Safety concepts regarding nuclear waste disposal in underground repositories generally rely on a combination of engineered and geological barriers that minimize potential radionuclide release out of the containment-providing rock zone and transport through the biosphere. The presence of water (e.g., groundwater and pore water of repository rocks), however, may alter the engineered barrier system, dissolve radionuclides, and facilitate radionuclide transport that over millennia may allow small fractions of water-soluble radionuclides to permeate to the biosphere. So while barrier systems aim to prevent or hinder water from contacting the waste, the possible intrusion of aqueous solutions must be considered for several safety case scenarios impacted by the long-term evolution of a repository. Dissolution, precipitation and solubility phenomena thus arise as important processes controlling the chemical behaviour of radionuclides and other key materials of relevance in the context of such repositories and their safety assessments. The solubility and aqueous speciation of radionuclides is of particular interest as they provide upper limits for water-transportable concentrations of radionuclides.For many radionuclides, solubility limits are only reached after release from the disposed waste products close to the disposal locations, where expected maximal concentrations are highest. It is then often the solubility of a secondary phase, precipitated after dissolution of a primary phase in the waste matrix, that controls the maximum transportable radionuclide concentration close to the disposal location.Solubility phenomena of radioactive and other gases in water provide important constraints on gas transport and pressure build-up. Moreover, due to its thermodynamic foundation, solubility assessments offer insight into time-independent constraints (e.g., maximum concentrations of radionuclides or gases in a fluid phase) on the evolution of the disposal system. Particularly important in this regard is the geochemical modelling of radionuclide behaviour in the engineered barrier system as well as in natural aquatic systems along the transport path of radionuclides to the biosphere. Despite its simplicity, the concept of solubility is difficult to apply in natural water systems, as various water constituents will influence solubility which may vary over the very long times considered in safety assessments of disposal. For instance, the interaction of natural waters with the components of the engineered barrier system surrounding the disposed waste products will influence solution pH, redox potentials or ligand concentrations. Information obtained from studies evaluating radionuclide behaviour provide valuable inputs that appropriately constrain safety analyses of nuclear waste disposal.In this series of articles, solubility phenomena related to different domains and key components in the context of nuclear waste disposal are presented. Several of these contributions provide insight on the chemical, thermodynamic and (SIT, Pitzer) activity models describing the investigated systems. This emphasizes the usefulness of solubility studies for the determination of thermodynamic properties, which can be implemented in thermodynamic databases (e.g., NEA-TDB, THEREDA, ThermoChimie, JAEA-TDB or PSI-Nagra, among others) and further in geochemical calculations of relevance for nuclear waste disposal.
Editorial21 November 2023
Editorial: Solubility phenomena in the context of nuclear waste disposalORIGINAL RESEARCH
14 April 2023
F. Bok, 1 more and V. Brendler
3 Authors
- FB
F. Bok
Actinide Thermodynamics Department, Germany
- HC
H. C. Moog
Department Repository Research, Germany
- VB
V. Brendler
Actinide Thermodynamics Department, Germany
Oxygen is one of the key reaction partners for many redox reactions also in the context of nuclear waste disposal. Its solubility influences radionuclides’ behavior, corrosion processes and even microbial activity. Therefore, a reliable calculation of the solubility of molecular oxygen in aqueous solutions is relevant for any safety assessment.
Available geochemical speciation and reactive transport programs handle these data very differently. In some codes the hypothetical equilibrium between dissolved oxygen and water is used to balance redox reactions. Equilibrium constants are given in “temperature grids” for up to 573.15 K. In other cases, temperature functions for the solubility of gaseous oxygen in water are given, without any reference to a valid temperature range. These settings become even more complicated when used in the context of modeling equilibria in high-saline solutions applying the Pitzer formalism. This raised the question about the experimental foundation of equilibrium constants given in such data files and their validity for the solubility of molecular oxygen in saline solutions.
For this article, a thorough literature review was conducted with respect to the solubility of molecular oxygen in pure water and saline solutions. From these primary experimental O2 solubility data a temperature-dependent Henry’s law function as well as temperature-dependent binary and ternary Pitzer ion-interaction coefficients were derived. An internally consistent set of thermodynamic data for dissolved oxygen is presented, along with statements about its validity in terms of temperature and, as far as Pitzer interaction coefficients are concerned, of solution composition. This self-consistent activity-fugacity model containing thermodynamic data, Henry's law temperature equation, and Pitzer interaction coefficients is capable of providing a more accurate description of redox transformations, allowing a reduction of conservatism in safety assessment calculations, not only in the context of a nuclear repository. The model reproduces well the reliable experimental data available, and is capable to predict the oxygen solubility in complex solution media. The temperature functions used to describe Henry's constant and the Pitzer interaction coefficients are consistent with the implementation in commonly used geochemical computational programs, allowing direct use without further modification.
ORIGINAL RESEARCH
4 April 2023
Hye-Ryun Cho, 4 more and Wooyong Um
6 Authors
- HC
Hye-Ryun Cho
Nuclear Chemistry Research Team, Republic of Korea
- SC
Sangki Cho
Nuclear Chemistry Research Team, Republic of Korea
- JK
Jueun Kim
Division of Advanced Nuclear Engineering, Republic of Korea
- SH
Sangsoo Han
Division of Advanced Nuclear Engineering, Republic of Korea
- HK
Hee-Kyung Kim
Nuclear Chemistry Research Team, Republic of Korea
- WU
Wooyong Um
Division of Advanced Nuclear Engineering, Republic of Korea
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