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Derive Mohr-Coulomb principal stress relation

Short answer

Mohr's theory: failure when shear stress reaches a function of normal stress. Mohr-Coulomb: τ_f = c + σ tan φ. From Mohr circle touching failure line: sin φ = (σ1-σ3)/(σ1+σ3+2c cot φ), so σ1 = σ3 tan^2(45°+φ/2) + 2c tan(45°+φ/2); failure plane at 45°+φ/2.

State Mohr's failure theory and derive the Mohr-Coulomb equation, i.e. the relation between the major and minor principal stresses at failure, cohesion and angle of internal friction (draw Mohr's circle with the Mohr-Coulomb failure line).

Mohr's failure theory

Mohr's theory states that a material fails when the shear stress on a plane reaches a limiting value that depends on the normal stress on that plane. Failure is therefore governed by a combination of normal and shear stress, not by the maximum stress alone:

τf=f(σ)\tau_f = f(\sigma)

The curve of τf\tau_f against σ\sigma is the failure envelope. Coulomb approximated it for soils by a straight line, giving the Mohr-Coulomb criterion:

τf=c+σtan⁡ϕ(effective stress: τf=c′+σ′tan⁡ϕ′)\tau_f = c + \sigma\tan\phi \qquad \text{(effective stress: } \tau_f = c' + \sigma'\tan\phi'\text{)}

Here cc is cohesion and ϕ\phi is the angle of internal friction. A stress state is safe if its Mohr circle lies below the line, and the soil fails when the circle touches it.

Derivation of the relation between σ1\sigma_1 and σ3\sigma_3

  tau |          . failure line
      |        .   tau = c + sigma tan(phi)
      |   _.-'-._.
      | .'   |   '.
      |/  phi|  C   \
 -----+-----+-+---+---+------ sigma
      c cot(phi) O   (s3)  (s1)

Consider the Mohr circle at failure, touching the failure line at point TT. Its centre CC is at σ1+σ32\frac{\sigma_1+\sigma_3}{2} and its radius is σ1−σ32\frac{\sigma_1-\sigma_3}{2}. The failure line meets the σ\sigma-axis at O′O', a distance ccot⁡ϕc\cot\phi to the left of the origin. In the right-angled triangle O′TCO'TC, the angle at O′O' is ϕ\phi and CT⊥O′TCT \perp O'T:

sin⁡ϕ=CTO′C=σ1−σ32ccot⁡ϕ+σ1+σ32\sin\phi = \frac{CT}{O'C} = \frac{\dfrac{\sigma_1-\sigma_3}{2}}{c\cot\phi + \dfrac{\sigma_1+\sigma_3}{2}} σ1−σ3=(σ1+σ3)sin⁡ϕ+2ccos⁡ϕ\sigma_1 - \sigma_3 = (\sigma_1+\sigma_3)\sin\phi + 2c\cos\phi σ1(1−sin⁡ϕ)=σ3(1+sin⁡ϕ)+2ccos⁡ϕ\sigma_1(1-\sin\phi) = \sigma_3(1+\sin\phi) + 2c\cos\phi σ1=σ3 1+sin⁡ϕ1−sin⁡ϕ+2c cos⁡ϕ1−sin⁡ϕ\boxed{\sigma_1 = \sigma_3\,\frac{1+\sin\phi}{1-\sin\phi} + 2c\,\frac{\cos\phi}{1-\sin\phi}}

Using 1+sin⁡ϕ1−sin⁡ϕ=tan⁡2(45∘+ϕ2)\frac{1+\sin\phi}{1-\sin\phi} = \tan^2\left(45^\circ+\frac{\phi}{2}\right) and cos⁡ϕ1−sin⁡ϕ=tan⁡(45∘+ϕ2)\frac{\cos\phi}{1-\sin\phi} = \tan\left(45^\circ+\frac{\phi}{2}\right):

σ1=σ3tan⁡2(45∘+ϕ2)+2ctan⁡(45∘+ϕ2)\sigma_1 = \sigma_3\tan^2\left(45^\circ+\frac{\phi}{2}\right) + 2c\tan\left(45^\circ+\frac{\phi}{2}\right)

Equivalent form: σ3=σ1tan⁡2(45∘−ϕ2)−2ctan⁡(45∘−ϕ2)\sigma_3 = \sigma_1\tan^2\left(45^\circ-\frac{\phi}{2}\right) - 2c\tan\left(45^\circ-\frac{\phi}{2}\right).

Failure plane angle: in triangle O′TCO'TC the angle ∠TCO′\angle TCO' is 90∘−ϕ90^\circ-\phi. The radius CTCT therefore makes an angle 2θf=180∘−(90∘−ϕ)=90∘+ϕ2\theta_f = 180^\circ - (90^\circ-\phi) = 90^\circ+\phi with the radius to the σ1\sigma_1 point, so the failure plane is inclined at θf=45∘+ϕ2\theta_f = 45^\circ + \frac{\phi}{2} to the major principal plane.

For cohesionless soil (c=0c=0): σ1=σ3tan⁡2(45∘+ϕ/2)\sigma_1 = \sigma_3\tan^2(45^\circ+\phi/2). For a saturated clay in undrained loading (ϕu=0\phi_u=0): σ1−σ3=2cu\sigma_1 - \sigma_3 = 2c_u.

✓ Answer checked by Claude Opus 5.5 (high effort)

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