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Numerical modelling of hydraulic decompression due to the excavation of tunnel and drifts at the Tournemire underground laboratory.



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C. Mügler 1, A. Genty and J. Cabrera 2, - Geotechnical and geological engeneering 22 : 525-543, 2004 . 1 CEA, Saclay, 91191 Gif sur Yvette Cedex, France 2 IRSN, BP 17, 92262 Fontenay-aux Roses Cedex, France

Type de document > *Article de revue

Mots clés > faille/fracture, géologie, radionucléides

Unité de recherche > IRSN/DSU/SSD, IRSN/DSU/SSD/BECS

Auteurs > CABRERA Justo

Date de publication > 19/01/2005


The Tournemire underground laboratory is situated in a clay formation and consists of a disaffected railway tunnel and two perpendicular drifts. The paper presents modelling and 3D simulations of the hydraulic behaviour of the argillaceous formation around the works. Experimental measurements of porosity, permeability and specific storage coefficients allowed us to model the hydraulic properties of the shale. Numerical simulations are performed with the code CASTEM. Numerical results of hydraulic heads are compared to experimental measurements. Calculations show that the excavation of the tunnel and drifts has induced an hydraulic decompression of the indurated argillaceous formations. The zones of decompression are centred around the structures and extend depending on the values ofhydraulic parameters such as permeability and specific storage selected in the model. Six years after the excavation of the drifts, the hydraulic steady state in the fractured zone is not yet reached.