2.4 Soil Exploration, Earth Pressure and Retaining Structures

2.4 Soil Exploration, Earth Pressure and Retaining Structures

Introduction to Geotechnical Site Characterization and Stability

  • Soil exploration is the systematic investigation of subsurface conditions to obtain critical information for safe and economical design of foundations, retaining structures, and earthworks.

  • Earth pressure theories provide the analytical framework for estimating lateral forces exerted by soil on structures like retaining walls, basement walls, and sheet piles.

  • Retaining structures are engineered systems designed to resist these lateral earth pressures and maintain the stability of soil masses at significantly different elevations.

  • This unit integrates field investigation techniques with theoretical analysis and practical design, forming a complete workflow from site understanding to structural stability assurance.


1. Soil Exploration: Methods, Planning, and Execution

1.1 Objectives and Planning of Soil Exploration

  • Primary Objectives:

    • Determine the nature and sequence of subsurface soil strata.

    • Obtain representative soil and rock samples for laboratory testing.

    • Determine the depth and location of groundwater table(s).

    • Identify problematic soils (expansive, collapsible, organic, liquefiable).

    • Assess in-situ engineering properties through field tests.

  • Planning Considerations:

    • Project Requirements: Type, magnitude, and sensitivity of the proposed structure.

    • Site Topography and Geology: Review of existing maps, aerial photos, and geological reports.

    • Exploration Program: Deciding the number, location, depth, and spacing of borings/tests.

      • Spacing: Typically 10-30 m for buildings, closer for heavy or sensitive structures.

      • Depth: Should extend to a depth where stress increase from the structure is insignificant (typically 1.5-2 times the footing width for buildings, or to competent bearing stratum).

1.2 Methods of Subsurface Exploration

  • Direct Methods (Visible Inspection):

    • Test Pits/Trenches: Provide direct visual examination of soil layers, stratification, and groundwater. Limited to shallow depths (3-5 m).

    • Open Excavations: Useful for large-scale projects like dams; allows large-scale sampling.

  • Semi-Direct Methods (Borings):

    • Auger Boring:

      • Hand Auger: Suitable for shallow depths (< 5 m) and soft soils.

      • Mechanical Auger (Hollow/Continuous Flight): Can reach greater depths; suitable for most soils except hard rock or gravel.

    • Wash Boring: Uses a chopping bit and water jetting to advance a casing. Fast but provides highly disturbed samples.

    • Rotary Drilling: Uses a rotating drill bit with circulating fluid (air, water, mud) to cut through soil and rock. Essential for rock coring and deep investigations.

    • Percussion Drilling: Uses repeated lifting and dropping of a heavy chisel bit. Effective for boulders, gravel, and hard rock.

  • Indirect Methods (Geophysical):

    • Seismic Refraction: Measures travel time of seismic waves to determine depth to bedrock and layer velocities.

    • Electrical Resistivity: Maps subsurface variations by measuring resistance to electrical current. Good for locating water tables, bedrock, and cavities.

    • Ground Penetrating Radar (GPR): Uses high-frequency radio waves to detect interfaces and objects in shallow subsurface.

1.3 Soil Sampling and Samplers

  • Objective: To obtain a representative sample with minimal disturbance for laboratory testing.

  • Types of Samples:

    • Disturbed Samples: Soil structure is destroyed. Used for index property tests (classification, water content, Atterberg limits). Obtained from split-spoon samplers or auger cuttings.

    • Undisturbed Samples: Soil structure, moisture content, and stress conditions are preserved as closely as possible. Required for strength, compressibility, and permeability tests.

Common Samplers

  • Split-Spoon Sampler (SPT Sampler):

    • A thick-walled, split cylinder driven into the soil.

    • Provides disturbed samples.

    • Used in conjunction with the Standard Penetration Test (SPT).

    • Recovery Ratio: R=Length of Sample RecoveredLength of Drive\boldsymbol{R = \frac{\text{Length of Sample Recovered}}{\text{Length of Drive}}}. Should be > 85% for good recovery.

  • Thin-Walled Tube Sampler (Shelby Tube):

    • A seamless, thin-walled steel tube (Area Ratio < 10%).

    • Gently pushed (not driven) into cohesive soil to obtain undisturbed samples.

    • Area Ratio:

      Ar=Do2Di2Di2×100%\boldsymbol{A_r = \frac{D_o^2 - D_i^2}{D_i^2} \times 100\%}

      where, Do\boldsymbol{D_o} is outer diameter and Di\boldsymbol{D_i} is inner diameter. Lower Ar\boldsymbol{A_r} means less disturbance.

  • Piston Sampler: Incorporates a stationary piston at the sampler tip to prevent soil from entering during lowering, reducing disturbance in soft clays.

1.4 Common Field Tests

  • Standard Penetration Test (SPT):

    • Procedure: Drive a standard split-spoon sampler a distance of 450 mm (18 in) using a 63.5 kg hammer falling 760 mm. Record the number of blows (N) for the last 300 mm of penetration.

    • Corrected N-value (N60\boldsymbol{N_{60}}): Corrects for field efficiency, rod length, borehole diameter, and sampling method.

    • Uses: Correlates to relative density (sands), consistency (clays), and estimates bearing capacity and settlement.

  • Cone Penetration Test (CPT):

    • Procedure: A conical tip (60°, 10 cm² area) is pushed continuously into the ground at a constant rate (2 cm/s). Measures tip resistance (qc\boldsymbol{q_c}) and sleeve friction (fs\boldsymbol{f_s}).

    • Friction Ratio: Rf=fsqc×100%\boldsymbol{R_f = \frac{f_s}{q_c} \times 100\%} (helps identify soil type).

    • Piezocone (CPTU): Also measures pore water pressure (u\boldsymbol{u}).

    • Advantages: Continuous profile, fast, repeatable, no borehole required.

  • Vane Shear Test (VST):

    • Procedure: A four-bladed vane is inserted into soft clay and rotated. The torque required to cause failure is measured.

    • Calculations: su=TK\boldsymbol{s_u = \frac{T}{K}}, where K\boldsymbol{K} is a vane constant based on its dimensions.

    • Purpose: Determines in-situ undrained shear strength (su\boldsymbol{s_u}) of soft to medium clays.

  • Plate Load Test (PLT):

    • Procedure: A rigid steel plate is placed at foundation level and loaded incrementally. Settlement is recorded for each load increment.

    • Purpose: Determines bearing capacity and settlement characteristics of the soil in-situ.

1.5 Site Investigation Report

  • A comprehensive document summarizing all findings. Key components include:

    1. Introduction: Scope and purpose of investigation.

    2. Site Description: Location, topography, access.

    3. Field Exploration Program: Methods used, boring locations, depths, dates.

    4. Subsurface Profile: Description of soil/rock strata, graphical logs for each boring.

    5. Groundwater Conditions: Observed water levels, seasonal variations.

    6. Field Test Results: SPT N-values, CPT profiles, VST results.

    7. Laboratory Test Results: Summary tables of index, strength, and compressibility properties.

    8. Analysis and Interpretation: Discussion of soil behavior, design parameters recommended.

    9. Conclusions and Recommendations: Suitability of site, recommended foundation type (shallow/deep), bearing capacity, estimated settlement, special precautions (dewatering, excavation support).


2. Earth Pressure Theories

2.1 Lateral Earth Pressure States

  • The lateral pressure (σh\boldsymbol{\sigma_h}) exerted by soil on a retaining structure depends on the wall movement relative to the backfill.

  • Three Fundamental States:

    1. At-Rest Earth Pressure (K0\boldsymbol{K_0}):

      • Occurs when the wall is rigid and does not move (e.g., basement wall, bridge abutment).

      • Coefficient of Earth Pressure at Rest: K0=σhσv\boldsymbol{K_0 = \frac{\sigma_h'}{\sigma_v'}}

      • For normally consolidated soils: K01sinϕ\boldsymbol{K_0 \approx 1 - \sin \phi'} (Jaky's formula).

      • For overconsolidated soils: K0(OC)K0(NC)(OCR)sinϕ\boldsymbol{K_0(OC) \approx K_0(NC) \cdot (OCR)^{\sin \phi'}}.

    2. Active Earth Pressure (Ka\boldsymbol{K_a}):

      • Occurs when the wall moves away from the soil mass sufficiently.

      • Soil reaches a state of plastic equilibrium, mobilizing its shear strength.

      • This is the minimum possible lateral pressure.

    3. Passive Earth Pressure (Kp\boldsymbol{K_p}):

      • Occurs when the wall moves into the soil mass sufficiently.

      • Soil is compressed and sheared, offering maximum resistance.

      • This is the maximum possible lateral pressure.

2.2 Rankine's Earth Pressure Theory (1857)

  • Assumptions: Soil is homogeneous, isotropic, cohesionless, the wall is frictionless (smooth) and vertical, and the ground surface is horizontal.

  • Active Earth Pressure Coefficient:

    Ka=1sinϕ1+sinϕ=tan2(45ϕ2)\boldsymbol{K_a = \frac{1 - \sin \phi}{1 + \sin \phi} = \tan^2 \left(45^\circ - \frac{\phi}{2}\right)}

    Pressure Distribution (for a cohesionless soil): σa=Kaσv=Kaγz\boldsymbol{\sigma_a = K_a \sigma_v = K_a \gamma z}

  • Passive Earth Pressure Coefficient:

    Kp=1+sinϕ1sinϕ=tan2(45+ϕ2)\boldsymbol{K_p = \frac{1 + \sin \phi}{1 - \sin \phi} = \tan^2 \left(45^\circ + \frac{\phi}{2}\right)}

    Pressure Distribution: σp=Kpσv=Kpγz\boldsymbol{\sigma_p = K_p \sigma_v = K_p \gamma z}

  • For Cohesive Soils (c-ϕ\boldsymbol{\phi} soil):

    • Active Pressure: σa=Kaγz2cKa\boldsymbol{\sigma_a = K_a \gamma z - 2c \sqrt{K_a}}

    • Passive Pressure: σp=Kpγz+2cKp\boldsymbol{\sigma_p = K_p \gamma z + 2c \sqrt{K_p}}

    • Tension Crack Depth (zc\boldsymbol{z_c}): zc=2cγKa\boldsymbol{z_c = \frac{2c}{\gamma \sqrt{K_a}}}. In design, tension is usually ignored, and pressure is taken as zero from surface to zc\boldsymbol{z_c}.

2.3 Coulomb's Earth Pressure Theory (1776)

  • Advantage over Rankine: Considers wall friction (δ\boldsymbol{\delta}) and sloping backfill (β\boldsymbol{\beta}).

  • Based on force equilibrium of a failing soil wedge.

  • Active Earth Pressure Coefficient:

    Ka=cos2(ϕθ)cos2θcos(δ+θ)[1+sin(δ+ϕ)sin(ϕβ)cos(δ+θ)cos(θβ)]2\boldsymbol{K_a = \frac{\cos^2 (\phi - \theta)}{\cos^2 \theta \cdot \cos(\delta + \theta) \left[ 1 + \sqrt{\frac{\sin(\delta+\phi)\sin(\phi-\beta)}{\cos(\delta+\theta)\cos(\theta-\beta)}} \right]^2}}

    where, θ\boldsymbol{\theta} is the wall inclination from vertical.

  • Passive Earth Pressure Coefficient (Similar form, different sign conventions).

  • Total Active Force per unit length:

    Pa=12KaγH2\boldsymbol{P_a = \frac{1}{2} K_a \gamma H^2}

    Acts at H/3\boldsymbol{H/3} from the base for triangular pressure distribution.

  • Direction of Force: Inclined at an angle δ\boldsymbol{\delta} to the normal of the wall.


3. Stability Analysis of Retaining Walls

3.1 Types of Retaining Walls

  • Gravity Walls: Rely on their own mass for stability (stone masonry, plain concrete). Usually massive.

  • Cantilever Walls: Reinforced concrete walls consisting of a vertical stem and a base slab (heel and toe). Most common for heights up to 6-8 m.

  • Counterfort/Buttress Walls: Similar to cantilever but have thin vertical ribs (counterforts behind the wall or buttresses in front) to reduce bending moments. Used for greater heights (>8 m).

  • Sheet Pile Walls: Thin, interlocking sections driven into the ground. Used for waterfront structures and temporary excavations.

  • Anchored/Braced Walls: Walls supported by anchors (ties) or braces to increase stability against high pressures.

3.2 Failure Modes and Stability Checks

A retaining wall must be checked against the following potential failure modes:

1. Overturning Failure

  • Mechanism: Wall rotates about its toe due to lateral earth pressure.

  • Factor of Safety (FOS):

    FOSoverturning=Resisting Moments about ToeOverturning Moments about Toe1.52.0\boldsymbol{FOS_{overturning} = \frac{\sum \text{Resisting Moments about Toe}}{\sum \text{Overturning Moments about Toe}} \geq 1.5 - 2.0}

2. Sliding Failure

  • Mechanism: Wall translates horizontally due to lateral force.

  • Resistance: Provided by base friction and/or passive resistance at the toe (shear key).

  • Factor of Safety (FOS):

    FOSsliding=Resisting Horizontal ForcesDriving Horizontal Forces1.5\boldsymbol{FOS_{sliding} = \frac{\sum \text{Resisting Horizontal Forces}}{\sum \text{Driving Horizontal Forces}} \geq 1.5}

    Resisting Forces=(V)tanδb+cbB+Pp\boldsymbol{\sum \text{Resisting Forces} = (\sum V) \cdot \tan \delta_b + c_b \cdot B + P_p} where, V\boldsymbol{\sum V} is total vertical force, δb\boldsymbol{\delta_b} is wall-soil base friction angle, cb\boldsymbol{c_b} is soil-wall base adhesion, B\boldsymbol{B} is base width, Pp\boldsymbol{P_p} is passive force at toe.

3. Bearing Capacity Failure

  • Mechanism: Soil beneath the toe fails in shear due to excessive vertical pressure.

  • Procedure: Calculate the maximum and minimum pressure (qmax,qmin\boldsymbol{q_{max}, q_{min}}) at the base using eccentricity formulas.

    • Eccentricity (e\boldsymbol{e}):

      e=B2MRMOV\boldsymbol{e = \frac{B}{2} - \frac{\sum M_R - \sum M_O}{\sum V}}

    • Must have eB/6\boldsymbol{e \leq B/6} to avoid tension under the base.

    • Soil Pressure (for eB/6\boldsymbol{e \leq B/6}):

      qmax,min=VB(1±6eB)\boldsymbol{q_{max, min} = \frac{\sum V}{B} \left(1 \pm \frac{6e}{B}\right)}

  • Factor of Safety (FOS):

    FOSbearing=qultqmax3.0\boldsymbol{FOS_{bearing} = \frac{q_{ult}}{q_{max}} \geq 3.0}

    where, qult\boldsymbol{q_{ult}} is the ultimate bearing capacity of the foundation soil.

4. Deep-Seated Shear (Overall Stability) Failure

  • Mechanism: A slip surface passes beneath the wall and behind it, involving a large soil mass. Common in weak soils.

  • Analysis Method: Slope stability analysis (e.g., Method of Slices, Bishop's method, using software). Check for circular or non-circular failure surfaces.

5. Internal Failure (Structural Checks)

  • Mechanism: Failure of the wall material itself (concrete crushing, steel yielding).

  • Analysis: Structural design of stem, heel, and toe slabs for bending moment and shear force, following reinforced concrete design codes.


4. Techniques to Increase Stability of Retaining Walls

4.1 Geometric Modifications

  • Increase Base Width (B\boldsymbol{B}): Directly increases resisting moments and reduces base pressure.

  • Use a Sloping Backfill: Reduces the active earth pressure coefficient (Ka\boldsymbol{K_a}) according to Coulomb's theory. A surcharge slope (β\boldsymbol{\beta}) is beneficial.

  • Provide a Toe Projection: Extends the lever arm for resisting moments against overturning.

  • Batter the Wall Face: Inclining the wall face into the backfill (negative batter) engages more wall friction and can reduce pressure.

4.2 Soil Improvement and Reinforcement

  • Use of Cohesionless Backfill: Draining, free-draining materials (sand, gravel) have higher ϕ\boldsymbol{\phi} and lower lateral pressure. They also prevent buildup of pore water pressure.

  • Provision of Drainage: This is the single most effective measure.

    • Weep Holes: Perforated pipes through the wall stem near its base.

    • Drainage Blanket: A layer of granular material behind the wall with a perforated collector pipe at the base.

    • Prevents hydrostatic pressure, which can double the lateral force.

  • Shear Key: A projection from the base slab into the underlying soil, engaging passive resistance to increase sliding resistance.

4.3 External Support Systems

  • Counterforts/Buttresses: Connect the stem to the base slab, reducing the unsupported span of the stem and base, allowing for a thinner, more efficient section.

  • Tiebacks/Ground Anchors: High-strength tendons drilled and grouted into the soil/rock behind the wall, then tensioned and connected to the wall. They provide an external resisting force.

  • Struts/Braces: Horizontal members placed between opposing walls in excavations. Common in temporary works like braced sheet pile walls.

4.4 Specialized Wall Systems

  • Reinforced Soil Walls (Mechanically Stabilized Earth - MSE): Uses horizontal layers of tensile reinforcement (geogrids, strips) within the soil mass to create a coherent, stable gravity structure.

  • Gabion Walls: Wire mesh boxes filled with rock. Flexible, permeable, and good for erosion control.

  • Crib Walls: Interlocking structural frames (timber, concrete) filled with granular material. Permeable and can tolerate some settlement.

4.5 Construction and Maintenance Considerations

  • Proper Compaction: Backfill should be compacted in thin lifts to desired density. Over-compaction near the wall can induce excessive lateral pressures.

  • Staged Construction: For high walls or weak foundations, construct and backfill in stages to allow for consolidation and strength gain.

  • Joints and Waterproofing: Provide construction joints and proper drainage to prevent water ingress and frost damage.

  • Monitoring: Install instrumentation (inclinometers, settlement markers) for critical walls to monitor performance during and after construction.


Summary and Design Synthesis

  • Soil exploration provides the essential data (stratigraphy, parameters, groundwater) that feeds into earth pressure calculations.

  • Earth pressure theory (Rankine/Coulomb) translates soil properties into design loads on the retaining structure.

  • Stability analysis ensures the proposed wall geometry is safe against overturning, sliding, bearing, and overall failure.

  • Stability enhancement techniques are integral to efficient design, often making an otherwise unstable section viable.

  • The final design is an iterative process balancing geotechnical safety, structural efficiency, constructability, and cost.

  • A well-investigated site and a rigorously analyzed design are the cornerstones of a safe and durable retaining structure.


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