MR002-0012
Thermal Pressurization Process in Nuclear Waste Disposal in Argillaceous Claystone
Abstract:
A thermoporoelastical model for argillaceous claystone is applied in this work. The model is validated against two in-situ heating experiments both at Bure, and is utilized to investigate the COx response at the repository scale, focusing on the THM behavior of the COx under thermal loads, such as pore pressure build-up due to thermal expansion of the fluid and solid skeleton, stress evolution around a repository, fluid flow in the rock matrix, and the potential for such changes to induce hydro-fracturing. To reach this goal, several scenarios and model configurations are conducted. The model simulations show that: 1) the highest potential for hydro-fracturing occurs in the middle between parallel emplacement micro-tunnels (cells) at the center of repository rather than at the edge of the repository; 2) a geometric simplification with a 2D model is reasonably accurate for modeling coupled THM processes at the center of the repository, though it would tend to overestimate the likelihood for hydro-fracturing and would substantially overestimate ground surface uplift; 3) the study confirms the importance of the center (or average) repository host-rock temperature evolution that can be the limiting temperature in the thermal management and repository design.