The REP experiment is part of the research programme conducted by Andra to investigate the possibility of reversible radwaste disposal in a Jurassic (Callovo-Oxfordian) argillite formation at the Meuse/Haute-Marne underground laboratory site in northeastern France. The experiment focuses on the hydromechanical response of the formation to sinking the laboratory access shaft. Modelling of boreholes and shaft sinking operations has helped to optimise measurement point locations based on initial stress tensor anisotropy, while minimising interaction between instrument boreholes. Analyses were made of model sensitivity to intrinsic rock characteristics, hydromechanical coupling properties and sensor installation procedures.

L'experimentation REP fait partie du programme de recherche pluridisciplinaire engage par l'Andra pour etudier la possibilite d'un stockage reversible des dechets radioactifs dans la formation Callovo-Oxfordienne des argilites du site de Meuse/Haute-Marne (Commune de Bure - France). Cette experimentation permettra d'etudier la REponse hydromecanique de la formation aux sollicitations engendrees par le fonçage du Puits d'accès du laboratoire souterrain de recherche. Afin d'optimiser le positionnement des points de mesures, compte tenu de l'anisotropie du tenseur des contraintes initiales, et de minimiser les interactions entre les forages d'instrumentation, des modelisations des forages et du creusement du puits ont ete conduites. Des analyses de sensibilite aux caracteristiques intrinsèques de la roche, aux proprietes de couplage HM et aux protocoles d'installation des capteurs ont ete faites.

Die REP-Untersuchung ist Teil des multidisziplinaren Forschungsprogramms, das die ANDRA im Callovo-Oxfordian-Tonstein in situ am Standort Meuse/Haute Marne (Gemeinde Bure - Frankreich) im Hinblick auf eine Eignung zur reversiblen Lagerung radioaktiver Abfalle durchfuehrt. Dabei soll das hydro-mechanische Verhalten der Formation auf die Beanspruchungen, die durch das Abteufen des Zugangsschachts zum Untertage-Forschungslabor erzeugt werden, untersucht werden. Zur optimalen Positionierung der Messpunkte unter Beruecksichtigung der Anisotropie des Tensors der Ausgangsspannungen und zur Minimierung der gegenseitigen Beeinflussung der Instrumentierbohrungen wurden ein Schachtabteuf- und Bohrmodelle entwickelt. Zur Untersuchung der inharenten Eigenschaften des Gesteins, des gekoppelten HM- Verhaltens und der Installationsprotokolle der Messsonden wurden Sensibilitatsanalysen durchgefuehrt.

Introduction

The REP experiment is part of a multi-disciplinary research programme conducted by Andra to investigate reversible radioactive waste disposal (Lebon and Hoorelbeke, 2002). The host rock is a Jurassic (Callovo-Oxfordian) shale at the Meuse/Haute-Marne (MHM) site in northeastern France. The experiment focuses on the hydromechanical response of the argillite to construction of the access shaft of the underground research laboratory (Su et al, 2000).

This experiment calls for a pause in the shaft sinking operations at a depth of 445 m to construct an experimental niche. This niche will provide a platform for employing instruments to monitor the continued construction of the shaft. The T-shaped geometry of this opening enables investigation of a large volume of rock around the shaft, between elevations - 460 and - 475 m below surface (Figure 1).

The aim of the REP experiment is to continuously monitor the rock mass response during passage of the working face and to compare the hydromechanical properties of the argillite formation before and after shaft sinking. These data will provide experimental bases for:

  • Determining an argillite constitutive mechanical law

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