ABSTRACT

As part of an ongoing study on the mechanical characteristics of the damaged rock zone (DRZ) around a tunnel boundary and its influence on the overall behaviour of the near-field host rock, a numerical study was conducted to investigate the dominant rock mass failure mechanisms around shallow tunnels located in a body of brittle rock mass. Preliminary studies have clearly indicated that, the rock mass behaviour was largely dictated by the different yield mechanisms involved. These mechanisms appear to be multifarious due to the complex state of the induced stresses around the tunnel boundary at shallow depth. Some of these yield mechanisms are often difficult to capture using the traditional yield criterion such as the Mohr- Coulomb. In the study reported in this paper a series of computer simulations were performed using typical in-situ stresses and rock mass conditions generally encountered in shallow tunnelling projects in Sweden. The presence of a disturbed/damaged rock zone with finite thickness was also added into the models. Due to the nature of the simulations the FLAC2D code was selected and used. The values for the input parameters were estimated using a systematic procedure. To prevent premature tensile yielding due to transient loading traction was applied during tunnel excavation. The results show that, the dominant yield mechanism occurring around the shallow tunnel in brittle rock is the one of tensile nature. Compressive mechanisms do occur but seems to be less critical to overall performance of the tunnel. However, they do influence the overall behaviour of the rock mass response. The results further indicated that, the ‘true’ locality of instability could be predicted from elastic analyses, by observing if all the major principle stresses are in tension in that locality. The shear strain increment plots of the model in plastic mode further supported this observation.

1 INTRODUCTION

Rock mass failure can occur either as gravity driven fallouts or stress driven failures. The former is usually associated with shallow and surface excavations, while the latter with deep excavations. However, experience has shown that both can occur irrespective of depth, dependent on the state of stress and rock mass characteristics (Diederichs, 1999). With the Swedish rock mass conditions and the state of stresses both of these failure types are evident even at very shallow depths (0–20 m). In this paper, as part of an ongoing study on the mechanical characteristics of the damaged rock zone (DRZ) around a tunnel boundary and its influence on the overall behaviour of the near-field host rock, the stress driven failures are investigated for shallow depth excavations. Typical in-situ stresses and rock mass conditions generally encountered in shallow tunnelling projects in Sweden are used. The rock mass is generally of good quality with brittle rock resemblance. Earlier studies of the same scenario by Saiang & Nordlund (2006) and Töyra (2006) have clearly indicated that, the rock mass behaviour was largely dictated by the different yield mechanisms involved.

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