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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.

Last updated: July 2026

2.3 Shear Strength Principles & Laboratory Testing

1. Mohr-Coulomb Failure Criterion

The shear strength of soil (τf\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:

τf=c′+σ′tan⁡ϕ′=c′+(σ−u)tan⁡ϕ′\tau_f = c' + \sigma' \tan\phi' = c' + (\sigma - u) \tan\phi'

Where:

  • c′c': Effective cohesion intercept (interparticle chemical bonding or cementation).
  • ϕ′\phi': Effective angle of internal friction (interlocking and mineral friction).
  • σ′\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 (σ1′\sigma'_1) and minor (σ3′\sigma'_3) effective principal stresses at failure satisfy:

σ1′=σ3′tan⁡2(45∘+ϕ′2)+2c′tan⁡(45∘+ϕ′2)=σ3′Nϕ+2c′Nϕ\sigma'_1 = \sigma'_3 \tan^2\left(45^\circ + \frac{\phi'}{2}\right) + 2 c' \tan\left(45^\circ + \frac{\phi'}{2}\right) = \sigma'_3 N_\phi + 2 c' \sqrt{N_\phi}

Where Nϕ=tan⁡2(45∘+ϕ′2)=1+sin⁡ϕ′1−sin⁡ϕ′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 θ\theta relative to the major principal stress plane (the horizontal plane when vertical stress is major):

θ=45∘+ϕ′2\theta = 45^\circ + \frac{\phi'}{2}

2. Laboratory Shear Strength Testing Methods

Test MethodSpecimen Drainage & StateMeasured ParametersKey Advantages / Limitations
Direct Shear Test (DST)Drained shear along a predetermined horizontal plane.Drained parameters (c′,ϕ′c', \phi').Simple, fast; forced failure plane, non-uniform stress/strain distribution.
Unconfined Compression (UC)Undrained compression (σ3=0\sigma_3 = 0), fast loading of saturated clay.Unconfined strength quq_u; Su=cu=qu/2S_u = c_u = q_u / 2.Quick, economical; only valid for saturated cohesive soils (ϕu=0\phi_u = 0).
Triaxial (UU)Unconsolidated-Undrained: no consolidation under σ3\sigma_3, no drainage during shear.Undrained shear strength Su=cuS_u = c_u (ϕu=0\phi_u = 0).Simulates end-of-construction short-term loading in saturated soft clays.
Triaxial (CU)Consolidated-Undrained: isotropic consolidation under σ3\sigma_3, sheared undrained with uu measured.Total (c,ϕc, \phi) and effective (c′,ϕ′c', \phi') parameters.Measures pore pressures (uu); simulates rapid drawdown or post-consolidation loading.
Triaxial (CD)Consolidated-Drained: full consolidation under σ3\sigma_3, sheared slowly (u=0u = 0).Drained parameters (c′,ϕ′c', \phi').Simulates long-term steady-state stability of slopes and retaining walls.

3. Detailed Triaxial Testing Framework

A cylindrical soil specimen (H:D=2:1H:D = 2:1) is encased in a rubber membrane, placed in a pressurized chamber (σ3\sigma_3), and loaded axially by a piston (Δσ=σ1−σ3\Delta\sigma = \sigma_1 - \sigma_3, termed the deviator stress).

Unconsolidated-Undrained (UU / Total Stress) Test

  • Cell pressure σ3\sigma_3 applied with drainage closed.
  • Axial deviator stress Δσ\Delta\sigma increased to failure with drainage closed.
  • For fully saturated soils (S=100%S = 100\%), increasing σ3\sigma_3 causes an equal pore pressure increase (Δu=Δσ3\Delta u = \Delta\sigma_3). Consequently, effective principal stress remains unchanged.
  • Mohr circles of total stress at failure for various σ3\sigma_3 have identical diameters (Δσf\Delta\sigma_f).
  • Total stress envelope is horizontal: ϕu=0andτf=cu=Su=σ1,f−σ3,f2\phi_u = 0 \quad \text{and} \quad \tau_f = c_u = S_u = \frac{\sigma_{1,f} - \sigma_{3,f}}{2}

Consolidated-Undrained (CU) Test with Pore Pressure Measurement

  • Specimen consolidated under cell pressure σ3\sigma_3 with drainage open (u→0u \to 0).
  • Drainage valves closed, axial load applied to failure while measuring excess pore pressure ufu_f.
  • Effective principal stresses at failure: σ3′=σ3−ufandσ1′=σ1−uf=σ3+Δσf−uf\sigma'_3 = \sigma_3 - u_f \quad \text{and} \quad \sigma'_1 = \sigma_1 - u_f = \sigma_3 + \Delta\sigma_f - u_f
  • Allows determination of both total parameters (c,ϕc, \phi) and effective parameters (c′,ϕ′c', \phi').

Skempton's Pore Pressure Parameters:

Δu=B[Δσ3+A(Δσ1−Δσ3)]\Delta u = B \left[ \Delta\sigma_3 + A (\Delta\sigma_1 - \Delta\sigma_3) \right]
  • For saturated soils, B=1.0B = 1.0.
  • Parameter AA at failure (AfA_f): Af<0A_f < 0 (heavily overconsolidated/dilative), Af=0.5−1.0A_f = 0.5 - 1.0 (normally consolidated clay), Af>1.0A_f > 1.0 (sensitive/collapsible clay).

Consolidated-Drained (CD) Test

  • Specimen fully consolidated under σ3\sigma_3.
  • Axial shearing performed at an extremely slow strain rate to ensure u≈0u \approx 0 throughout.
  • Total stresses equal effective stresses (σ1=σ1′,σ3=σ3′\sigma_1 = \sigma'_1, \sigma_3 = \sigma'_3).
  • For normally consolidated clays and clean sands, effective cohesion is zero (c′=0c' = 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 (ecrite_{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=1OCR = 1): Contractive behavior, positive AfA_f, c′≈0c' \approx 0.
  • Overconsolidated Clay (OCR>4−8OCR > 4-8): Dilative behavior, negative AfA_f, exhibits true/apparent effective cohesion c′>0c' > 0.

5. Stress Paths in p′−qp'-q Space

To track continuous stress states during testing without drawing multiple Mohr circles, stress paths plot invariant stress parameters:

p′=σ1′+σ3′2andq=σ1′−σ3′2=Δσ2p' = \frac{\sigma'_1 + \sigma'_3}{2} \quad \text{and} \quad q = \frac{\sigma'_1 - \sigma'_3}{2} = \frac{\Delta\sigma}{2}

The failure line in p′−qp'-q space is defined by:

q=a′+p′tan⁡α′q = a' + p' \tan\alpha'

Converting a′a' and α′\alpha' to Mohr-Coulomb parameters c′c' and ϕ′\phi':

sin⁡ϕ′=tan⁡α′⟺ϕ′=arcsin⁡(tan⁡α′)\sin\phi' = \tan\alpha' \quad \Longleftrightarrow \quad \phi' = \arcsin(\tan\alpha') c′=a′cos⁡ϕ′c' = \frac{a'}{\cos\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′=0c' = 0). The test results at failure are:

  • Chamber cell pressure: σ3=200 kPa\sigma_3 = 200 \text{ kPa}
  • Deviator stress at failure: Δσf=160 kPa\Delta\sigma_f = 160 \text{ kPa}
  • Measured pore pressure at failure: uf=100 kPau_f = 100 \text{ kPa}

Calculate:

  1. Total principal stresses (σ1,σ3\sigma_1, \sigma_3) and total principal stress ratio at failure.
  2. Effective principal stresses (σ1′,σ3′\sigma'_1, \sigma'_3) at failure.
  3. Effective angle of internal friction (ϕ′\phi').
  4. Orientation of the failure plane (θ\theta) relative to the horizontal major principal plane.
  5. Effective normal stress (σ′\sigma') and shear stress (τf\tau_f) on the failure plane.

Solution:

  1. Total Principal Stresses:

    σ3=200 kPa\sigma_3 = 200 \text{ kPa} σ1=σ3+Δσf=200+160=360 kPa\sigma_1 = \sigma_3 + \Delta\sigma_f = 200 + 160 = 360 \text{ kPa} Total Ratio σ1σ3=360200=1.80\text{Total Ratio } \frac{\sigma_1}{\sigma_3} = \frac{360}{200} = 1.80
  2. Effective Principal Stresses:

    σ3′=σ3−uf=200−100=100 kPa\sigma'_3 = \sigma_3 - u_f = 200 - 100 = 100 \text{ kPa} σ1′=σ1−uf=360−100=260 kPa\sigma'_1 = \sigma_1 - u_f = 360 - 100 = 260 \text{ kPa}
  3. Effective Angle of Internal Friction (ϕ′\phi'): For normally consolidated clay (c′=0c' = 0), the principal stress relationship is:

    σ1′=σ3′tan⁡2(45∘+ϕ′2)=σ3′(1+sin⁡ϕ′1−sin⁡ϕ′)\sigma'_1 = \sigma'_3 \tan^2\left(45^\circ + \frac{\phi'}{2}\right) = \sigma'_3 \left(\frac{1 + \sin\phi'}{1 - \sin\phi'}\right) σ1′σ3′=260100=2.60\frac{\sigma'_1}{\sigma'_3} = \frac{260}{100} = 2.60 1+sin⁡ϕ′1−sin⁡ϕ′=2.60  ⟹  1+sin⁡ϕ′=2.60(1−sin⁡ϕ′)=2.60−2.60sin⁡ϕ′\frac{1 + \sin\phi'}{1 - \sin\phi'} = 2.60 \implies 1 + \sin\phi' = 2.60 (1 - \sin\phi') = 2.60 - 2.60 \sin\phi' 3.60sin⁡ϕ′=1.60  ⟹  sin⁡ϕ′=1.603.60=0.44443.60 \sin\phi' = 1.60 \implies \sin\phi' = \frac{1.60}{3.60} = 0.4444 ϕ′=arcsin⁡(0.4444)=26.38∘\phi' = \arcsin(0.4444) = 26.38^\circ
  4. Failure Plane Orientation (θ\theta):

    θ=45∘+ϕ′2=45∘+26.38∘2=45∘+13.19∘=58.19∘\theta = 45^\circ + \frac{\phi'}{2} = 45^\circ + \frac{26.38^\circ}{2} = 45^\circ + 13.19^\circ = 58.19^\circ
  5. Stresses on Failure Plane:

    σ′=σ1′+σ3′2+σ1′−σ3′2cos⁡(2θ)=260+1002+260−1002cos⁡(116.38∘)\sigma' = \frac{\sigma'_1 + \sigma'_3}{2} + \frac{\sigma'_1 - \sigma'_3}{2} \cos(2\theta) = \frac{260 + 100}{2} + \frac{260 - 100}{2} \cos(116.38^\circ) σ′=180+80(−0.4444)=180−35.56=144.44 kPa\sigma' = 180 + 80 (-0.4444) = 180 - 35.56 = 144.44 \text{ kPa} τf=σ′tan⁡ϕ′=144.44×tan⁡(26.38∘)=144.44×0.4960=71.64 kPa\tau_f = \sigma' \tan\phi' = 144.44 \times \tan(26.38^\circ) = 144.44 \times 0.4960 = 71.64 \text{ kPa}

    Alternatively, using τf=σ1′−σ3′2sin⁡(2θ)=80×sin⁡(116.38∘)=80×0.8958=71.66 kPa✓\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

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Mohr-Coulomb Failure Envelope and Effective Stress Circle
Test Your Knowledge

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

35 kPa

B

50 kPa

C

70 kPa

D

140 kPa

Test Your Knowledge

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'?

A

19.5°

B

25.0°

C

26.4°

D

30.0°

Test Your Knowledge

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

Unconsolidated-Undrained (UU) test

B

Consolidated-Undrained (CU) test with pore pressure measurement

C

Consolidated-Drained (CD) test

D

Direct Shear Test (DST)

Test Your Knowledge

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?

A

45°

B

60°

C

75°

D

30°

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