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

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

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702 A. Discussion <strong>of</strong> selected referencestotal Np(VI) concentration was used for all the measurements, <strong>and</strong> too narrow adomain <strong>of</strong> CO 2 (g) partial pressure was used).• Calculations using different models did not result in clear differences in the overallleast-square sum, ∑ . Therefore, it is not clear (considering only the statisticalresults) whether other species exist or not.Second, as observed by the author, the overall formation constants deduced fromthese potentiometric titrations do not agree with those deduced from the equilibriumpotential measurement data. The values for only one <strong>of</strong> the pairs <strong>of</strong> stepwise constants,β i /β 3 , are consistent.Third, there are several problems in the selection <strong>of</strong> species or <strong>chemical</strong> problemsthat could cause small systematic errors.• According to Maya, the final product <strong>of</strong> the titrations was NpO 2+2. The assumptionwas then made that NpO 2 (CO 3 ) 2−2(aq) is a major intermediate product,but, surprisingly, not NpO 2 CO 3 (aq) which is the intermediate species betweenNpO 2 (CO 3 ) 2−2<strong>and</strong> NpO 2+2. Reanalyses <strong>of</strong> the equilibrium potential measurementdata, <strong>and</strong> consideration <strong>of</strong> behaviour in the analogous uranium system indicatethat NpO 2 CO 3 (aq) is probably stable over a broader range <strong>of</strong> conditionsthan NpO 2 (CO 3 ) 2−2 .• Maya concluded (NpO 2 ) 3 (CO 3 ) 6−6was not important because slightly poorerfits to his data were obtained using models that included this species. However,based on later work, the stability <strong>of</strong> the species (NpO 2 ) 3 (CO 3 ) 6−6is now well established[86GRE/RIG, 90RIG]. The absorption spectrum <strong>of</strong> (NpO 2 ) 3 (CO 3 ) 6−6has been clearly detected [86GRE/RIG, 90RIG] in solutions similar to those usedfor Maya’s measurements [84MAY].• It has also been observed [86GRE/RIG, 90RIG] that, in contrast to the behaviour<strong>of</strong> the analogous solid in the U(VI) <strong>and</strong> Pu(VI) systems, precipitation <strong>of</strong>NpO 2 CO 3 (s) is quite slow. Recent solubility measurements [98VIT/CAP], suggestthat some <strong>of</strong> Maya’s solutions were probably supersaturated with respect toNp(VI). This might have introduced systematic deviations in the titration data;<strong>and</strong> there are no indications that the solutions were checked for possible precipitationor colloid formation [90RIG].Any attempted reanalysis <strong>of</strong> the data is open to question because not all the datawere provided in the original publication <strong>and</strong> because there are some inconsistencies<strong>and</strong> obvious typographical errors in the author’s Table 1 (a list <strong>of</strong> the values used inthe present review are presented in [98VIT/CAP]). Although the author used differentcarbon dioxide gas partial pressures, <strong>and</strong> varied the ratio <strong>of</strong> hydroxide to carbonate lig<strong>and</strong>,further experiments with higher carbon dioxide gas partial pressures <strong>and</strong> differenttotal Np(VI) concentrations would be required to generate data to unequivocally determinethe stoichiometries <strong>of</strong> the important species, <strong>and</strong> to obtain accurate values fortheir formation constants. This is particularly the case for any polymeric mixed-lig<strong>and</strong>species.

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