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

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224 12. Neptunium group 14 compounds <strong>and</strong> complexes12.1.2.1.3.a Np(V) carbonate complexesThree types <strong>of</strong> experimental measurements, liquid-liquid extraction, spectrophotometry<strong>and</strong> solubility, have been used to derive formation constants fordioxo<strong>neptunium</strong>(V) carbonate complexes.Using a liquid-liquid extraction technique with 0.1 or 0.2 M NaClO 4 aqueous solutions,the equilibrium constants, K 1 = β 1 ,for<strong>and</strong> K 2 = β 2 /β 1 ,forNpO + 2 + CO2− 3Å NpO 2 CO − 3(12.14)NpO 2 CO − 3 + CO2− 3Å NpO 2 (CO 3 ) 3−2(12.15)were measured by Bidoglio, Tanet <strong>and</strong> Chatt [85BID/TAN]. Their β 1 value does notcorrespond to the experimental data shown in figures <strong>of</strong> the publication, but even followingre-evaluation in the present review (see Appendix A), none <strong>of</strong> these β 1 values,nor the K 2 value are in accord with other published work <strong>and</strong> with the thermodynamicdata selected here. Inoue <strong>and</strong> Tochiyama [85INO/TOC] also used a liquid-liquid extractiontechnique to determine the values <strong>of</strong> β 1 <strong>and</strong> β 2 in1MNaClO 4 . Within thesmall uncertainties assigned by the authors, the values are not in good agreement withthose selected in the present review. Although larger uncertainties could be assumed(see Appendix A), this work was not used in the final selection <strong>of</strong> thermodynamicvalues in the present review.Values for β 1 , K 2 <strong>and</strong> the stepwise complexation constant, K 3 = β 3 /β 2 ,forNpO 2 (CO 3 ) 3−2+ CO 2−3Å NpO 2 (CO 3 ) 5−3(12.16)can be deduced from absorption spectrophotometric studies (see the discussion <strong>of</strong>[90RIG] in Appendix A); but, <strong>of</strong> these, the most difficult constant to determine isK 2 because the NpO 2 (CO 3 ) 3−2complex cannot be obtained alone to measure its molarabsorptivity (cf. Figure 12.5). This difficulty is even more important at high ionicstrengths. This in turn introduces difficulties when treating the experimental data toobtain β 1 <strong>and</strong> K 3 values. Too low a solubility can also cause problems in the determination<strong>of</strong> values for β 1 <strong>and</strong> K 2 .Riglet’s β 1 values [90RIG] in 0, 0.5, 1 <strong>and</strong> 2 M NaClO 4 are lower than (but stillwithin the stated uncertainties <strong>of</strong>) the values selected below in the present review, <strong>and</strong>the corresponding value <strong>of</strong> ε 1 is in fair agreement with the one selected here (seeTable 12.5). In the present review only the β 1 value in 0.5 M NaClO 4 could be redeterminedfrom the experimental information available in the thesis (see Appendix A) <strong>and</strong>was used in the present review to calculate the selected β1 ◦ value. The extrapolation(using the SIT) to zero ionic strength using Riglet’s spectrophotometric data, gave avalue <strong>of</strong> log 10 K2 ◦ <strong>and</strong> a corresponding ε 2 value in reasonable agreement with thoseselected below, but none <strong>of</strong> Riglet’s K 2 values have been used because the experimentalinformation available is insufficient to allow K 2 to be recalculated.The spectrophotometric data used in determining K 3 were limited to those solutionsin which the extent <strong>of</strong> dissociation <strong>of</strong> the limiting complex was not greater than 25%.

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