As stressed by Skempton, the shear strength which is mobilised in first-time slides in highly overconsolidated clays can be much less than the peak shear strength measured in ordinary laboratory tests. This paper is devoted to this subject, focusing on the changes of the stress field which precede slope failure. In particular, it is shown that in many cases slope failure must imply a rotation of the principal stresses causing the development of shear strains in a zone whose thickness depends on the initial stress field. In brittle soils this can produce a decrease of the shear strength from the peak to a value comprised between the peak and the critical strength even without formation of a slip surface.

  • Foreword

  • Skempton's contribution

  • Considerations about the mechanics of slope failure

  • A strain-softening mechanism in brittle soils

  • More complex slope failures

  • Further considerations and conclusions

  • References

This content is only available via PDF.
You do not currently have access to this chapter.
Don't already have an account? Register

Purchased this content as a guest? Enter your email address to restore access.

Please enter valid email address.
Email address must be 94 characters or fewer.