2.3 Shear Strength Principles & Laboratory Testing
Key Takeaways
- The Mohr-Coulomb failure criterion defines soil shear strength as τf = c' + σ' tan φ', governed by effective cohesion (c') and effective friction angle (φ').
- Direct Shear Testing (DST) provides rapid drained strength parameters on horizontal failure planes, whereas Unconfined Compression (UC) tests give quick undrained shear strength (Su = qu / 2) for saturated clays.
- Triaxial testing variants (UU, CU, CD) simulate distinct field drainage conditions; CU testing with pore pressure measurement yields both total (c, φ) and effective (c', φ') strength parameters.
- Cohesionless soils exhibit contractive (loose sand) or dilative (dense sand) volumetric response during shear, converging toward a critical state void ratio (ecrit).
- Stress path representation in p'-q space converts circular failure envelopes into linear relations (q = a' + p' tan α'), facilitating continuous stress evolution tracking during loading.
2.3 Shear Strength Principles & Laboratory Testing
1. Mohr-Coulomb Failure Criterion
The shear strength of soil ($\tau_f$) is the maximum resistance per unit area that a soil mass can offer against sliding along an internal failure surface under applied stress.
Effective Stress Form of Mohr-Coulomb Criterion:
Where:
- $c'$: Effective cohesion intercept (interparticle chemical bonding or cementation).
- $\phi'$: Effective angle of internal friction (interlocking and mineral friction).
- $\sigma'$: Effective normal stress acting on the failure plane.
Principal Stresses at Failure
In Mohr's circle of stress, failure occurs when the circle becomes tangent to the Mohr-Coulomb envelope. The major ($\sigma'_1$) and minor ($\sigma'_3$) effective principal stresses at failure satisfy:
Where $N_\phi = \tan^2\left(45^\circ + \frac{\phi'}{2}\right) = \frac{1 + \sin\phi'}{1 - \sin\phi'}$.
Failure Plane Orientation
The failure plane is inclined at an angle $\theta$ relative to the major principal stress plane (the horizontal plane when vertical stress is major):
2. Laboratory Shear Strength Testing Methods
| Test Method | Specimen Drainage & State | Measured Parameters | Key Advantages / Limitations |
|---|---|---|---|
| Direct Shear Test (DST) | Drained shear along a predetermined horizontal plane. | Drained parameters ($c', \phi'$). | Simple, fast; forced failure plane, non-uniform stress/strain distribution. |
| Unconfined Compression (UC) | Undrained compression ($\sigma_3 = 0$), fast loading of saturated clay. | Unconfined strength $q_u$; $S_u = c_u = q_u / 2$. | Quick, economical; only valid for saturated cohesive soils ($\phi_u = 0$). |
| Triaxial (UU) | Unconsolidated-Undrained: no consolidation under $\sigma_3$, no drainage during shear. | Undrained shear strength $S_u = c_u$ ($\phi_u = 0$). | Simulates end-of-construction short-term loading in saturated soft clays. |
| Triaxial (CU) | Consolidated-Undrained: isotropic consolidation under $\sigma_3$, sheared undrained with $u$ measured. | Total ($c, \phi$) and effective ($c', \phi'$) parameters. | Measures pore pressures ($u$); simulates rapid drawdown or post-consolidation loading. |
| Triaxial (CD) | Consolidated-Drained: full consolidation under $\sigma_3$, sheared slowly ($u = 0$). | Drained parameters ($c', \phi'$). | Simulates long-term steady-state stability of slopes and retaining walls. |
3. Detailed Triaxial Testing Framework
A cylindrical soil specimen ($H:D = 2:1$) is encased in a rubber membrane, placed in a pressurized chamber ($\sigma_3$), and loaded axially by a piston ($\Delta\sigma = \sigma_1 - \sigma_3$, termed the deviator stress).
Unconsolidated-Undrained (UU / Total Stress) Test
- Cell pressure $\sigma_3$ applied with drainage closed.
- Axial deviator stress $\Delta\sigma$ increased to failure with drainage closed.
- For fully saturated soils ($S = 100%$), increasing $\sigma_3$ causes an equal pore pressure increase ($\Delta u = \Delta\sigma_3$). Consequently, effective principal stress remains unchanged.
- Mohr circles of total stress at failure for various $\sigma_3$ have identical diameters ($\Delta\sigma_f$).
- Total stress envelope is horizontal:
Consolidated-Undrained (CU) Test with Pore Pressure Measurement
- Specimen consolidated under cell pressure $\sigma_3$ with drainage open ($u \to 0$).
- Drainage valves closed, axial load applied to failure while measuring excess pore pressure $u_f$.
- Effective principal stresses at failure:
- Allows determination of both total parameters ($c, \phi$) and effective parameters ($c', \phi'$).
Skempton's Pore Pressure Parameters:
- For saturated soils, $B = 1.0$.
- Parameter $A$ at failure ($A_f$): $A_f < 0$ (heavily overconsolidated/dilative), $A_f = 0.5 - 1.0$ (normally consolidated clay), $A_f > 1.0$ (sensitive/collapsible clay).
Consolidated-Drained (CD) Test
- Specimen fully consolidated under $\sigma_3$.
- Axial shearing performed at an extremely slow strain rate to ensure $u \approx 0$ throughout.
- Total stresses equal effective stresses ($\sigma_1 = \sigma'_1, \sigma_3 = \sigma'_3$).
- For normally consolidated clays and clean sands, effective cohesion is zero ($c' = 0$).
4. Drained vs. Undrained Soil Response & Critical State Concept
Granular Soil Behavior (Sands)
- Loose Sand: Contractive during shear (volume decreases), generating positive pore pressure in undrained loading. Reaches peak strength smoothly.
- Dense Sand: Dilative during shear (volume expands due to particle interlocking), generating negative pore pressure in undrained loading. Exhibits sharp peak strength followed by strain softening to critical state.
- Critical State: At large shear strains, all specimens reach the critical state void ratio ($e_{crit}$) where continuous shearing occurs at constant volume and constant shear stress without further volume change.
Fine-Grained Soil Behavior (Clays)
- Normally Consolidated Clay ($OCR = 1$): Contractive behavior, positive $A_f$, $c' \approx 0$.
- Overconsolidated Clay ($OCR > 4-8$): Dilative behavior, negative $A_f$, exhibits true/apparent effective cohesion $c' > 0$.
5. Stress Paths in $p'-q$ Space
To track continuous stress states during testing without drawing multiple Mohr circles, stress paths plot invariant stress parameters:
The failure line in $p'-q$ space is defined by:
Converting $a'$ and $\alpha'$ to Mohr-Coulomb parameters $c'$ and $\phi'$:
6. Comprehensive Worked Example
Problem Statement: A Consolidated-Undrained (CU) triaxial compression test with pore pressure measurement was conducted on a saturated normally consolidated clay ($c' = 0$). The test results at failure are:
- Chamber cell pressure: $\sigma_3 = 200 \text{ kPa}$
- Deviator stress at failure: $\Delta\sigma_f = 160 \text{ kPa}$
- Measured pore pressure at failure: $u_f = 100 \text{ kPa}$
Calculate:
- Total principal stresses ($\sigma_1, \sigma_3$) and total principal stress ratio at failure.
- Effective principal stresses ($\sigma'_1, \sigma'_3$) at failure.
- Effective angle of internal friction ($\phi'$).
- Orientation of the failure plane ($\theta$) relative to the horizontal major principal plane.
- Effective normal stress ($\sigma'$) and shear stress ($\tau_f$) on the failure plane.
Solution:
-
Total Principal Stresses:
-
Effective Principal Stresses:
-
Effective Angle of Internal Friction ($\phi'$): For normally consolidated clay ($c' = 0$), the principal stress relationship is:
-
Failure Plane Orientation ($\theta$):
-
Stresses on Failure Plane: Alternatively, using $\tau_f = \frac{\sigma'_1 - \sigma'_3}{2} \sin(2\theta) = 80 \times \sin(116.38^\circ) = 80 \times 0.8958 = 71.66 \text{ kPa} \quad \checkmark$$
An unconfined compression test (UC) on a saturated clay specimen yields an unconfined compressive strength qu = 140 kPa. What is the undrained shear strength Su of the clay?
A Consolidated-Drained (CD) triaxial test on a normally consolidated clay (c' = 0) fails at an effective minor principal stress σ'3 = 100 kPa and an effective major principal stress σ'1 = 300 kPa. What is the effective internal friction angle φ'?
Which laboratory triaxial test procedure is most appropriate to evaluate the immediate, short-term stability of an embankment foundation constructed rapidly over a saturated soft clay deposit?
A soil specimen has an effective angle of internal friction φ' = 30°. At what angle θ relative to the major principal stress plane will the failure plane form?