Anisotropic hydro-viscoplastic modelling of a drift at the Meuse/Haute-Marne URL

被引:6
作者
Coarita-Tintaya, Ever-Dennys [1 ,2 ]
Golfier, Fabrice [2 ]
Souley, Mountaka [1 ]
Vu, Minh-Ngoc [3 ]
机构
[1] French Natl Inst Ind Environm & Risks Ineris, Nancy, France
[2] Univ Lorraine UL, CNRS, GeoRessources Lab, Nancy, France
[3] French Natl Radioact Waste Management Agcy Andra, R&D, Chatenay Malabry, France
关键词
Hydromechanical coupling; tunnel; anisotropy; Callovo-Oxfordian claystone; Comsol Multiphysics; CALLOVO-OXFORDIAN CLAYSTONE; STRAIN LOCALIZATION; DAMAGE BEHAVIOR; EXCAVATION; ARGILLITE;
D O I
10.1080/19648189.2020.1797887
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The Meuse/Haute-Marne underground research laboratory was built in the Callovo-Oxfordian (COx) clay formation for the purpose of assessing the feasibility and safety of a deep geological formation to host an industrial radioactive waste repository (Cigeo project) in France. Some observations related to the drifts oriented in the direction of the major horizontal stress remain to be theoretically and numerically understood. In order to contribute to the understanding of the hydromechanical behaviour of the COx claystone, an elasto-viscoplastic model with transient creep was developed, including the inherent elastic and hydraulic anisotropies. Comparison within situmeasurements was made, with encouraging results.
引用
收藏
页码:2731 / 2745
页数:15
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