Over the assessment period of one million years, a repository for high-level radioactive waste (HAW) will be influenced by a multitude of processes and developments that must be considered when designing the repository. One such development is the climate, whose influences are highly dynamic and complex. To address these challenges, further research is required for global climate modelling using “Earth system Models of Intermediate Complexity” (EMICS) and in far-field modelling of potential repository sites in Germany. In this work far-field groundwater models are set up to estimate climate and parameter uncertainties to characterise and document the effects, and to show how or to what extent these uncertainties can be reduced in accordance with the requirements of EndlSiUntV §11.
The climatic states most relevant to the radionuclide transport in the far-field were identified and modelled using different boundary conditions. Groundwater models were set up and run for temperate climate, glaciation, permafrost, the presence of erosion valleys and sea level rise. A generic geological model from previous projects was used as the basis for modelling a potential repository site in claystone (Reinhold et al. 2013). The flow and transport processes of advection, density-driven flow, dispersion, diffusion, sorption and decay were implemented using the code “distributed density-driven flow (d3f++)” (Schneider et al. 2023, Fein 2004, Fein & Schneider 1999). The pollutant transport from the repository into the surrounding geological layers is modelled and evaluated at observation points. In addition, the mass integrals of the various model units are used to analyse the mass flow out of the host rock according to §4 section 5 of the EndlSiAnfV.
Simulations are carried out for different climate states and parameter variations in order to quantify their influence on the radionuclide distribution in the far-field. The results show a low influence of the climatic states and a significant influence of the diffusion as the primary transport process in the clay rock and the sorption as a strong retarding process. Only for low diffusion coefficients the hydraulic gradient affect the transport velocities. Site selection must be preceded by sufficiently good exploration to determine the rock properties as well as possible in order to be able to provide a robust safety case for the repository in the future.
References
Bundesministerium für Umwelt, Naturschutz, und nukleare Sicherheit (BMUV) (2020): Endlagersicherheitsanforderungsverordnung - EndlSiAnfV. BGBl. I S. 2094.
Bundesministerium für Umwelt, Naturschutz, und nukleare Sicherheit (BMUV) (2020): Endlagersicherheitsuntersuchungsverordnung - EndlSiUntV. BGBl. I S. 2094, 2103.
Fein, Eckard; Schneider, Anke (1999): d3f – Ein Programmpaket zur Modellierung von Dichteströmungen. Abschlussbericht. GRS-139. Braunschweig.
Reinhold, Klaus; Jahn, Steffen; Kühnlenz, Tatjana, Ptock, Lennart, Sönnke, Jürgen (2013): Methodenentwicklung und Anwendung eines Sicherheitsnachweiskonzeptes für einen generischen HAW-Endlagerstandort im Tonstein (AnSichT). Endlagerstandortmodell Nord (AnSichT) - Teil I: Beschreibung des geologischen Endlagerstandortmodells. Zwischenbericht. BGR. Hannover.
Schneider, Anke; Conen, Niklas Paul; Gehrke, Anne; Hilbert, Julian; Knodel, Markus M.; Kröhn, Klaus-Peter et al. (2023): HYMNE - hydrogeological modelling at a regional scale. GRS-750. Braunschweig.