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Fracture effect on the hydro-mechanical behaviour of Callovo-Oxfordian claystone
Abstract Excavation of the galleries for the geological disposal of radioactive waste can induce an excavation damaged zone (EDZ), which can have consequences on the long-term safety of the repository. In this study, intact Callovo-Oxfordian (COx) claystone taken from the Meuse/Haute-Marne Underground Research Laboratory in France was artificially fractured in different directions, and the hydro-mechanical behaviour was investigated by performing high pressure oedometer test and hydraulic conductivity test. Comparison between the fractured and intact COx samples allows identification of the effects of fracture in terms of swelling, compression, hydraulic conductivity and creep. It appears that the presence of fracture decreases the swelling strain and this phenomenon depends on the infiltration path and the orientation of fracture. In particular, the infiltration path affects the global swelling rate of fractured claystone. The self-sealing of fracture is mainly attributed to the swelling of COx claystone grains in the fracture zone. Lower compression coefficient a, higher compression index C c* and higher secondary consolidation coefficient C α are observed for the fractured claystone, indicating a higher compressibility and creep than the intact one. The compression and creep behaviours depend on both the orientation of fracture and the stress level. Comparison of hydraulic conductivities between fractured and intact claystone indicates that the hydraulic conductivity can be partially recovered due to the collapse of macro-pores in the filled fracture zone. This is also confirmed by analysing the evolution of consolidation coefficients c v with stress. Beyond a stress level about 16 MPa, the fracture effect can be neglected, but the compressibility increases further due to grain breakage. Interestingly, this stress is close to the in-situ stress before excavation.
Highlights The presence of fracture decreases the swelling strain and this phenomenon depends on the infiltration path and the orientation of fracture. The self-sealing of fracture is mainly attributed to the swelling of COx claystone grains in the fracture zone. The compression and creep behaviours depend on both the orientation of fracture and the stress level. k of fractured claystone can be partially recovered under high stress due to the collapse of macro-pores in the filled fracture zone.
Fracture effect on the hydro-mechanical behaviour of Callovo-Oxfordian claystone
Abstract Excavation of the galleries for the geological disposal of radioactive waste can induce an excavation damaged zone (EDZ), which can have consequences on the long-term safety of the repository. In this study, intact Callovo-Oxfordian (COx) claystone taken from the Meuse/Haute-Marne Underground Research Laboratory in France was artificially fractured in different directions, and the hydro-mechanical behaviour was investigated by performing high pressure oedometer test and hydraulic conductivity test. Comparison between the fractured and intact COx samples allows identification of the effects of fracture in terms of swelling, compression, hydraulic conductivity and creep. It appears that the presence of fracture decreases the swelling strain and this phenomenon depends on the infiltration path and the orientation of fracture. In particular, the infiltration path affects the global swelling rate of fractured claystone. The self-sealing of fracture is mainly attributed to the swelling of COx claystone grains in the fracture zone. Lower compression coefficient a, higher compression index C c* and higher secondary consolidation coefficient C α are observed for the fractured claystone, indicating a higher compressibility and creep than the intact one. The compression and creep behaviours depend on both the orientation of fracture and the stress level. Comparison of hydraulic conductivities between fractured and intact claystone indicates that the hydraulic conductivity can be partially recovered due to the collapse of macro-pores in the filled fracture zone. This is also confirmed by analysing the evolution of consolidation coefficients c v with stress. Beyond a stress level about 16 MPa, the fracture effect can be neglected, but the compressibility increases further due to grain breakage. Interestingly, this stress is close to the in-situ stress before excavation.
Highlights The presence of fracture decreases the swelling strain and this phenomenon depends on the infiltration path and the orientation of fracture. The self-sealing of fracture is mainly attributed to the swelling of COx claystone grains in the fracture zone. The compression and creep behaviours depend on both the orientation of fracture and the stress level. k of fractured claystone can be partially recovered under high stress due to the collapse of macro-pores in the filled fracture zone.
Fracture effect on the hydro-mechanical behaviour of Callovo-Oxfordian claystone
Wang, Hao (author) / Cui, Yu-Jun (author) / Vu, Minh Ngoc (author) / Talandier, Jean (author) / Conil, Nathalie (author)
Engineering Geology ; 303
2022-04-12
Article (Journal)
Electronic Resource
English
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