For the compressive stress-induced failure of tunnels at depth,rock fracturing process is often closely associated with the generation of surface parallel fractures in the initial stage,and shear failure is likely to occur in the final process during the formation of shear bands,breakouts or V-shaped notches close to the excavation boundaries.However,the perfectly elastoplastic,strain-softening and elasto-brittle-plastic models cannot reasonably describe the brittle failure of hard rock tunnels under high in-situ stress conditions.These approaches often underestimate the depth of failure and overestimate the lateral extent of failure near the excavation.Based on a practical case of the mine-by test tunnel at an underground research laboratory(URL)in Canada,the influence of rock mass dilation on the depth and extent of failure and deformation is investigated using a calibrated cohesion weakening and frictional strengthening(CWFS)model.It can be found that,when modeling brittle failure of rock masses,the calibrated CWFS model with a constant dilation angle can capture the depth and extent of stress-induced brittle failure in hard rocks at a low confinement if the stress path is correctly represented,as demonstrated by the failure shape observed in the tunnel.However,using a constant dilation angle cannot simulate the nonlinear deformation behavior near the excavation boundary accurately because the dependence of rock mass dilation on confinement and plastic shear strain is not considered.It is illustrated from the numerical simulations that the proposed plastic shear strain and confinement-dependent dilation angle model in combination with the calibrated CWFS model implemented in FLAC can reasonably reveal both rock mass failure and displacement distribution in vicinity of the excavation simultaneously.The simulation results are in good agreement with the field observations and displacement measurement data.