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

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260 12. Neptunium group 14 compounds <strong>and</strong> complexesIn this review the stoichiometry <strong>of</strong> the Np(IV) limiting complex was assumed tobe Np(CO 3 ) 6−5, despite the lack <strong>of</strong> experimental confirmation <strong>of</strong> this stoichiometry. Aquantitative interpretation <strong>of</strong> the (relatively poor) experimental data leads to a rough estimate<strong>of</strong> the stability <strong>of</strong> Np(CO 3 ) 6−5based on the formal potential <strong>of</strong> the Np(V)/Np(IV)redox couple. However, recent, solubility data are used to calculate the value <strong>of</strong> theformation constant selected for Np(CO 3 ) 4−4. Spectrophotometric data for the dissociation<strong>of</strong> the limiting complex are used to calculate the equilibrium constant for thereaction <strong>and</strong> the stability constant for Np(CO 3 ) 6−5. The model assumed here seemsto be sufficient to explain all published data. The species Np(OH) 4 (aq), Np(CO 3 ) 6−5<strong>and</strong> Np(CO 3 ) 4−4are probably formed in concentrated carbonate/bicarbonate media.There are insufficient data to allow selection <strong>of</strong> formation constant values for othercomplexes, but that does not mean they do not exist.12.1.2.1.4.aThe limiting Np(IV) carbonate complexFedoseev, Peretrukhin <strong>and</strong> Krot [79FED/PER] proposed the rough value E ◦′ (12.21, 1MNa 2 CO 3 ) = 0.1 V/SHE for the redox potential <strong>of</strong> the equilibriumNp(V) + e − Å Np(IV) (12.21)A reasonable assessment <strong>of</strong> the uncertainty in this value is probably ± 0.2 V (AppendixA). Delmau, Vitorge <strong>and</strong> Capdevila [96DEL/VIT] later obtained a steady measurementin the same medium <strong>and</strong> determined E ◦′ (12.21, 1MNa 2 CO 3 , pH=10.12) =0.244 V/SHE. The major redox equilibrium can now be interpreted in terms <strong>of</strong> the limitingcarbonate complexes <strong>of</strong> Np(IV) <strong>and</strong> Np(V) whose stoichiometries <strong>and</strong> stabilitiesin these <strong>chemical</strong> conditions are now reasonably well established (see below in thissection <strong>and</strong> Section 12.1.2.1.3.a respectively).NpO 2 (CO 3 ) 5−3+ e − + 2CO 2 (g) Å Np(CO 3 ) 6−5(12.22)The potential <strong>of</strong> the Np(V)/Np(IV) redox couple E(12.21), is corrected for CO 2 (g)partial pressure to obtain the formal potential E ◦′ (12.22). This is the main source <strong>of</strong>uncertainty: when a closed 1 M Na 2 CO 3 solution ( p CO2 = 10 −6.3 atm [95VIT]) iscontacted with air (p CO2 = 10 −3.5 atm), p CO2 can progressively increase, decreasingpH <strong>and</strong> shifting the redox potential <strong>of</strong> the solution by as much as +330 mV. Conversely,water reduction produced OH − anion in the course <strong>of</strong> the electro<strong>chemical</strong> preparation<strong>of</strong> Np(IV) from Np(V). E ◦′ (12.22, 1MNa 2 CO 3 , p CO2 = 1 atm) = 0.514 <strong>and</strong> 0.535V/SHE are calculated by this review from the above values E ◦′ (12.21, 1MNa 2 CO 3 )=0.1V/SHE[79FED/PER] assuming equilibrium with air, <strong>and</strong> from E ◦′ (12.21, 1MNa 2 CO 3 , pH 10.12) = 0.244 V/SHE [96DEL/VIT] respectively. Further discussion isprovided in Appendix A. From the mean <strong>of</strong> the two values, E ◦′ (12.22, 1MNa 2 CO 3 ,p CO2 = 1 atm, 298.15 K) = (0.524 ± 0.101) V/SHE (the uncertainty reflects the inaccuracyin the value <strong>of</strong> p CO2 ), this review calculates log 10 β 5 (12.23,1MNa 2 CO 3 , γ Np 4+= 1, 298.15 K) = (41.96 ± 1.70) in molal units for the equilibriumNp 4+ + 5CO 2−3Å Np(CO 3 ) 6−5(12.23)

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