Lateral earth pressures are crucial in designing retaining walls and understanding soil-structure interactions. This topic explores three key pressure states: at-rest, active, and passive. Each state represents different soil conditions and wall movements, affecting the magnitude of horizontal stresses on structures.
Understanding these pressure states helps engineers design safer and more efficient retaining structures. We'll examine factors influencing earth pressures, calculation methods, and their impact on wall stability. This knowledge is essential for tackling real-world geotechnical challenges in construction and earthwork projects.
Earth Pressure States in Soil
Types of Earth Pressure States
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Top images from around the web for Types of Earth Pressure States Crib Walls and Retaining Walls – Trailism View original
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12.1 Stress and Strain | Physical Geology View original
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Earth pressure states represent horizontal stresses exerted by soil on retaining structures
At-rest earth pressure develops when retaining structure experiences no lateral movement
Active earth pressure occurs when retaining wall moves away from soil mass
Allows soil to expand horizontally
Reduces lateral pressure
Passive earth pressure forms when retaining wall moves towards soil mass
Compresses soil
Increases lateral pressure
Magnitude of earth pressure follows order passive > at-rest > active
Earth pressure coefficients (K) relate vertical effective stress to horizontal effective stress
K0 for at-rest state
Ka for active state
Kp for passive state
Transition from at-rest to active or passive states involves soil deformation
Stress redistribution within soil mass occurs during state changes
Soil particles rearrange leading to volume changes (expansion or compression)
Shear planes may develop in soil mass during active or passive pressure development
Magnitude of wall movement required for full active or passive pressure development varies
Typically 0.1-0.5% of wall height for active state (sandy soils)
Approximately 2-4% of wall height for passive state (sandy soils)
Stress paths differ for each pressure state transition
Factors Influencing Earth Pressure
Soil Properties and Groundwater Conditions
Soil type impacts earth pressure magnitudes (sand, clay, silt)
Unit weight of soil affects vertical stress and resulting lateral pressures
Cohesion in clayey soils reduces active pressures and increases passive resistance
Internal friction angle influences soil shear strength and pressure coefficients
Groundwater conditions alter effective stresses in soil mass
Saturated soil exerts higher pressures due to buoyancy effects
Seepage forces can increase or decrease earth pressures
Pore water pressures impact effective stress calculations
Positive pore pressures reduce effective stress
Negative pore pressures (suction) can increase soil strength
Structural Geometry and Loading Conditions
Retaining structure height directly affects magnitude of earth pressures
Wall inclination modifies pressure distribution and resultant force direction
Surcharge loads on retained soil increase earth pressures
Uniform loads (distributed pressure)
Point loads (concentrated forces)
Type of wall movement influences pressure state development
Rotation about top (active case)
Rotation about bottom (passive case)
Translation (uniform movement)
Soil compaction during backfilling can induce residual lateral stresses
Overconsolidation ratio affects at-rest earth pressure coefficient (K0)
Higher OCR leads to increased K0 values
Environmental and Reinforcement Factors
Temperature changes cause soil volume fluctuations
Expansion in hot conditions
Contraction in cold conditions
Freeze-thaw cycles alter soil structure and strength properties
Moisture content fluctuations impact soil cohesion and effective stress
Reinforcement elements modify earth pressure distribution
Geosynthetics (geotextiles, geogrids) in mechanically stabilized earth walls
Soil nails in nailed soil walls
Anchors or tiebacks in anchored wall systems
Vegetation root systems can provide additional soil reinforcement
Chemical changes in soil (e.g., cementation) may alter pressure characteristics over time
Earth Pressure Calculation
Rankine's and Coulomb's Earth Pressure Theories
Rankine's theory calculates active and passive earth pressures
Assumes cohesionless soils, horizontal backfills, vertical walls
Neglects wall friction
Active pressure coefficient: K a = t a n 2 ( 45 ° − φ / 2 ) K_a = tan^2(45° - φ/2) K a = t a n 2 ( 45° − φ /2 )
Passive pressure coefficient: K p = t a n 2 ( 45 ° + φ / 2 ) K_p = tan^2(45° + φ/2) K p = t a n 2 ( 45° + φ /2 )
Coulomb's theory accounts for wall friction, inclined backfills, cohesive soils
More complex equations for pressure coefficients
Considers wall-soil interface friction angle (δ)
Allows for inclined backfill surface (β)
Incorporates wall face inclination (α)
Both theories assume plane failure surfaces in soil mass
Graphical solutions (e.g., Culmann's method) available for complex geometries
Pressure Calculations and Force Distributions
Calculate vertical effective stress at any depth: σ v ′ = γ ∗ z σ'_v = γ * z σ v ′ = γ ∗ z
Determine horizontal earth pressure: σ h = K ∗ σ v ′ + u σ_h = K * σ'_v + u σ h = K ∗ σ v ′ + u
K is the appropriate earth pressure coefficient (Ka, K0, or Kp)
u is the pore water pressure
Incorporate surcharge loads in pressure calculations
Uniform surcharge: Δ σ h = K ∗ q Δσ_h = K * q Δ σ h = K ∗ q
Point loads: Use Boussinesq theory for stress distribution
Account for cohesion in cohesive soils
Reduces active pressure: σ a = K a ∗ σ v ′ − 2 c ∗ √ ( K a ) σ_a = K_a * σ'_v - 2c * √(K_a) σ a = K a ∗ σ v ′ − 2 c ∗ √ ( K a )
Increases passive pressure: σ p = K p ∗ σ v ′ + 2 c ∗ √ ( K p ) σ_p = K_p * σ'_v + 2c * √(K_p) σ p = K p ∗ σ v ′ + 2 c ∗ √ ( K p )
Calculate resultant force magnitude and point of application
Triangular distribution: F = 1 / 2 ∗ γ ∗ H 2 ∗ K F = 1/2 * γ * H^2 * K F = 1/2 ∗ γ ∗ H 2 ∗ K , acts at H/3 from base
Trapezoidal distribution: Use method of moments
Earth Pressure Impact on Retaining Structures
Stability Analysis of Retaining Walls
Evaluate sliding stability
Compare horizontal driving forces to resisting forces
Factor of safety against sliding: F S s l i d i n g = R e s i s t i n g F o r c e D r i v i n g F o r c e FS_{sliding} = \frac{Resisting Force}{Driving Force} F S s l i d in g = Dr i v in g F orce R es i s t in g F orce
Assess overturning stability
Compare overturning moments to resisting moments
Factor of safety against overturning: F S o v e r t u r n i n g = R e s i s t i n g M o m e n t O v e r t u r n i n g M o m e n t FS_{overturning} = \frac{Resisting Moment}{Overturning Moment} F S o v er t u r nin g = O v er t u r nin g M o m e n t R es i s t in g M o m e n t
Check bearing capacity
Ensure applied pressure does not exceed soil bearing capacity
Consider eccentricity of resultant force
Analyze global stability using slip circle methods (Bishop, Janbu)
Evaluate internal stability of reinforced soil structures
Tensile capacity of reinforcement layers
Pullout resistance of reinforcement
Dynamic and Long-term Considerations
Assess seismic earth pressures
Mononobe-Okabe method for pseudo-static analysis
Seed-Whitman approach for dynamic earth pressures
Consider earth pressure redistribution during and after construction
Account for soil consolidation and creep effects
Evaluate potential for progressive failure
Analyze cumulative deformations under cyclic loading
Assess long-term creep behavior of retained soil
Analyze composite retaining systems
Load transfer between soil and structural elements (anchors, tiebacks)
Distribution of earth pressures in multi-tiered walls
Consider effects of drainage systems on long-term pressure distribution
Weep holes, drainage blankets, geocomposite drains