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

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

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768 A. Discussion <strong>of</strong> selected references<strong>of</strong> magnitude as the NaClO 4 concentration. Therefore, the ionic medium wasnot constant over the series <strong>of</strong> solubility measurements, <strong>and</strong> the concentration <strong>of</strong>Na + varied from 0.15 to 0.43 M (at least as recalculated in the present review-seebelow). The pH measurements reported by the authors (9.61 to 10.5) are, for somesamples, considerably greater than the theoretical values calculated assuming theabove procedure. The authors also may have added a strong base (possibly NaOH)to vary the pH. It is not possible to accurately calculate the amount <strong>of</strong> NaOH thatmight have been added for pH adjustment, as equilibration with air during the pHadjustment would have also added an acidic reactant (carbon dioxide gas). Thus, theconcentrations <strong>of</strong> Na + <strong>and</strong> the ionic strength corrections to the equilibrium constantsfor the carbonate protonation reactions cannot be estimated with good accuracy (<strong>and</strong>the ones used by the authors are then probably in error).The authors reported the absorption spectrum <strong>of</strong> the solution most concentrated inNp(VI) <strong>and</strong> total carbonate. Although <strong>of</strong> poor quality compared with the previouslypublished spectra [81WES/SUL, 86GRE/RIG] cited by the authors, the spectrum (contraryto the contention <strong>of</strong> the authors) still clearly corresponds to the spectrum <strong>of</strong> thepure limiting complex, NpO 2 (CO 3 ) 4−3. The analysis <strong>of</strong> the absorbance measurementsstrongly relies on the values <strong>of</strong> the molar absorbances for the pure species. Such valueswere not proposed by the authors, nor can the values be deduced because there was noevidence for a second absorbing species.The authors plotted their experimental solubility data as a function <strong>of</strong> the logarithm<strong>of</strong> the aqueous concentration <strong>of</strong> CO 2−3, <strong>and</strong> proposed a slope analysis. In the presentreview it is concluded that the range <strong>of</strong> experimental conditions was too small, the<strong>chemical</strong> conditions too poorly defined, <strong>and</strong> the scatter <strong>of</strong> the experimental results toolarge, to obtain any useful result from such an analysis. The authors’ proposed initialcomplex, final complex, <strong>and</strong> the number <strong>of</strong> OH lig<strong>and</strong>s they claim were exchanged arecompletely in error.[93PRA/YAM]See [91YAM/PRA].[93SAW/MAH]The authors carried out potentiometric titrations using a fluoride electrode at (23±1) ◦ C(“room temperature”) <strong>and</strong> I = 1M(NaClO 4 ). This method is well established <strong>and</strong> hasa high precision. This study supersedes the one published earlier by the same group[86MAH/SAW], in which log 10 β 1 (A.69, q = 1, I = 1M) = (3.07 ± 0.04) was reported.This earlier result was called into question by these authors [93SAW/MAH], becausehigher complexes had not been considered in the evaluation in [86MAH/SAW].Pure starting solutions <strong>of</strong> Pu(III) were obtained by adding an excess <strong>of</strong> quinhydroneto a Pu stock solution before each experiment. The remaining quinhydrone servedas a holding reductant for Pu(III). The absorption spectra were recorded before eachexperiment to ensure absence <strong>of</strong> Pu(IV). The liquid junction potential was carefullyevaluated at each titration point as a function <strong>of</strong> the free proton concentration. The data

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