ThermoQuakes 3D thermo-mechanical modelling of seismicity related to the final disposal of spent nuclear fuel and radioactive waste in hard rock (SSM, 2015-2017)
Time frame: 2015 - 2017
Funding: Swedish Radiation Authority (Strål Säkerhets Myndigheten - SSM)
Principal InvestigatorsA. Zang, GFZ, Section 2.6, Germany
Personnel: Jeoung Seok Yoon, GFZ Section 2.6, Germany
The Swedish Radiation Authority (SSM - Strålsäkerhetsmyndigheten) is the Swedish regulator for the process to build a deep geological repository for high-level radioactive waste. For the selected site Forsmark we model the impact of thermal and earthquake loads on the naturally fractured crystalline rock mass surrounding the repository and their association with complex geologic structures. Besides the thermo-mechanical processes the model can also simulate the induced seismic events (TM-D model) from dynamic rupturing as well as those arising from dissipation of the energy in form of seismic waves.
To be able to assess the safety of a repository for radioactive waste and spent nuclear fuel, it is necessary to consider all possible threats that could impair the physical integrity of the barriers. One environmental threat is an earthquake occurring at nearby faults, and the effect of an earthquake relevant to the repository safety is the shear displacement of rock fractures induced by an earthquake event occurring at nearby large faults (Fig.1).
In this project, we use 3D discrete element based thermo-mechanical coupled dynamic modelling to investigate the safety of the repository at Forsmark Sweden for final disposal of spent nuclear fuels. Especially, we investigate the impacts of larger magnitude (M>6) earthquakes that could occur in the next few hundred years near the Forsmark site. Followings are the objectives of the project.
Fig.2. Temporal change of the slip (in meter) distribution of a dynamically rupturing fault. The co-seismic slip concentrates at one point on the fault plane and propagates outward, which results in asymmetric and heterogeneous slip profiles. Black dots are the deposition holes. (Click for animation)
Fig.3. Rupture area vs. moment magnitude relation of earthquake faults. The results of simulated earthquake faulting (black stars) are compared with the global tectonic earthquake fault data (dots).