. Even for perchlorate solutionsthere are insufficient data, <strong>and</strong> the data are too badly scattered, to calculate an interactionε term for the hydrolysis reaction. An estimated value <strong>of</strong> ε (PuOH 3+ ,ClO − 4 ) =0.50 kg·mol −1 was used to calculate ε =−0.18 kg·mol −1 <strong>and</strong> used with the experimentallog ∗ 10 β 1 values from the three spectroscopic studies in perchlorate media[50KRA/NEL, 60RAB/KLI, 96NIT/SIL] (equally weighted) to obtain the selectedlog10 ∗ β◦ 1 (17.2, 298.15 K) =−(0.78 ± 0.60)The uncertainty has been increased to overlap with the values from the potentiometricstudies [51RAB/LEM, 57RAB]. Within the uncertainties, the value is the same asthose selected for corresponding reactions involving uranium [92GRE/FUG] <strong>and</strong> <strong>neptunium</strong>(Section 8.1.4) species. Hence, f G ◦ m (PuOH3+ , aq, 298.15 K) = −(710.7 ± 4.4) kJ·mol −1Two studies [57RAB, 60RAB/KLI] provide information on the temperature dependence<strong>of</strong> the first hydrolysis constant <strong>of</strong> Pu 4+ . The reported values <strong>of</strong> r H m forthe reaction 17.2 are (30.5 ± 2.1) [57RAB] <strong>and</strong> (35.6 ± 3.8) [60RAB/KLI], both determinedin perchlorate media <strong>of</strong> approximately 2 M ionic strength. Both these valueswere obtained from changes in equilibrium constants over quite small temperature differences,<strong>and</strong> the actual hydrolysis constants reported in the two studies are only in

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