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Chapter 10 — Shear Strength

10.1 The Mohr–Coulomb criterion

Shear strength is the soil's resistance to sliding — the property that governs bearing capacity, slope stability, and earth pressure. The Mohr–Coulomb criterion expresses it as:

\[\tau_f = c' + \sigma'_n \tan\phi'\]

where \(c'\) is effective cohesion, \(\sigma'_n\) is the effective normal stress, and \(\phi'\) is the effective friction angle. For total-stress (undrained) conditions, the same form uses \(c_u\) and \(\phi_u = 0\):

\[\tau_f = c_u\]

Figure: soil-mechanics-mohr-coulomb

Figure. The Mohr–Coulomb failure envelope: shear strength \(\tau_f = c' + \sigma'\tan\phi'\), with the failure circle tangent to the envelope (after FHWA-NHI-06-088).

10.2 Drained vs. undrained strength

The choice of strength parameters depends on drainage:

  • Drained — pore pressures have equilibrated; use effective parameters \(c', \phi'\). Critical for long-term conditions and for sands.
  • Undrained — no drainage during loading; use total parameters, usually \(c_u\) with \(\phi = 0\). Critical for short-term conditions in saturated clays.

The lower factor of safety from both governs the design.

10.3 Laboratory tests

  • Direct shear — simple, gives \(c'\) and \(\phi'\); drainage controllable.
  • Triaxial compression — the most versatile: UU (unconsolidated undrained) for \(c_u\); CU (consolidated undrained) with pore-pressure measurement for effective parameters; CD (consolidated drained) for drained strength.
  • Unconfined compression — a quick \(c_u\) for clays.
  • Ring shear — for residual strength on pre-existing slip surfaces.

10.4 Factors affecting shear strength

  • Density and stress history — denser and more over-consolidated soils are stronger.
  • Cementation and structure — natural bonding adds apparent cohesion.
  • Anisotropy and fissures — strength varies with direction; fissures weaken the mass.
  • Rate of loading — undrained strength depends on loading rate.
  • Residual strength — on a pre-existing slip surface, strength drops to the residual value, which governs reactivated landslides.

10.5 Key takeaways

  • \(\tau_f = c' + \sigma'\tan\phi'\) (effective) or \(\tau_f = c_u\) (undrained).
  • Choose drained vs. undrained by the drainage condition; the lower \(F\) governs.
  • Triaxial tests give the full range: UU, CU, CD.
  • Density, stress history, structure, and rate all affect strength.
  • On slip surfaces, use residual strength.