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CE-802 (B) · Foundation Engineering/Quick Revision Short Notes

Foundation Engineering (CE-802 (B)) - Unit 1 Short Notes

UNIT 1: SUBSURFACE INVESTIGATION & SOIL SAMPLING

I. Planning & Execution of Site Exploration

Objectives: To determine soil profile, groundwater, and engineering properties for safe, economical foundation design.

IS 1892 (Part 1) Criteria for Borehole Depth & Spacing:

  • Depth: Should penetrate to a significant depth where stress increase from foundation ≤ 10-20% of effective overburden. For preliminary studies, depth ≈ width of largest planned foundation.

  • Spacing: Governed by soil variability.

    • Homogeneous soils: 30-50 m.

    • Variable soils: 15-30 m.

    • Critical sites/structures: Closer spacing (5-15 m).

Boring Methods:

Method Principle Advantages Limitations
Auger Boring (Manual/Mechanical) Helical auger cuts & brings soil to surface. Fast in cohesionless soils, cheap. Disturbs soft clays, cannot handle boulders/water.
Rotary Drilling Rotating bit with circulating fluid (mud/water) brings cuttings. Fastest, handles all soils & rock, good for deep holes, maintains hole stability with mud. Expensive, requires water/mud management.
Percussion (Shell & Auger) Dropping chisel/bit to crush rock, bailer removes cuttings. Good for hard strata/rock. Slow, severe sample disturbance.
Wash Boring Water jet loosens soil, bailer removes slurry. Simple, cheap. High disturbance, not for sampling.

Geophysical Methods (Indirect Exploration):

  • Seismic Refraction: Measures wave velocity to infer soil/rock layers & depth to bedrock.

  • Electrical Resistivity: Measures soil resistivity to map stratigraphy & groundwater.

  • Ground Penetrating Radar (GPR): High-resolution imaging of shallow layers (limited by conductivity).

[!TIP] Exam Focus: Rotary drilling is frequently asked for its advantages (speed, depth, stability). Remember IS 1892 criteria link depth to stress distribution (Boussinesq) and spacing to soil variability.

II. In-Situ Testing

Standard Penetration Test (SPT):

  • Procedure: Drive a split spoon sampler (50 mm ID) 450 mm into soil at borehole bottom using a 63.5 kg hammer falling 760 mm. Count blows for each 150 mm penetration. Last 300 mm blows = N-value.

  • Significance of N-value: Empirical index for:

    • Relative density of sands.

    • Consistency of clays.

    • Bearing capacity & settlement estimation.

    • Liquefaction potential assessment.

Corrections to Field N-value (N_field):

  1. Overburden Pressure Correction (N₁): For cohesionless soils.

$$N_1 = N_{field} \times \left( \frac{\bar{\sigma}_v'}{100 \text{ kPa}} \right)^{0.5} \quad \text{(for } \bar{\sigma}_v' \text{ in kPa)}$$

  1. Dilatancy Correction (N₂): For dense, saturated fine sands/silts (N₁ > 15). Corrects for negative pore pressure.

$$N_2 = 15 + 0.5(N_1 - 15) \quad \text{(if } N_1 > 15\text{)}$$

  1. Energy Correction (N₆₀): Corrects to 60% standard energy (E_B = 2.68 N-m). Most crucial for design.

$$N_{60} = N_{field} \times \frac{E_m}{E_B}$$

where $$\displaystyle E_m $$ = actual hammer energy ratio (often 50-90%).

Final Corrected N-value (N₆₀,corr): Apply corrections sequentially: N_field → N₁ → N₂ → N₆₀. Use N₆₀,corr for design correlations.

Cone Penetration Test (CPT/CPTu):

  • Procedure: Push a cone (10 cm² area) into soil at 20 mm/s, measuring cone resistance (q_c) and sleeve friction (f_s) continuously.

  • Output: Continuous soil profile, identifies layers, estimates strength/compressibility.

  • CPTu: Adds pore pressure (u) measurement for better soil typing and consolidation parameters.

  • SPT vs. SCPT:

    | Feature | SPT | SCPT | | :--- | :--- | :--- | | Sample | Disturbed (split spoon) | No sample (continuous profiling) | | Disruption | High (dynamic) | Low (static) | | Data | Discrete (every 1.5 m) | Continuous | | Cost | Low | High |

Vane Shear Test: For soft clays (< 25 kPa). Inserts a four-blade vane, measures peak & residual torque to calculate undrained shear strength ($$\displaystyle c_u $$).

Pressuremeter Test (PMT): Inflates a membrane in a borehole, measures pressure-deformation to derive in-situ modulus (E_M) and limit pressure (p_L) for bearing capacity.

III. Soil Sampling

Disturbed vs. Undisturbed Samples:

Feature Disturbed Undisturbed
Structure Altered/ destroyed Preserved
Strength Lost Retained
Use Classification, water content, compaction tests Strength (triaxial, oedometer), consolidation tests
Identification Hand sample, chunks Shelby tube (intact core), piston sampler

Sampling Tools & Quality Parameters:

  • Open Drive Sampler (Shelby Tube): Thin-walled, pushed/driven. Inside Clearance (C_i) & Outside Clearance (C_o) critical.

$$C_i = \frac{D_i - D_c}{D_c} \times 100\% \quad ; \quad C_o = \frac{D_c - D_o}{D_o} \times 100\%$$

*   **C_i (1-3%):** Reduces friction, aids sample entry.

*   **C_o (0-2%):** Reduces soil compression on sample.
  • Area Ratio (A_r): Ratio of cutting edge area to tube area.

$$A_r = \frac{(D_o^2 - D_i^2)}{D_i^2} \times 100\%$$

*   **A_r < 10%** for undisturbed clays. Lower = less disturbance.
  • Length-Diameter Ratio (L/D): Should be > 2 for good quality.

CNS Layer (Cavity, No Strain): The idealized sampling disturbance zone. A thin layer around the sample where soil is strained but not sheared. Minimizing CNS layer is key for undisturbed sampling.

Bore-log Report Components:

  1. Project details, borehole location & elevation.

  2. Soil description (color, consistency, stratification).

  3. Depth of water table & strata changes.

  4. SPT N-values (with corrections noted).

  5. Sample type & recovery.

  6. Laboratory test results (if any).

  7. Graphical log (soil symbols, N-value plot).

[!TIP] Common Pitfall: Confusing Area Ratio (A_r) formula. Remember it's based on annular area of cutting edge vs. inner area of tube. For Shelby tube, $$\displaystyle D_i $$ is inner diameter.


UNIT 1: SHALLOW FOUNDATIONS - BEARING CAPACITY & SETTLEMENT

I. Types & Selection

Types: Isolated, Combined, Strip, Raft/Mat, Floating. Selection Factors:

  • Soil: Strength, compressibility, depth to bedrock.

  • Load: Magnitude, type (axial, moment), distribution.

  • Structure: Sensitivity to settlement, rigidity.

  • Cost: Excavation vs. material.

  • Basic Criteria: Adequate bearing capacity & acceptable total & differential settlement.

II. Bearing Capacity

Key Definitions:

  • Gross Pressure (q): Total load / area.

  • Net Pressure (q_net): $$\displaystyle q_{net} = q - \gamma D_f $$ (D_f = depth).

  • Ultimate Bearing Capacity (q_u): Max gross pressure before shear failure.

  • Net Ultimate (q_nu): $$\displaystyle q_{nu} = q_u - \gamma D_f $$.

  • Net Safe (q_ns): $$\displaystyle q_{ns} = \frac{q_{nu}}{FOS} $$.

  • Allowable Bearing Pressure (q_all): Usually = q_ns or settlement-controlled value.

Modes of Shear Failure (Sketch Essential):

  1. General Shear: Deep foundations, dense soils. Continuous failure surface to surface, large settlements, distinct peak.

  2. Local Shear: Medium dense/medium stiff soils. Failure surfaces limited, moderate settlements.

  3. Punching Shear: Very loose soils/very deep foundations. Soil punches under footing, minimal surface heave, large settlements.

Terzaghi's Bearing Capacity Theory (1943):

  • Assumptions: Strip footing, rough base, soil above base ignored (γD_f term added later), Rankine's active earth pressure at sides, Mohr-Coulomb failure.

  • Equation (for strip footing):

$$q_u = c N_c + \gamma D_f N_q + 0.5 \gamma B N_\gamma$$

*   $$\displaystyle N_c, N_q, N_\gamma $$: Bearing capacity factors (function of φ).

*   For **square footing:** $$\displaystyle q_u = 1.3c N_c + \gamma D_f N_q + 0.4 \gamma B N_\gamma $$.

*   For **circular footing:** $$\displaystyle q_u = 1.3c N_c + \gamma D_f N_q + 0.3 \gamma B N_\gamma $$.

*   For **rectangular footing:** Use shape factors (s_c, s_q, s_γ).

IS Code Method (BIS: IS 6403):

  • Generalized Equation:

$$\boxed{q_{nu} = c N_c s_c d_c i_c + \gamma D_f N_q s_q d_q i_q + 0.5 \gamma B N_\gamma s_\gamma d_\gamma i_\gamma}$$

*   **Shape Factors (s):** Account for footing shape (e.g., $$\displaystyle s_c = 1 + 0.2 \frac{B}{L} $$ for rectangular).

*   **Depth Factors (d):** For deep foundations ($$\displaystyle D_f/B > 1 $$).

*   **Inclination Factors (i):** For inclined loads.

*   **Note:** For most shallow foundations, $$\displaystyle d_c = d_q = d_\gamma = 1 $$, $$\displaystyle i_c = i_q = i_\gamma = 1 $$ if load vertical.

Water Table Correction:

  • If water table at/above foundation base, use submerged unit weight (γ') for the γB N_γ term.

  • For water table within depth D_f, use effective overburden at base for γD_f N_q term.

  • General Rule: Use effective stresses in the bearing capacity equation.

Numerical Approach:

  1. Determine soil parameters (c, φ, γ).

  2. Find N_c, N_q, N_γ from tables (Terzaghi or IS).

  3. Apply shape, depth, load inclination factors.

  4. Apply water table correction (use γ' where appropriate).

  5. Compute q_nu, then q_ns with FOS (typically 2.5-3.0).

III. Settlement of Foundations

Components:

  1. Immediate (Elastic) Settlement (S_i): Occurs during/just after construction in cohesive soils (undrained) & cohesionless soils (due to shear distortion).

  2. Primary Consolidation Settlement (S_c): Due to expulsion of pore water from cohesive soils under sustained load. Time-dependent.

  3. Secondary Compression (S_s): Post-primary consolidation due to soil structure rearrangement.

Immediate Settlement (S_i) for Cohesive Soils (Elastic Half-Space):

$$\boxed{S_i = \frac{q B (1 - \mu^2)}{E_s} I_f}$$

  • q = net pressure.

  • B = footing width.

  • μ = Poisson's ratio.

  • E_s = Secant modulus from undrained triaxial test (E_s ≈ 2-3 E_u for normally consolidated clays).

  • I_f = Influence factor (from charts like 2:1 distribution or 3D elastic charts). For flexible square footing on clay, I_f ≈ 1.0 - 1.2.

Consolidation Settlement (S_c) - One Dimensional:

$$S_c = \frac{C_c}{1 + e_0} H \log_{10} \left( \frac{\bar{\sigma}_0' + \Delta \bar{\sigma}'}{\bar{\sigma}_0'} \right)$$

  • C_c = compression index.

  • e_0 = initial void ratio.

  • H = thickness of compressible layer.

  • $$\displaystyle \bar{\sigma}_0' $$ = initial effective stress.

  • $\Delta \bar{\sigma}'$ = increase in effective stress (from 2:1 or other distribution).

Plate Load Test:

  • Procedure: Load a rigid plate (usually 0.3 m sq.) at ground level, measure settlement.

  • Load-Settlement Curve: Ultimate load (q_u,plate) from curve (usually at settlement = 20% plate width).

  • Extrapolation to Field Footing:

    • For Clay: Settlement is proportional to width (B).

$$S_{field} = S_{plate} \times \frac{B_{field}}{B_{plate}}$$

*   **For Sand:** Bearing capacity is proportional to width.

$$q_{u,field} = q_{u,plate} \times \frac{B_{field}}{B_{plate}}$$

*   **Note:** Assumes similar stress distribution & soil homogeneity.

[!TIP] Critical Distinction: In clay, settlement ∝ B (same pressure). In sand, bearing capacity ∝ B (same settlement). This is a classic exam question.


UNIT 1: DEEP FOUNDATIONS - PILES

I. Introduction & Classification

Necessity: When shallow foundations inadequate (low bearing capacity, large settlement, scour, etc.). Classification:

  • By Material: Timber, Concrete (precast/cast-in-situ), Steel, Composite.

  • By Function/Action:

    • End-bearing: Transfers load to hard stratum.

    • Friction: Load by skin friction along shaft.

    • Combined: Both end-bearing & friction.

    • Tension/Anchor: Resists uplift.

    • Sheet: Retains soil (cofferdams, bulkheads).

  • By Construction:

    • Driven: Precast, displacement (crowding soil).

    • Bored: Cast-in-situ, non-displacement (less disturbance).

    • Screwed/Under-reamed: Special types.

II. Pile Load Capacity

Static Load Carrying Capacity (Q_u):

$$Q_u = Q_b + Q_s$$

  • End Bearing (Q_b): $$\displaystyle Q_b = q_b \times A_p $$

    • Clay: $$\displaystyle q_b = N_c c $$ (N_c ≈ 9 for deep piles).

    • Sand: $$\displaystyle q_b = \gamma D_p N_q $$ (N_q from bearing capacity factors).

  • Shaft Friction (Q_s): $$\displaystyle Q_s = f_s \times A_s $$

    • α-method (Clays): $$\displaystyle f_s = \alpha \cdot c_u $$ (α = adhesion factor, 0.4-1.0, decreases with depth/softness).

    • β-method (Sands): $$\displaystyle f_s = \beta \cdot \bar{\sigma}_v' $$ (β = friction factor, ≈ K tanδ, K ≈ 1-2, δ ≈ 0.75φ).

Dynamic Formulae (Impact Driving):

  • Engineering News Formula (ENF):

$$Q_{safe} = \frac{W h}{S + C} \times \frac{W + n W'}{W + W'}$$

*   W = hammer weight, h = fall, S = set (penetration/blow), C = constant (2.5 cm), n = efficiency (0.6-0.8), W' = pile weight.

*   **Limitations:** Ignores elastic compression, restitution.
  • Hiley's Formula (Improved ENF):

$$\boxed{Q_{safe} = \frac{\eta W h}{S + \frac{C}{2}} \times \frac{W + n W'}{W + W'}}$$

*   η = **coefficient of restitution** (0.25-0.5 for concrete-steel).

*   **Includes** average elastic compression (C/2).

*   **Most commonly used** in practice.

Pile Capacity from SPT/CPT:

  • SPT: $$\displaystyle Q_b = N \cdot A_p \cdot q_b $$ (q_b from correlations), $$\displaystyle Q_s = \sum (f_s \cdot \Delta A_s) $$ where $$\displaystyle f_s $$ from N-value correlations.

  • CPT: Directly uses $$\displaystyle q_c $$ and $$\displaystyle f_s $$ with empirical correlations (e.g., $$\displaystyle f_s = \alpha \cdot q_c $$ for clays).

III. Pile Groups & Negative Skin Friction

Pile Group Efficiency (η_g):

$$\eta_g = \frac{Q_{ug}}{n \cdot Q_{up}}$$

  • η_g < 1 for most groups due to group effect (overlap of stress bulbs).

  • Block Failure: Occurs in soft clays at close spacing (< 3D). Entire soil block fails.

$$Q_{ug(block)} = c \cdot (B_g \cdot L_g) \cdot N_c + \gamma D_f (B_g L_g) N_q$$

*   B_g, L_g = group dimensions.
  • Individual Failure: Piles fail individually, group capacity < nQ_up.

Geometric Properties for Spacing:

  • Center-to-center spacing (s): Minimum 2-3 times pile diameter (D) for clays, 3-4D for sands to minimize group effect.

  • Group Shape: Square, rectangular, triangular. Efficiency depends on arrangement.

Negative Skin Friction (NSF):

  • Cause: Downward movement of soil relative to pile (e.g., soft clay consolidation, fill placement, water table drop).

  • Effect: Increases load on pile (reduces capacity), causes additional settlement.

  • Calculation for Single Pile in Cohesive Soil:

$$\boxed{Q_{nsf} = \bar{f}_{nsf} \times A_s = \left( \gamma \cdot \Delta z \cdot K \cdot \tan \delta \right) \times (\pi D L_{nsf})}$$

*   $$\displaystyle \bar{f}_{nsf} $$ = average NSF stress.

*   Δz = thickness of compressible layer.

*   K = lateral earth pressure coefficient (≈ 1.0 for NC clays).

*   δ = interface friction angle (≈ φ for rough concrete).

*   L_nsf = length through compressible layer.
  • Design: Net allowable load = Q_u - Q_nsf.

IV. Special Pile Types

Under-reamed Piles:

  • Concept: Single/multiple bulbs (under-reams) on shaft in expansive soils.

  • Suitability: Expansive soils (high shrink-swell), loess, collapsible soils. Bulbs provide tension anchorage to resist uplift.

  • Ultimate Tensile Capacity:

$$Q_{tu} = Q_{s(adhesion)} + Q_{b(under-ream)}$$

*   $$\displaystyle Q_{s(adhesion)} = \alpha \cdot c_u \cdot A_s $$ (up to bulbs).

*   $$\displaystyle Q_{b(under-ream)} = A_b \cdot q_b $$ (q_b = 9c_u for clay, bearing on bulb base).

*   **Neglect suction** (as per problem statement).

Well Foundations (Caissons):

  • Components (Neat Sketch Required):

    1. Well curb: Bottom cutting edge (steel/iron).

    2. Well steining: Masonry/concrete above curb (provides weight for sinking).

    3. Cutting edge: Beveled edge for penetration.

    4. Lining/Wall: Brick/stone/concrete rings.

    5. Bottom plug: Concrete plug at bottom (after sinking).

    6. Top plug: Concrete plug at top (after dewatering).

    7. Well cap: RCC beam to distribute load from pier.

  • Types: Open (dry), Pneumatic (compressed air), Box (prefabricated).

  • Sinking Methods: By gravity, with kentledge, with water jetting (in sand), with pneumatic pressure.

V. Numerical Problems (Comprehensive)

  • Single Pile Capacity: Always check Q_b and Q_s separately. For clay, $$\displaystyle Q_b = 9c_u A_p $$ (deep pile). For sand, $$\displaystyle Q_b = \gamma D_p N_q A_p $$.

  • Pile Group Capacity (Neglecting End Bearing):

$$Q_{ug} = \alpha \cdot c_u \cdot (A_s)_{group}$$

where $$\displaystyle (A_s)_{group} $$ = total surface area of all piles in group. Apply group efficiency if spacing < 3D.
  • Layered Soils: Calculate Q_b from bearing stratum. Calculate Q_s by summing contributions from each layer: $$\displaystyle Q_s = \sum (\alpha_i c_{ui} \cdot \Delta A_s) $$.

  • Dynamic Formula (Hiley's): Must compute elastic compression (C) of pile + cap:

$$C = \frac{Q_u L}{A E} \quad \text{(in cm)}$$

where Q_u = ultimate load, L = length, A = area, E = modulus.

[!TIP] Exam Trap: In pile group problems, if spacing is given as 90 cm for 300 mm dia piles, s/D = 3.0. For soft clay, this is critical spacing—may need to consider block failure or reduced efficiency. Always check: if s < 3D, group efficiency < 1.


UNIT 1: EARTH PRESSURE & RETAINING STRUCTURES

I. Types of Lateral Earth Pressure

  • At-rest (K₀): Wall does not move (e.g., basement walls before backfill). $$\displaystyle K₀ = 1 - \sin \phi' $$ (for NC soils).

  • Active (Kₐ): Wall moves away from soil (unloading). Minimum pressure.

  • Passive (Kₚ): Wall moves into soil (loading). Maximum pressure.

  • Relationship: $$\displaystyle K_a K_p = 1 $$ (for $$\displaystyle \phi' > 0 $$).

II. Classical Theories

Rankine's Theory (1875):

  • Assumptions: Wall smooth (δ=0), horizontal backfill, no wall friction, infinite wall.

  • For Cohesionless Soil (φ'):

$$K_a = \tan^2 \left(45^\circ - \frac{\phi'}{2}\right) \quad ; \quad K_p = \tan^2 \left(45^\circ + \frac{\phi'}{2}\right)$$

  • For Cohesive Soil (c', φ'):

    • Active: $$\displaystyle \sigma_h = K_a \gamma z - 2c \sqrt{K_a} $$ (tension crack if $$\displaystyle \sigma_h < 0 $$).

    • Passive: $$\displaystyle \sigma_h = K_p \gamma z + 2c \sqrt{K_p} $$.

  • Pressure Diagram: Triangular for c-φ soil with c'=0. For c'>0, active diagram has negative zone near top.

Coulomb's Theory (1776):

  • Assumptions: Inclined failure plane, wall friction (δ) considered, inclined backfill (β) possible.

  • Derivation: Wedge analysis, minimize active thrust by varying failure plane angle.

  • Active Earth Pressure Coefficient:

$$K_a = \frac{\cos^2(\phi' - \delta)}{\cos^2 \delta \cos(\delta + \beta) \left[1 + \sqrt{\frac{\sin(\phi' + \delta) \sin(\phi' - \beta)}{\cos(\delta + \beta)}} \right]^2}$$

*   For δ=0, β=0 → reduces to Rankine's K_a.
  • Merits over Rankine:

    1. Considers wall friction (δ) → more realistic.

    2. Allows inclined backfill (β).

    3. Applicable for both cohesionless & cohesive soils.

    4. Passive pressure from Coulomb is more reliable (Rankine overestimates).

Comparison:

Feature Rankine Coulomb
Wall Friction Neglected (δ=0) Considered (δ>0)
Backfill Horizontal only Inclined allowed
Failure Plane Vertical wall → 45+φ/2 Inclined, variable
K_a Value Higher (for δ>0) Lower, more realistic
K_p Value Lower (overly conservative) Higher, more realistic

III. Graphical Methods

  • Culmann's Graphical Method: For active pressure with irregular, inclined backfill and surcharge. Construct failure wedges from wall, draw pressure lines.

  • Rebhann's Graphical Method: For passive pressure.

IV. Earth Pressure on Retaining Walls

Numerical Calculation Steps:

  1. Draw pressure diagram for each layer (consider water table, surcharge).

  2. For cohesionless soil: $$\displaystyle \sigma_h = K \gamma z $$ (above WT: γ_dry; below: γ_sat).

  3. For cohesive soil (active): $$\displaystyle \sigma_h = K \gamma z - 2c \sqrt{K} $$. Check for tension crack depth $$\displaystyle z_c = \frac{2c}{\gamma \sqrt{K}} $$.

  4. With water table/seepage: Use submerged unit weight (γ') below WT. Add hydrostatic pressure (u = γ_w z) on total stress diagram.

  5. Resultant Thrust (P): Area of pressure diagram. Point of application = centroid.

    • Triangular: at h/3 from base.

    • Trapezoidal: divide into triangle+rectangle.

Example (Stratified Backfill): Calculate K for each layer (use φ of that layer). Sum pressures at interfaces. Plot diagram, find total P and its point of action.

V. Retaining Wall Design & Stability

Modes of Failure:

  1. Overturning: Wall rotates about toe. Check FOS = Resisting Moment / Overturning Moment ≥ 1.5.

  2. Sliding: Wall slides along base. Check FOS = (μ W + P_p) / P_a ≥ 1.5 (μ = friction coeff., P_p = passive force at toe).

  3. Bearing Capacity Failure: Excessive pressure on soil. Check $$\displaystyle q_{max} \leq q_{all} $$.

  4. Excessive Settlement/Differential Settlement.

Sheet Piles vs. Retaining Walls:

Feature Sheet Piles Retaining Walls
Function Retention (cofferdams, bulkheads) Support (free-standing)
Design Flexible (bending, deflection) Rigid (gravity/cantilever)
Material Steel, timber, vinyl Masonry, concrete, RCC
Depth Can be very deep Usually shallow to moderate
Uses Temporary/permanent walls, excavation support Bridge abutments, garden walls, basement

Uses of Sheet Piles:

  1. Cofferdams for foundations in water.

  2. Retaining walls for excavations.

  3. Bulkheads for waterfronts.

  4. Slope stabilization.

  5. Noise barriers.

[!TIP] Earth Pressure Calculation: Always draw the pressure diagram. For cohesive soil with water table, remember: active pressure = (K γ' z) - 2c√K + (γ_w z) (hydrostatic on top of effective stress diagram). Tension crack depth is critical for cohesive backfills.


UNIT 1: SPECIAL TOPICS & SOIL IMPROVEMENT

I. Problematic Soils

Expansive Soils (Black Cotton Soils):

  • Characteristics:

    • High montmorillonite clay content.

    • High shrinkage/swelling potential (low liquid limit? No, high LL > 50%).

    • Low strength when wet, hard when dry.

    • High compressibility, low permeability.

    • Cracks on drying.

  • Problems:

    • Heave (swelling) → lifts foundation.

    • Shrinkage → settlement & cracks in structure.

    • Volume change → differential movement.

  • Preventive Measures:

    1. Moisture Control: Maintain constant water content (impermeable blanket, landscaping).

    2. Replacement: Remove & replace with non-expansive fill.

    3. Stabilization: Lime/cement treatment.

    4. Under-reamed Piles: Best solution for heavy structures. Bulbs anchor in non-swelling zone.

    5. Raft Foundations: Spread load, reduce pressure.

Collapsible Soils:

  • Characteristics:

    • Loose, porous, cemented (e.g., loess, wind-blown silt).

    • Dry has moderate strength.

    • Sudden collapse upon wetting (loss of cementation).

    • Low density, high void ratio.

  • Problems: Sudden, large settlement upon wetting (rainfall, leakage).

  • Preventive Measures:

    1. Pre-wetting: Saturate soil before construction to induce collapse.

    2. Compaction: Dynamic compaction, heavy tamping.

    3. Piles: Transfer load through collapsible zone.

    4. Chemical Stabilization: Lime/cement to break cementation bonds before wetting.

II. Soil Stabilization & Improvement

Need: To improve strength, reduce compressibility/permeability, control swell. Situations: Weak subgrade, expansive soils, fills, slope stabilization.

Methods:

  1. Mechanical: Compaction (increases density, strength).

  2. Chemical: Lime (for clay, reduces plasticity, pozzolanic), Cement (for sand/clay, binds particles), Bitumen (for waterproofing, base course).

  3. Electrical: Electro-osmosis.

    • Mechanism: Apply DC electric field → water migrates from anode to cathode in clay (electro-osmotic flow).

    • Application: Consolidate very soft, saturated clays (e.g., for slope stabilization, preloading). Often combined with chemical injection (electro-chemical).

III. Geosynthetics

Types & Functions:

Type Material Primary Functions
Geotextiles Woven/Non-woven fabrics Separation, Filtration, Reinforcement, Drainage
Geogrids Polymer grids (uniaxial/biaxial) Reinforcement (high tensile strength)
Geomembranes HDPE, LDPE sheets Containment (liners for landfills, ponds)
Geocomposites Combinations (e.g., geotextile + geonet) Drainage (geocomposite drains)
Geocells 3D honeycombs Reinforcement, Confinement (slope protection, load support)

Uses in Foundation Engineering:

  1. Separation: Prevent mixing of fine subgrade with coarse ballast/aggregate (railways, roads).

  2. Reinforcement: Increase bearing capacity, reduce settlement in weak soils (geogrids/geotextiles in embankments, rafts).

  3. Filtration: Allow water flow but retain soil particles (drainage layers, behind retaining walls).

  4. Containment: Liners for ponds, landfills (geomembranes).

  5. Drainage: Geocomposite drains for vertical/horizontal drainage (prefabricated).

IV. Compaction

Objectives: Increase density → increase strength, decrease compressibility/permeability, control swelling.

Field Equipment:

  • Sheepsfoot: Best for cohesive soils (kneading action).

  • Smooth-wheel (Tamping): Granular soils.

  • Pneumatic-tired: Flexible mat, good for both.

  • Vibratory: Best for clean sands/gravels.

Proctor Tests:

Feature Standard Proctor (ASTM D698) Modified Proctor (ASTM D1557)
Hammer Weight 2.5 kg (5.5 lb) 4.5 kg (10 lb)
Drop Height 305 mm (12 in) 457 mm (18 in)
No. of Layers 3 5
Blows per Layer 25 25
Compaction Energy ~600 kN-m/m³ ~2700 kN-m/m³
OMC Higher Lower
MDD Lower Higher

[!TIP] Key Difference: Modified Proctor has higher energy → higher MDD, lower OMC. Used for highway/airfield fills. Standard Proctor for general earthworks.


Final Note: This compilation strictly follows the RGPV CE-802(B) blueprint, prioritizing repeated exam topics (SPT corrections, IS bearing capacity, pile group/NSF, earth pressure theories, problematic soils). All definitions, formulas, and procedures are boxed for quick revision. Practice numerical problems from past papers using the step-by-step methods outlined.

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