Géotechnique des ouvrages souterrains comportements
Transcription
Géotechnique des ouvrages souterrains comportements
Géotechnique Géotechnique des des ouvrages ouvrages souterrains souterrains comportements comportements post post rupture rupture Thierry YOU, CFMR/AFTES 2006 Géotechnique des ouvrages souterrains comportements post rupture Laboratoire Retours d’expérience Conclusions CFMR/AFTES 2006 Augmentation contrainte axiale D’après Lockner et al. Observations of quasi-Static fault growth from acoustic emissions, in Fault Mechanics and Transport Properties of Rocks, B. Evans and T.-F. Wong ed., 1992 ESSAI TRIAXIAL LABO SUR ECHANTILLON MARNE Vitesse de déformation = 2.10-6 s-1 Pression de confinement = 4 MPa 50 45 Contrainte Axiale MPa 40 35 E = 10.1 GPa 30 25 E = 9.3 GPa 20 E = 4.9 GPa 15 10 E = 7.7 GPa 5 0 0 0.005 0.01 0.015 Déformation Axiale 0.02 0.025 SYDNEY ROCK FALL EXPLANATIONS (20+) • A large number of explanations were put forward by the parties involved, many of them with ulterior motives: unsuitable section, inappropriate and damaging explosive, poor workmanship (drilling, bolting, etc.), untested rock bolts, too differed bolt grouting, poor site organisation, unsuitable numerical and structural models, underdesigned rockbolts, inappropriate bolting patterns, unsuitable excavation sequence, poor and inefficient quality control, lack of design methodology (EC7), lack of monitoring and inspection, unforeseen stress release, random vertical joints, lack of spot bolt decision on visible instabilities, inclined defects in sheet facies, too high water pressure imposed in the fissures, etc. • At that stage, none of the specified monitoring measures that had been prepared for design validation (geological joint mapping, convergence measurement, profile mapping, pull-out test, etc.), that certainly would have helped as new design basic data, had been implemented. • Maintaining roof integrity was crucial for stability, as was established latter (You et al. Johannesburg ISRM2003) SYDNEY - UDEC DESIGN METHODOLOGY FOR HYDROCARBON CAVERNS INFLUENCE OF IN-SITU STRESSES ON LARGE SECTIONS Top heading and bench 1 INFLUENCE OF IN-SITU STRESSES ON LARGE SECTIONS VISAKHAPATNAM BED egg-shape cross-section Revised basket-handle cross-section ARMS,4 - 2006 Singapore UNDERGROUND STORAGE IN MINED CAVERN PRINCIPLES Stability Operation Hydrodynamic Containment Neither a Mine, neither a Civil Construction, neither a Laboratory ARMS,4 - 2006 Singapore INFLUENCE OF IN-SITU STRESSES ON LARGE SECTIONS Basic parameters and model geometry used for the numerical analysis m id -p illa r g ro u n d le ve l (y = 0 m ) d o m ain fo r fin e r m e s h in g h o rizo n ta l fra c tu re c a ve r n ARMS,4 - 2006 Singapore Joint aperture for the rounded shape after product filling ARMS,4 - 2006 Singapore 32 33 34 35 36 37 Géotechnique des ouvrages souterrains comportements post rupture PREMIÈRES CONCLUSIONS Le concept est encore un objet de recherche La définition des modes de rupture n’est pas toujours aisée Le phénomène peut aussi être relatif. CFMR/AFTES 2006