Shear Strength of Soil

The shear strength of a soil is its resistance to shearing stresses. It is a fundamental property required to analyze the stability of slopes, the bearing capacity of foundations, and the lateral earth pressure on retaining walls.

Mohr-Coulomb Failure Criterion

The shear strength (τf\tau_f) is typically described by the Mohr-Coulomb Failure Criterion, which states that failure occurs when the shear stress on any plane reaches a critical value dependent on the normal stress on that plane.

Shear Strength Equation

Effective Stress Analysis (Drained)

$$ \tau_f = c' + \sigma' \tan \phi' $$
Total Stress Analysis (Undrained): For saturated clays loaded rapidly, pore pressures do not dissipate.

Total Stress Analysis (Undrained)

$$ \tau_f = c_u + \sigma \tan \phi_u $$

Interactive Mohr's Circle

Visualize the state of stress and the failure envelope. Adjust the principal stresses (σ1,σ3\sigma_1, \sigma_3) and soil properties (c,ϕc, \phi) to see when failure occurs.

Mohr-Coulomb Failure Criterion

Stable
Major Stress (σ₁)100
Minor Stress (σ₃)40
Cohesion (c)10
Friction Angle (φ)30 °
σ (Normal)τ (Shear)Failure Envelopeσ₁σ₃τ_max = 30

If the circle touches or crosses the red failure envelope, the soil fails in shear. The radius of the circle represents the maximum shear stress (taumax=(sigma1sigma3)/2\\tau_{max} = (\\sigma_1 - \\sigma_3)/2).

Pore Pressure Parameters (Skempton)

To predict how pore water pressure (uu) will change in a saturated clay when subjected to changes in total principal stresses (Δσ1,Δσ3\Delta \sigma_1, \Delta \sigma_3), engineers use Skempton's Pore Pressure Parameters (AA and BB).

Skempton's Equation

The change in pore water pressure (Δu\Delta u) during undrained loading is given by:

Skempton's Pore Pressure Equation

$$ \Delta u = B [ \Delta \sigma_3 + A (\Delta \sigma_1 - \Delta \sigma_3) ] $$

Laboratory Tests

To determine the shear strength parameters (c,ϕc, \phi), several laboratory tests are used.

Direct Shear Test

A sample is placed in a split box and sheared along a predetermined horizontal plane.
  • Procedure: Apply normal load (NN), then apply shear force (TT) until failure. Repeat for different normal loads.
  • Advantages: Simple, inexpensive, good for sands.
  • Disadvantages: Failure plane is forced, stress distribution is non-uniform, drainage is hard to control.

Triaxial Test

A cylindrical sample is encased in a rubber membrane and subjected to confining pressure (σ3\sigma_3). An axial load (Δσd\Delta \sigma_d) is increased until failure.
  • UU (Unconsolidated-Undrained): Quick test. Simulates end-of-construction stability for saturated clays. (ϕu=0,cu\phi_u = 0, c_u).
  • CU (Consolidated-Undrained): Sample consolidated under σ3\sigma_3, then sheared undrained. Pore pressure (uu) is measured to get effective strength parameters (c,ϕc', \phi').
  • CD (Consolidated-Drained): Slow test. Excess pore pressure dissipates completely. Simulates long-term stability. (c,ϕc', \phi').

Unconfined Compression Test (UCT)

A special case of the triaxial test where confining pressure σ3=0\sigma_3 = 0.
  • quq_u: Unconfined compressive strength.
  • cu=qu/2c_u = q_u / 2: Undrained shear strength.
  • Suitable only for cohesive soils (clays).

Field Tests

Vane Shear Test (VST)

Used for soft to stiff clays. A four-bladed vane is pushed into the soil and rotated.

Vane Shear Strength

$$ c_u = \frac{T}{\pi \left( \frac{d^2 h}{2} + \frac{d^3}{6} \right)} $$
Key Takeaways
  • Shear Strength depends on cohesion (cc) and friction angle (ϕ\phi).
  • Mohr's Circle is used to represent the stress state at a point. Failure occurs when the circle touches the Failure Envelope.
  • Effective Stress Parameters (c,ϕc', \phi') govern long-term stability and drained conditions.
  • Total Stress Parameters (cu,ϕuc_u, \phi_u) govern short-term stability in saturated clays (End-of-Construction).
  • Skempton's Parameters (AA and BB) are essential for predicting undrained pore pressure responses to loading.
  • Triaxial Tests (UU, CU, CD) provide the most comprehensive data on soil strength and pore pressure behavior.