Numerical Analyses of the Influence of Blast-Induced Damaged Rock Around Shallow Tunnels in Brittle Rock
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Abstract
Most of the railway tunnels in Sweden are shallow-seated (<20 m of rock cover) and are located in hard brittle rock masses. The majority of these tunnels are excavated by drilling and blasting, which, consequently, result in the development of a blast-induced damaged zone around the tunnel boundary. Theoretically, the presence of this zone, with its reduced strength and stiffness, will affect the overall performance of the tunnel, as well as its construction and maintenance. The Swedish Railroad Administration, therefore, uses a set of guidelines based on peak particle velocity models and perimeter blasting to regulate the extent of damage due to blasting. However, the real effects of the damage caused by blasting around a shallow tunnel and their criticality to the overall performance of the tunnel are yet to be quantified and, therefore, remain the subject of research and investigation. This paper presents a numerical parametric study of blast-induced damage in rock. By varying the strength and stiffness of the blast-induced damaged zone and other relevant parameters, the near-field rock mass response was evaluated in terms of the effects on induced boundary stresses and ground deformation. The continuum method of numerical analysis was used. The input parameters, particularly those relating to strength and stiffness, were estimated using a systematic approach related to the fact that, at shallow depths, the stress and geologic conditions may be highly anisotropic. Due to the lack of data on the post-failure characteristics of the rock mass, the traditional Mohr–Coulomb yield criterion was assumed and used. The results clearly indicate that, as expected, the presence of the blast-induced damage zone does affect the behaviour of the boundary stresses and ground deformation. Potential failure types occurring around the tunnel boundary and their mechanisms have also been identified.
Keywords
Blast-induced damaged zone Overbreak Inherent rock properties Brittle rock Rock mass strength and stiffness Shallow tunnels Numerical analysesList of Symbols
For Undamaged Rock Mass
- σi
intact compressive strength (MPa)
- σm
compressive strength of the undamaged rock mass (MPa)
- Em
deformation modulus of the undamaged rock mass (GPa)
- ϕm
frictional strength of the undamaged rock mass (°)
- cm
cohesive strength of the undamaged rock mass (MPa)
- σtm
tensile strength of the undamaged rock mass (MPa)
For Damaged Rock Mass
- D
disturbance factor
- σd
compressive strength of the damaged rock mass (MPa)
- Ed
deformation modulus of the damaged rock mass at the tunnel boundary (GPa)
- Ed(ij)
deformation modulus of the damaged rock mass at point i, j (GPa)
- ϕd
frictional strength of the damaged rock mass (°)
- cd
cohesive strength of the damaged rock mass (MPa)
- σtd
tensile strength of the damaged rock mass (MPa)
- Ld
total thickness of the damaged rock zone (m)
- Ld(ij)
thickness of the damaged rock zone at point i, j (m)
- σdUB
upper bound compressive strength of the damaged rock mass
- σdBC
base case compressive strength of the damaged rock mass
- σdLB
lower bound compressive strength of the damaged rock mass
- cdUB
upper bound cohesive strength of the damaged rock mass
- cdBC
base case cohesive strength of the damaged rock mass
- cdLB
lower bound cohesive strength of the damaged rock mass
Other Notations
- σθ − σr
induced differential or deviatoric stress
- σθ
tangential stress (induced)
- σr
radial stress (induced)
- σ3max
maximum confining stress
- σ3min
minimum confining stress
- σnmax
maximum normal stress derived from normal stress–shear stress envelope
- σnmin
minimum normal stress derived from normal stress–shear stress envelope
- τmax
maximum shear stress derived from normal stress–shear stress envelope
- τmin
minimum shear stress derived from normal stress–shear stress envelope
Notes
Acknowledgements
The authors wish to acknowledge the Swedish Railroad Administration (Banverket) for funding this study, and Mr. Peter Lundman and Dr. Finn Ouchterlony for discussing the tunnel and rock excavation guidelines in Sweden. Doctors Evert Hoek and Mark Diederichs are sincerely acknowledged for their communications regarding the use of the Hoek–Brown criterion for shallow excavations and the use of disturbance factor descriptions for estimating the deformation modulus for the damaged rock.
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