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

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728 A. Discussion <strong>of</strong> selected referencessolutions was estimated to be less than 0.01 mM but there is not much informationin the experimental procedure discussing how this was achieved or how the calculationsto do this estimation were carried out (the redox potential measurements indicatethat solutions were equilibrated with the air, <strong>and</strong> this is not consistent with low CO 2concentrations in the solutions). Experimental solubility values, when plotted againstpH (7 to 12.4), are scattered <strong>and</strong> there is practically no significant pH dependency at8 < pH < 11.5. Most <strong>of</strong> the results are not in agreement with previous solubility measurements[76SEV/KHA, 78MUS, 85LIE/TRE]. The erratic results are likely the result<strong>of</strong> carbonate complexation, <strong>and</strong> gradual ripening or dissolution <strong>of</strong> colloidal material.[88ULL/SCH]The sections <strong>of</strong> this publication dealing with the uranium system were discussed ina previous volume <strong>of</strong> the NEA review [92GRE/FUG]. The paper reports results <strong>of</strong>calorimetric experiments for the heat <strong>of</strong> reaction <strong>of</strong> Np(VI) (0.0289 to 0.0447 M) <strong>and</strong>Pu(VI) (0.010 to 0.016 M), perchlorate salts in aqueous Na 2 SO 4 solutions (0.15 M,for the Np(VI) solutions, 0.07 M, for the Pu(VI) solutions) with aliquots <strong>of</strong> Na 2 CO 3(0.1 to 1 M). The actinides were initially present in solution as AnO 2+2 ,AnO 2SO 4 (aq)<strong>and</strong> AnO 2 (SO 4 ) 2−2. By the end <strong>of</strong> each titration, the limiting carbonato complex,AnO 2 (CO 3 ) 4−3, had formed. The distributions <strong>of</strong> the SO2−4complexes were calculatedfrom equilibrium constants (<strong>and</strong> enthalpies) previously determined using the same apparatus,[86ULL/SCH]. The calculation procedure for the evaluation <strong>of</strong> all equilibriumconstants <strong>and</strong> the enthalpy <strong>of</strong> the non-limiting complex is different from that <strong>of</strong> thisreview. The enthalpy <strong>of</strong> the limiting complexes is essentially model independent. Itwas not possible to re-evaluate this data set with the appropriate assignment <strong>of</strong> activitycoefficients. The errors assigned to the equilibrium constants <strong>and</strong> the enthalpies<strong>of</strong> the intermediate carbonato complexes must be exp<strong>and</strong>ed to reflect the non-st<strong>and</strong>ardprocedure.The authors [88ULL/SCH] concluded that only the limiting carbonate complex,NpO 2 (CO 3 ) 4−3, was formed when there was an excess <strong>of</strong> carbonate. The mean <strong>of</strong>the experimental heat <strong>of</strong> reaction values for the <strong>neptunium</strong> system, for experimentsin which the final CO 2−3 :Np ratio is > 3, is H =−(64.5 ± 2.3) kJ·mol−1 . Thismolar enthalpy <strong>of</strong> reaction value is more negative than the value previously reportedby Schreiner et al. [85SCH/FRI], probably because the initial sulphate concentrationswere not the same. Correction <strong>of</strong> the value for sulphate complexation as done in the originalpaper [88ULL/SCH] by addition <strong>of</strong> 22.5 kJ·mol −1 (with an uncertainty assumedequal to that found for the enthalpy <strong>of</strong> solution reported in this paper (±2.3 kJ·mol −1 ))results in the value r H m = −(42.0 ± 3.2) kJ·mol −1forNpO 2+2+ 3CO 2−3Å NpO 2 (CO 3 ) 4−3This values applies in an ill-defined aqueous medium that was different for differentstages <strong>of</strong> the experiment, ranging in ionic strength from 0.3 to 1.1 M.

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