Excavation-induced fractures network surrounding tunnel: properties and evolution under loading

Author:

De La Vaissière R.1,Morel J.1,Noiret A.1,Côte P.2,Helmlinger B.3,Sohrabi R.4,Lavanchy J.-M.4,Leveau F.5,Nussbaum C.6,Morel J.7

Affiliation:

1. Agence nationale pour la gestion des déchets radioactifs (ANDRA), RD960 55290 Bure, France

2. Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR), Route de Bouaye CS4, 44344 Bouguenais, France

3. Solexperts France, Technopôle Nancy-Brabois 3, rue du Bois de la Champelle, 54500 Vandœuvre-lès-Nancy, France

4. AF Consult, Taefernstrasse 26, 5405 Baden, Switzerland

5. GEOTER, RD960 55290 Bure, France

6. SWISSTOPO, Fabrique de Chaux, CH-2882 St-Ursanne, Switzerland

7. SOLDATA, Parc de l’île, 21 rue du port, 92022 Nanterre, France

Abstract

AbstractThe investigation of the induced fractures network around seals in drifts or shafts, and in particular its evolution, is a key issue for the performance assessment of an underground waste repository. Within this framework, a specific experiment was designed and implemented in the Meuse/Haute-Marne Underground Research Laboratory (URL). This experiment, called CDZ (Compression of the Damaged Zone), is dedicated to studying the effect of mechanical compression within the induced fractures zone of the Callovo-Oxfordian claystone (COx). An unequalled level of knowledge in the 3D structure of the fractures network has been attained. A multidisciplinary approach was applied to observe not only the initial state of the induced fracture zone but also its evolution during a loading cycle. The investigations show that the fracture network which composed the Excavation Damaged Zone (EDZ) was initially interconnected and open for flow and then partially closed progressively following the increasing mechanical stress applied on the drift wall. Moreover, the evolution of the EDZ after unloading indicates a self-sealing process.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference23 articles.

1. Factoring anisotropy into iterative geometric reconstruction algorithms for seismic tomography

2. Andra (2010) Référentiel du site Meuse/Haute-Marne – Tome 2. C.RP.ADS.09.0007.

3. Geometry and properties of the excavation induced fractures at the meuse/haute-marne URL drifts;Armand;International Journal of Rock Mechanics and Mining Sciences,2014

4. Bauer C. Pépin G. Lebon P. (2003) Proceedings of the EC Cluster Conference on Impact of the EDZ on the Performance of Radioactive Waste Geological Disposal (3–5 November 2003, Luxembourg), EDZ in the performance assessment of the Meuse/Haute-Marne site: conceptual model used and questions addressed to the research. European Commission Report EUR21028EN .

5. Bernier F. Li X. L. (2007) Fractures and self-healing within the excavation disturbed zone in clays (SELFRAC). Final Report. European Commission Report, EUR 22585, 62.

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