URANIUM(VI) IN AQUEOUS SOLUTIONS AT 25°C AND A PRESSURE OF 1 BAR: INSIGHT FROM EXPERIMENTS AND CALCULATIONS

dc.contributor.authorRedkin A.F.
dc.contributor.authorWood S.A.
dc.date.accessioned2026-06-04T15:32:06Z
dc.date.issued2007
dc.description.abstractThe behavior of the 0.1 mNaCl + 0.002 mHCl + 1.9 × 10-5 mUO2(NO3)2 solution was studied at pH from 2.7 to 11.0, 25°C, and 1 bar in an argon atmosphere. The curve of variations in U concentration exhibits two minima at pH = 6.6 ± 0.7 and 10.0 ± 0.5. These minima are related to the precipitation of schoepite and clarkeite, respectively. The experimental data were used to refine the stability constants of U(VI) (hydroxo) complexes. For the polymer species of U(VI) with charges from +2 to -1, the method of additivity of thermochemical increments was used, and increments of the linear relation were determined for the calculation of the Gibbs free energies of formation (Δf G298.150) of respective homologue series. The proposed method was applied to calculate the Δf G298.150 of formation of U(VI) (hydroxo)complexes containing from one to five uranium atoms. © Pleiades Publishing, Ltd. 2007.
dc.identifierhttps://elibrary.ru/item.asp?id=13536368
dc.identifier.citationGeochemistry International, 2007, 45, 11, 1111-1123
dc.identifier.doi10.1134/S0016702907110043
dc.identifier.issn0016-7029
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/53187
dc.titleURANIUM(VI) IN AQUEOUS SOLUTIONS AT 25°C AND A PRESSURE OF 1 BAR: INSIGHT FROM EXPERIMENTS AND CALCULATIONS
dc.typeСтатья

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