Lateral Earth Pressures & Retaining Wall Design
Soil Mechanics Handbook
Chapter 1.12: Lateral Earth Pressures & Retaining Wall Design
1. Active, Passive, and At-Rest Lateral Earth States
Earth retaining structures must be designed to withstand lateral pressures from the soils they confine. The magnitude of this lateral stress depends directly on the minute outward or inward movement of the retaining wall structure:
- At-Rest State ($K_0$): Occurs when the wall is completely rigid and unyielding. This state is common in unyielding bridge abutments and basement retaining box cells.
- Active State ($K_a$): Occurs when the wall rotates or moves away from the backfill mass. The soil stretches horizontally and reaches a lower-bound pressure limit. Only minimal structural movement ($\approx 0.1\%$ of wall height in sand) is required to trigger this state.
- Passive State ($K_p$): Occurs when the wall is driven heavily into the soil mass. This compresses the soil horizontally until it reaches an upper-bound resistance limit. Activating full passive resistance requires significantly larger structural displacements ($\approx 1\%$ to $5\%$ of wall height).
2. Rankine’s Plastic Equilibrium Formulations
Rankine’s theory (1857) assumes a friction-less vertical wall back and a homogeneous, semi-infinite backfill mass. For a horizontal ground surface profile, the expressions for the lateral coefficients are derived directly from the Mohr-Coulomb failure criteria:
Because $K_a$ and $K_p$ are mathematical reciprocals ($K_a \cdot K_p = 1$), a higher internal friction angle ($\phi$) reduces the active driving thrust and increases the passive stabilizing resistance.
3. Coulomb’s Wedge Theory vs. Wall Friction Effects
Unlike Rankine's approach, **Coulomb’s Theory (1776)** considers a wedge of soil that slips along a failure plane. It accounts for wall friction ($\delta$) and an inclined back face.
Because wall friction generates downward shear resistance along the back face as the soil wedge drops, it curves the actual failure plane. Coulomb's linear wedge assumption provides highly accurate results for active pressures. However, for passive pressure calculations where wall friction is high ($\delta > \phi/2$), it overestimates resistance. In those cases, design engineers substitute **Log-Spiral analytical methods** to prevent unsafe designs.
4. Critical Tension Crack Geometry in Cohesive Backfills
When retaining cohesive ($c-\phi$) soils, the active pressure equation includes a negative cohesion term: $\sigma_a = K_a \sigma_v - 2c\sqrt{K_a}$. At shallow depths, this cohesion term creates a theoretical tensile stress zone.
Because soil cannot sustain tensile forces, the soil pulls away from the wall, forming a **tension crack**. The critical depth of this crack ($z_c$) occurs where the active stress is exactly zero:
Over time, these cracks can fill with rainwater, creating hydrostatic forces. To mitigate this risk, **MoRTH Section 700** mandates the installation of granular filter media wraps and weep-holes to ensure rapid drainage.
๐ฌ Interactive Rankine Earth Pressure Profile Generator
Model a retaining wall structure. Input the backfill variables to generate coefficients, total active thrust forces, and overturning moments.
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