Solubility of U(VI) in chloride solutions. I. The stable oxides/hydroxides in NaCl systems, solubility products, hydrolysis constants and SIT coefficients. (November 2017)

• Record Type: Journal Article
• Authors: Altmaier, Marcus; Yalçıntaş, Ezgi; Gaona, Xavier; Neck, Volker; Müller, Regina; Schlieker, Martina; Fanghänel, Thomas
• Is Part Of: Journal of chemical thermodynamics. Volume 114(2017)
• Page Start: 2
• Page End: 13
• Publication Date: 2017-11
• Subjects: Uranium(VI) -- Saline solutions -- Solubility -- Hydrolysis -- Metaschoepite -- Sodium uranate; Thermodynamics -- Periodicals; Thermochemistry -- Periodicals; Thermodynamique -- Périodiques; Thermochimie -- Périodiques; Thermochemistry; Thermodynamics; Periodicals; 541.369
• DOI: 10.1016/j.jct.2017.05.039
• Languages: English
• ISSNs: 0021-9614

Abstract

Highlights: New uranium(VI) solubility studies in dilute to concentrated NaCl solution. Systematic evaluation of U(VI) hydrolysis species and solubility limits. Comprehensive thermodynamic model (SIT) derived. Robust geochemical modelling of U(VI) source term concentrations. Abstract: The solubility of uranium(VI) is studied at T = (22 ± 2) °C in carbonate-free 0.03–5.61 mol·kgw −1 NaCl solutions at pHm = 4–14.5 (pHm = −log [H + ]). The solid phases metaschoepite UO3 ·2H2 O(cr) and sodium uranate Na2 U2 O7 ·H2 O(cr) (or NaUO2 O(OH)(cr)) are characterized by XRD, SEM–EDS, thermogravimetry and quantitative chemical analysis. UO3 ·2H2 O(cr) controls the solubility of U(VI) in acidic to near neutral pH conditions regardless of NaCl concentration. Na2 U2 O7 ·H2 O(cr) forms in alkaline systems and is stable at pHm ≥ 7 over the complete range of NaCl concentrations investigated. The solubility of UO3 ·2H2 O(cr) at pHm < 7 in NaCl solutions is very well described with the hydrolysis constants recommended by the NEA–TDB, a set of SIT coefficients evaluated in the present study and a solubility product of log * K °s, 0 {UO3 ·2H2 O(cr)} = (5.35 ± 0.13). Titration experiments and UV–vis absorption spectra of saturated solutions at pHm = 4–5 in dilute to concentrated NaCl solutions confirm the speciation calculated in the present study and show the predominance of the trinuclear hydroxide complex (UO2 )3 (OH)4 2+ at high chloride concentrations. Solubility data obtained at 7 ≤ pHm ≤ 14.5 with Na2 U2 O7 ·H2 O(cr) and in solutions equilibrated simultaneously with Na2 U2 O7 ·H2 O(cr) and UO3 ·2H2 O(cr) yield a solubility product of log * K °s, 0 {0.5 Na2 U2 O7 ·H2 O(cr)} = (12.2 ± 0.2) and the formation constants of the anionic hydrolysis species UO2 (OH)3 − (log * β °(1, 3) = −(20.7 ± 0.4)) and UO2 (OH)4 2− (log * β °(1, 4) = −(31.9 ± 0.2)). SIT coefficients for these species are derived based on the solubility data obtained in dilute to concentrated NaCl systems. The chemical, thermodynamic and SIT activity models provided in this work for the system U VI –Na + –H + –Cl − –OH − –H2 O(l) represent an accurate and robust tool for the calculation of U(VI) solubility and aqueous speciation in a variety of geochemical conditions relevant in the context of nuclear waste disposal.