EGU23-16485, updated on 17 Aug 2024
https://doi.org/10.5194/egusphere-egu23-16485
EGU General Assembly 2023
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Automatized large-scale 3D THM simulations capturing glacial cycle effects on German nuclear waste repositories in salt rock

Florian Zill1,2, Christian Silbermann2, Tobias Meisel1, Friederike Tiedtke2, Dominik Kern2, Anton Carl3, Andreas Jockel3, Thomas Nagel2, Olaf Kolditz1, Heinz Konietzky2, and René Kahnt4
Florian Zill et al.
  • 1Helmholtz-Centre for Environmental Research (UFZ), Leipzig, Germany
  • 2Institute of Geotechnics, TU BA Freiberg, Freiberg, Germany
  • 3ERCOSPLAN Erfurter Consulting und Planungsbüro GmbH, Erfurt, Germany
  • 4G.E.O.S. Ingenieurgesellschaft mbH, Halsbrücke, Germany

To properly assess the present and future conditions of potential nuclear waste repository sites, understanding their evolution in the past is mandatory. Here, glaciation cycles strongly affect the long-term thermo-hydro-mechanical (THM) evolution of the geosystem.

The AREHS project studies the effects of time-dependent boundary conditions on the evolution of large-scale hydrogeological systems. The focus is on numerical long-term modeling taking into account thermal-hydraulic-mechanical couplings. On the basis of generic geological models for different host rock formations, complex 3D-THM-simulations are performed. The long-term evolution during glacial cycles is simulated using the open-source multi-field finite element code OpenGeoSys, as well as multiple pre-and postprocessing tools integrated into an automatized workflow. This workflow facilitates testing/benchmarking and improves reproducibility as well as overall software quality in a sense of modularization. The impact of the glacial THM loading and atmospheric temperature evolution is taken into account using appropriate time-dependent THM boundary conditions. The simulation results are analyzed with respect to potential safety-critical parameters, such as maximum temperature, hydraulic pressure, subsidence, equivalent effective stress and strain. Some general conclusions will be drawn for the host rock salt in Germany.

How to cite: Zill, F., Silbermann, C., Meisel, T., Tiedtke, F., Kern, D., Carl, A., Jockel, A., Nagel, T., Kolditz, O., Konietzky, H., and Kahnt, R.: Automatized large-scale 3D THM simulations capturing glacial cycle effects on German nuclear waste repositories in salt rock, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-16485, https://doi.org/10.5194/egusphere-egu23-16485, 2023.