Hybrid Finite-Discrete Element Simulation of the EDZ Formation and Mechanical Sealing Process Around a Microtunnel in Opalinus Clay

被引:102
作者
Lisjak, Andrea [1 ]
Tatone, Bryan S. A. [1 ]
Mahabadi, Omid K. [1 ]
Grasselli, Giovanni [8 ]
Marschall, Paul [2 ]
Lanyon, George W. [3 ]
de la Vaissiere, Remi [4 ]
Shao, Hua [5 ]
Leung, Helen [6 ]
Nussbaum, Christophe [7 ]
机构
[1] Geomech Inc, Toronto, ON, Canada
[2] Natl Cooperat Disposal Radioact Waste NAGRA, Wettingen, Switzerland
[3] Fracture Syst Ltd, St Ives, Cornwall, England
[4] French Natl Agcy Radioact Waste Management ANDRA, Bure, France
[5] Fed Inst Geosci & Nat Resources BGR, Hannover, Germany
[6] NWMO, Toronto, ON, Canada
[7] Fed Off Topog Swisstopo, Wabern, Switzerland
[8] Univ Toronto, Dept Civil Engn, Toronto, ON, Canada
关键词
Excavation damaged zone (EDZ); EDZ sealing; Opalinus Clay; Numerical modeling; Hybrid finite-discrete element method (FDEM); Mont Terri underground rock laboratory; Underground nuclear waste disposal; Rock fractures; EXCAVATION DAMAGED ZONE; ROCK; FRACTURE; BEHAVIOR; BOREHOLE; FEM/DEM; TUNNEL; MODEL; FLOW;
D O I
10.1007/s00603-015-0847-2
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The analysis and prediction of the rock mass disturbance around underground excavations are critical components of the performance and safety assessment of deep geological repositories for nuclear waste. In the short term, an excavation damaged zone (EDZ) tends to develop due to the redistribution of stresses around the underground openings. The EDZ is associated with an increase in hydraulic conductivity of several orders of magnitude. In argillaceous rocks, sealing mechanisms ultimately lead to a partial reduction in the effective hydraulic conductivity of the EDZ with time. The goal of this study is to strengthen the understanding of the phenomena involved in the EDZ formation and sealing in Opalinus Clay, an indurated claystone currently being assessed as a host rock for a geological repository in Switzerland. To achieve this goal, hybrid finite-discrete element method (FDEM) simulations are performed. With its explicit consideration of fracturing processes, FDEM modeling is applied to the HG-A experiment, an in situ test carried out at the Mont Terri underground rock laboratory to investigate the hydro-mechanical response of a backfilled and sealed microtunnel. A quantitative simulation of the EDZ formation process around the microtunnel is first carried out, and the numerical results are compared with field observations. Then, the re-compression of the EDZ under the effect of a purely mechanical loading, capturing the increase of swelling pressure from the backfill onto the rock, is considered. The simulation results highlight distinctive rock failure kinematics due to the bedded structure of the rock mass. Also, fracture termination is simulated at the intersection with a pre-existing discontinuity, representing a fault plane oblique to the bedding orientation. Simulation of the EDZ re-compression indicates an overall reduction of the total fracture area as a function of the applied pressure, with locations of ineffective sealing associated with self-propping of fractures. These results are consistent with hydraulic testing data revealing a negative correlation between pressure values and an increase in the EDZ transmissivity.
引用
收藏
页码:1849 / 1873
页数:25
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