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Shear strength on horizontal plane, WT 3.5 m

Short answer

Water table at 3.5 m: γ = 19.29 kN/m³, σ′ = 57.9 kPa, shear strength = 57.9 tan30° = 33.4 kPa. Water table at surface: γsat = 20.93 kN/m³, σ′ = (20.93−9.81)×3 = 33.4 kPa, strength = 33.4 tan30° = 19.3 kPa.

Calculate the potential shear strength on a horizontal plane at a depth of 3 m below the surface in a formation of cohesionless soil when the water table is at a depth of 3.5 m. The degree of saturation may be taken as 0.5 on the average. Void ratio = 0.50; grain specific gravity = 2.70; angle of internal friction = 30°. What will be the modified value of shear strength if the water table reaches the ground surface?

Assumptions: γw=9.81\gamma_w = 9.81 kN/m³; the soil above the water table is partly saturated (Sr=0.5S_r = 0.5); c=0c=0 and capillary effects are neglected. Strength =σ′tan⁡ϕ= \sigma'\tan\phi on the horizontal plane.

Case 1: Water table at 3.5 m (below the 3 m depth, so there is no pore pressure at the plane)

γ=(Gs+Sre)γw1+e=(2.70+0.5×0.50)(9.81)1.50=19.29 kN/m3\gamma = \frac{(G_s + S_r e)\gamma_w}{1+e} = \frac{(2.70 + 0.5\times0.50)(9.81)}{1.50} = 19.29\ \text{kN/m}^3 σ′=σ=19.29×3=57.9 kPa\sigma' = \sigma = 19.29\times 3 = 57.9\ \text{kPa} s=σ′tan⁡ϕ=57.9tan⁡30∘=33.4 kPas = \sigma'\tan\phi = 57.9\tan30^\circ = 33.4\ \text{kPa}

Case 2: Water table at the ground surface (fully saturated, Sr=1S_r = 1)

γsat=(Gs+e)γw1+e=(2.70+0.50)(9.81)1.50=20.93 kN/m3\gamma_{sat} = \frac{(G_s + e)\gamma_w}{1+e} = \frac{(2.70+0.50)(9.81)}{1.50} = 20.93\ \text{kN/m}^3 σ′=(20.93−9.81)×3=33.4 kPa\sigma' = (20.93 - 9.81)\times 3 = 33.4\ \text{kPa} s=33.4tan⁡30∘=19.3 kPas = 33.4\tan30^\circ = 19.3\ \text{kPa}

Answer: shear strength is about 33.4 kPa with the water table at 3.5 m, and falls to about 19.3 kPa (a reduction of about 42%) when the water table rises to the ground surface.

✓ Answer checked by Claude Opus 5.5 (high effort)

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