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

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

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574 A. Discussion <strong>of</strong> selected referencesFigure A.1: Calculated log 10 K for average data with the adjustment <strong>of</strong> E by the author.The line is log 10 K = 0.39 + 0.145 [NO − 3 ]1.00.80.6log K0.40.20.00.0 0.5 1.0 1.5 2.0[NO 3 ]Since in a spectrophotometric study the properties <strong>of</strong> the complex are measured,its existence is established. Hence the speciation proposed by the author together withthe value calculated for the constant at I = 2 M are accepted in the present review.Properly, in order that the value can be converted to the molal scale <strong>and</strong> used in thest<strong>and</strong>ard SIT procedure (see Appendix B), the constant should be extrapolated so asto apply to trace nitrate concentrations at I =2M(HClO 4 ). For this reason the valueestimated by the author using the assumption that the activity coefficients, <strong>and</strong> alsothe constant K (A.1, I = 2M), do not change while the medium is changed from2MHClO 4 to2MHNO 3 , is accepted. However, for this reason (<strong>and</strong> because thestudy was carried out at 20 ◦ C rather than 25 ◦ C) the estimated uncertainty is increasedto 0.20. If an attempt is made to take account <strong>of</strong> the variation in the ionic mediumat constant ionic strength using the SIT, a linear dependence <strong>of</strong> the constant on theconcentration <strong>of</strong> nitrate is predicted. As can be seen from Figure A.1,thisseemstobethe case, <strong>and</strong> from the intercept <strong>of</strong> the line at zero nitrate, a value <strong>of</strong> log 10 K(A.1, 2MHClO 4 ) = 0.39 ± 0.1 is estimated. The results for the mixtures (9.1 M NH 4 NO 3+ 1 M HNO 3 )<strong>and</strong>(9.1MCa(NO 3 ) 2 + 0.1 M HNO 3 ) are further complicated by theinteraction <strong>of</strong> the negatively charged hexanitrato complex ion with NH + 4 <strong>and</strong> Ca2+ .The results from the measurements at high ionic strength from the work <strong>of</strong> Hindman[49HIN] are unlikely to provide thermodynamic data that can be used for the purposes<strong>of</strong> the present review, <strong>and</strong> are not considered further here.

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