Types of Shear Failure
1. General shear failure:
- It occurs in dense sand or stiff clay.
- A heave on the sides is always observed in general shear failure.
- The failure surfaces extend up to the ground level.
2. Local Shear Failure
- It occurs in medium-dense sand or on in clay of medium consistency.
- Failure surface extend to the ground surface after considerable vertical movement.
- A heave is observed only when there is a substantial vertical settlement
Some characteristics of local shear failure are:
- 1. Failure is not sudden and there is no tilting of footing.
- 2. Failure surface does not reach the ground surface and slight bulging of soil around the footing is observed
- 3. Failure surface is not well defined
- 4. Failure is progressive
- 5. In the load-settlement curve, there is no well-defined peak
- 6. Failure is characterized by considerable settlement directly beneath the foundation
- 7. Significant compression of soil below the footing and partial development of plastic equilibrium is observed.
- 8. Well-defined wedge and slip surface only beneath the foundation.
Local shear Failure
Important Points
- In General Shear Failure A well – defined failure pattern is observed.
3. Punching shear failure:
- It occurs in loose sand or soft clay.
- No heave is observed and failure surface does not extend upto the ground level.
- Only vertical movement of footing.
Criteria for General Shear Failure and Local Shear Failure
- 1. For a cohesionless soil, if Φ is >36°, a general shear failure is likely to occur and, if fΦ< 29°, local shear failure occurs.
- 2. If failure strain is less than 5%, general shear failure will occur and local shear failure occurs at a failure strain of 10–20%.
- 3. It relative density is greater than 70%, general shear failure would occur and if it is less than 35% local shear occurs.
- 4. If N > 30, GSF occurs and if N < 5, LSF occurs.
- 5. If e < 0.55, GSF occurs. If e > 0.75, LSF occurs.