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Cheatsheet Soil Mechanics - Civil Engineering SSC JE (Technical) - Civil Engineering

1. Soil Phase Relationships

1.1 Three-Phase System

ParameterFormula & Definition
Void Ratio (e)e = Vv/Vs (ratio of void volume to solid volume)
Porosity (n)n = Vv/V × 100% (ratio of void volume to total volume)
Relationshipe = n/(1-n) and n = e/(1+e)
Degree of Saturation (S)S = Vw/Vv × 100% (percentage of voids filled with water)
Water Content (w)w = Ww/Ws × 100% (mass of water to mass of solids)
Air Content (ac)ac = Va/V × 100%

1.2 Unit Weights

TypeFormula
Bulk Unit Weight (γ)γ = W/V = (G + Se)γw/(1+e)
Dry Unit Weight (γd)γd = Ws/V = Gγw/(1+e) = γ/(1+w)
Saturated Unit Weight (γsat)γsat = (G + e)γw/(1+e)
Submerged Unit Weight (γ')γ' = γsat - γw = (G - 1)γw/(1+e)
Zero Air Voids Unit Weightγzav = Gγw(1+w)/(1+wG)

1.3 Key Relationships

  • Se = wG (fundamental relationship between saturation, water content, specific gravity, and void ratio)
  • For fully saturated soil: S = 1, therefore e = wG
  • Specific Gravity (G): ratio of unit weight of soil solids to unit weight of water (2.6-2.8 for most soils)

2. Soil Classification

2.1 Grain Size Distribution

Soil TypeParticle Size Range
Gravel4.75 mm to 80 mm
Coarse Sand2.0 mm to 4.75 mm
Medium Sand0.425 mm to 2.0 mm
Fine Sand0.075 mm to 0.425 mm
Silt0.002 mm to 0.075 mm
Clay< 0.002 mm

2.2 Gradation Coefficients

ParameterFormula & Interpretation
Uniformity Coefficient (Cu)Cu = D60/D10; Cu > 4 (gravel) or > 6 (sand) indicates well-graded
Coefficient of Curvature (Cc)Cc = (D30)2/(D10 × D60); 1 < Cc < 3 indicates well-graded
Effective Size (D10)Particle size at 10% finer; controls permeability

2.3 Atterberg Limits

Limit/IndexDefinition & Formula
Liquid Limit (LL or wL)Water content at 25 blows in Casagrande apparatus; transition from liquid to plastic state
Plastic Limit (PL or wP)Water content at which soil crumbles when rolled to 3 mm thread
Shrinkage Limit (SL or wS)Water content below which no volume change occurs on drying
Plasticity Index (PI or IP)PI = LL - PL (range of water content over which soil is plastic)
Liquidity Index (LI or IL)LI = (w - PL)/(LL - PL) (consistency of natural soil)
Consistency Index (CI or IC)CI = (LL - w)/(LL - PL) = 1 - LI
Flow Index (IF)Slope of flow curve in liquid limit test
Toughness Index (IT)IT = PI/IF

2.4 Soil Classification Systems

2.4.1 IS Classification System

  • Coarse-grained (> 50% retained on 75μ sieve): Gravel (G) and Sand (S)
  • Fine-grained (> 50% passing 75μ sieve): Silt (M) and Clay (C)
  • Well-graded: W; Poorly-graded: P; Low plasticity: L; High plasticity: H
  • A-line equation: PI = 0.73(LL - 20)
  • Clay: plots above A-line; Silt: plots below A-line

2.4.2 Activity

Activity (A)Classification
A = PI / (% clay fraction)A < 0.75: Inactive; 0.75-1.25: Normal; > 1.25: Active

3. Soil Compaction

3.1 Compaction Parameters

ParameterDescription
Optimum Moisture Content (OMC)Water content at which maximum dry density is achieved
Maximum Dry Density (MDD)Peak dry density on compaction curve
Zero Air Voids LineTheoretical line representing S = 100%; actual curve lies to the left

3.2 Compaction Tests

Test TypeDetails
Standard Proctor Test2.6 kg rammer, 310 mm drop, 3 layers, 25 blows/layer, 1000 cm³ mold
Modified Proctor Test4.9 kg rammer, 450 mm drop, 5 layers, 25 blows/layer, 1000 cm³ mold

3.3 Field Compaction Control

MethodFormula/Description
Degree of Compaction= (γd,fieldd,max) × 100%
Sand Cone MethodMeasures in-situ density by volume replacement with calibrated sand
Core Cutter MethodDirect measurement using cylindrical cutter of known volume

3.4 Compaction Effects

  • Dry of OMC: flocculated structure, higher permeability, higher strength, more compressible
  • Wet of OMC: dispersed structure, lower permeability, lower strength, less compressible

4. Permeability and Seepage

4.1 Darcy's Law

ParameterFormula
Darcy's Lawv = ki (velocity = coefficient of permeability × hydraulic gradient)
Discharge Velocity (v)v = q/A (apparent velocity through total cross-section)
Seepage Velocity (vs)vs = v/n = ki/n (actual velocity through voids)
Hydraulic Gradient (i)i = Δh/L (head loss per unit length)
Discharge (q)q = kiA

4.2 Coefficient of Permeability (k)

Soil Typek (cm/s)
Gravel> 10-1
Sand10-3 to 10-1
Silt10-7 to 10-3
Clay< 10-7

4.3 Laboratory Permeability Tests

Test TypeFormula & Application
Constant Head Testk = QL/(Aht); for coarse-grained soils (k > 10-4 cm/s)
Falling Head Testk = (aL/At) ln(h1/h2); for fine-grained soils (k < 10-4 cm/s)

4.4 Layered Soil Permeability

Flow DirectionEquivalent Permeability
Horizontal Flow (Parallel)kh = (k1H1 + k2H2 + ... + knHn)/H
Vertical Flow (Series)kv = H/(H1/k1 + H2/k2 + ... + Hn/kn)

4.5 Empirical Relations

  • Hazen's Formula: k (cm/s) = C(D10)2 where C = 100-150, D10 in cm
  • Kozeny-Carman: k = (e3/(1+e)) × constant

4.6 Flow Net

ParameterFormula
Seepage Dischargeq = kH(Nf/Nd) per unit length, where Nf = number of flow channels, Nd = number of equipotential drops
Head LossΔh = H/Nd
Hydraulic Gradienti = Δh/Δl (between two equipotential lines)
Exit Gradientie = H/(Nd × d) where d = length of last flow element at exit

4.7 Seepage Pressure and Critical Gradient

ParameterFormula
Seepage ForceFs = iγwV (force per unit volume = iγw)
Critical Hydraulic Gradientic = (G-1)/(1+e) = γ'/γw (condition for piping/quick sand)
Factor of Safety (Piping)F = ic/ie (should be > 4-5)

5. Effective Stress and Capillarity

5.1 Effective Stress Principle

ParameterFormula & Description
Total Stress (σ)σ = γz (stress due to total unit weight of soil)
Pore Water Pressure (u)u = γwhw (neutral stress)
Effective Stress (σ')σ' = σ - u (controls shear strength and volume change)

5.2 Stress Conditions

ConditionCalculation
Dry Soilσ' = γdz; u = 0
Saturated Soil (GWT at surface)σ = γsatz; u = γwz; σ' = γ'z
Saturated Soil (GWT at depth)Above GWT: σ' = γz; Below GWT: σ' = γz - γw(z-zw)
Submerged Soilσ' = γ'z = (γsat - γw)z

5.3 Capillary Rise

ParameterFormula
Height of Capillary Risehc = C/e × D10 where C = 0.1-0.5 cm²
Simplified Formulahc (mm) ≈ 30/D10 (mm) for fine sand
Capillary Pressureu = -γwh (negative pore pressure above GWT)

6. Compressibility and Consolidation

6.1 One-Dimensional Consolidation

ParameterFormula & Definition
Void Ratio ChangeΔe = e0 - ef
Compression Index (Cc)Cc = -Δe/Δlog(σ') = (e1 - e2)/log(σ'2/σ'1) for normally consolidated clay
Recompression Index (Cr)Cr = Δe/Δlog(σ') for overconsolidated clay; Cr = 0.1 to 0.2 × Cc
Coefficient of Volume Compressibilitymv = -Δe/(1+e0)Δσ' = av/(1+e0) (units: m²/kN)
Coefficient of Compressibilityav = -Δe/Δσ'

6.2 Settlement Calculation

FormulaApplication
S = (Cc/(1+e0)) × H × log(σ'f/σ'0)Normally consolidated clay (σ'0 = σ'p)
S = (Cr/(1+e0)) × H × log(σ'f/σ'0)Overconsolidated clay when σ'f < σ'p
S = [(Cr/(1+e0)) × H × log(σ'p/σ'0)] + [(Cc/(1+e0)) × H × log(σ'f/σ'p)]Overconsolidated clay when σ'f > σ'p
S = mv × Δσ' × HGeneral formula for any clay

6.3 Preconsolidation and OCR

ParameterDefinition
Preconsolidation Pressure (σ'p)Maximum past effective stress experienced by soil
Present Effective Stress (σ'0)Current in-situ effective stress
Overconsolidation Ratio (OCR)OCR = σ'p/σ'0; OCR = 1 (normally consolidated); OCR > 1 (overconsolidated); OCR < 1 (underconsolidated)

6.4 Time-Dependent Consolidation

ParameterFormula
Coefficient of Consolidationcv = k/(mvγw) (units: m²/year or cm²/s)
Time FactorTv = cvt/d² where d = drainage path length
Drainage Path (d)d = H (one-way drainage); d = H/2 (two-way drainage)
Degree of Consolidation (U%)U = (St/Sf) × 100% (ratio of settlement at time t to final settlement)

6.5 Time Factor Relations

U (%)Tv
U < 60%Tv = (π/4)(U/100)²
U > 60%Tv = 1.781 - 0.933 log(100 - U)
50%Tv = 0.197
90%Tv = 0.848

6.6 Empirical Relations

  • Cc = 0.009(LL - 10) (Skempton)
  • Cc = 0.007(LL - 7) (Azzouz et al.)
  • Cc/(1+e0) ≈ 0.208e0 + 0.0083

6.7 Laboratory Consolidation Test

  • Oedometer test (one-dimensional consolidation)
  • Sample: 60 mm diameter, 20 mm thick
  • Casagrande log method for determining σ'p
  • Load increment ratio (LIR) = 1 (each load = previous load)

7. Shear Strength

7.1 Mohr-Coulomb Failure Criterion

ParameterFormula
Total Stressτf = c + σ tan φ
Effective Stressτf = c' + σ' tan φ' = c' + (σ - u) tan φ'
  • τf = shear strength; c, c' = cohesion (total, effective); φ, φ' = friction angle (total, effective)
  • Effective stress parameters (c', φ') govern long-term strength
  • Total stress parameters (c, φ) used for short-term undrained conditions

7.2 Direct Shear Test

AspectDescription
Sample Size60 mm × 60 mm square
DrainageCan perform drained or undrained tests
Stress StateNon-uniform; failure plane predetermined
Parametersc and φ from Mohr-Coulomb plot

7.3 Triaxial Test Types

Test TypeConsolidationDrainage During ShearApplication
UU (Unconsolidated Undrained)NoNoφu = 0; cu = undrained shear strength; rapid loading of saturated clay
CU (Consolidated Undrained)YesNo (pore pressure measured)c', φ' determined; staged construction with pore pressure
CD (Consolidated Drained)YesYesc', φ' determined; long-term stability

7.4 Shear Strength Parameters

Soil Typec' (kPa)φ' (degrees)
Sand (Loose)028-32
Sand (Dense)036-42
Normally Consolidated Clay020-30
Overconsolidated Clay> 020-35

7.5 Stress-Strain Behaviour

Soil TypeBehaviour
Dense Sand/OC ClayStrain-softening; peak strength > residual strength; dilatant (volume increase during shear)
Loose Sand/NC ClayStrain-hardening; no peak; contractant (volume decrease during shear)

7.6 Mohr Circle Relations

ParameterFormula
Major Principal Stressσ1 = σ3 + Δσ where Δσ = deviator stress
Normal Stress on Failure Planeσf = (σ1 + σ3)/2 + (σ1 - σ3)/2 × cos 2θ
Shear Stress on Failure Planeτf = (σ1 - σ3)/2 × sin 2θ
Failure Plane Angleθ = 45° + φ/2 (from horizontal)
Stress Ratio at Failureσ13 = (1 + sin φ)/(1 - sin φ) = tan²(45° + φ/2)

7.7 Undrained Shear Strength

MethodFormula/Description
UU Triaxial Testcu = (σ1 - σ3)/2; φu = 0
Unconfined Compression Testqu = (σ1 - σ3) with σ3 = 0; cu = qu/2
Vane Shear Testcu = T/(πD²H/2 + πD³/6) where T = torque, D = diameter, H = height
SensitivitySt = cu,undisturbed/cu,remolded

7.8 Pore Pressure Parameters

ParameterFormula
Pore Pressure ChangeΔu = B[Δσ3 + A(Δσ1 - Δσ3)]
B ParameterB = Δu/Δσ3; B = 1 for saturated soil, B < 1 for partially saturated
A Parameter at FailureAf = Δu/(Δσ1 - Δσ3); Af > 0.5 for NC clay, Af < 0 for dense sand/OC clay

8. Earth Pressure Theory

8.1 At-Rest Earth Pressure

ParameterFormula
Coefficient (K0)K0 = σ'h/σ'v (lateral stress/vertical stress at rest)
Jaky's Formula (NC)K0 = 1 - sin φ'
Overconsolidated ClayK0(OC) = K0(NC) × OCRsin φ'
Pressurep0 = K0γz

8.2 Active Earth Pressure (Rankine)

ParameterFormula
Coefficient (Ka)Ka = (1 - sin φ)/(1 + sin φ) = tan²(45° - φ/2)
Pressure (Cohesionless)pa = Kaγz
Pressure (c-φ soil)pa = Kaγz - 2c√Ka
Total Force (per unit width)Pa = (1/2)KaγH² (acts at H/3 from base)
Critical Depth (zc)zc = 2c/(γ√Ka) (depth at which pa = 0)

8.3 Passive Earth Pressure (Rankine)

ParameterFormula
Coefficient (Kp)Kp = (1 + sin φ)/(1 - sin φ) = tan²(45° + φ/2)
Pressure (Cohesionless)pp = Kpγz
Pressure (c-φ soil)pp = Kpγz + 2c√Kp
Total Force (per unit width)Pp = (1/2)KpγH² (acts at H/3 from base)

8.4 Coulomb's Earth Pressure Theory

CoefficientFormula
Ka (Coulomb)Ka = cos²(φ - α)/[cos²α cos(δ + α)(1 + √(sin(φ+δ)sin(φ-β)/(cos(α+δ)cos(α-β))))²]
Kp (Coulomb)Kp = cos²(φ + α)/[cos²α cos(δ - α)(1 - √(sin(φ+δ)sin(φ+β)/(cos(α-δ)cos(α-β))))²]
  • α = backfill slope angle; β = wall face inclination; δ = wall friction angle (δ = 2φ/3 for rough wall)
  • For vertical wall (β = 0), horizontal backfill (α = 0), no wall friction (δ = 0): Coulomb = Rankine

8.5 Effect of Surcharge and Water Table

  • Uniform surcharge (q): Add qKa or qKp to pressure diagram
  • Water table present: Use γ above WT and γ' below WT; add hydrostatic pressure separately
  • Submerged backfill: pa = Kaγ'z + γwz (superposition)

9. Bearing Capacity

9.1 Terzaghi's Bearing Capacity

Foundation TypeUltimate Bearing Capacity (qu)
Strip Footingqu = cNc + γDfNq + 0.5γBNγ
Square Footingqu = 1.3cNc + γDfNq + 0.4γBNγ
Circular Footingqu = 1.3cNc + γDfNq + 0.3γBNγ

9.2 Terzaghi's Bearing Capacity Factors

φ (degrees)NcNqNγ
05.71.00.0
109.62.71.2
2017.77.45.0
3037.222.519.7
4095.781.3100.4

9.3 Meyerhof's Bearing Capacity (General)

ParameterFormula
Ultimate Bearing Capacityqu = cNcscdcic + γDfNqsqdqiq + 0.5γBNγsγdγiγ
Safe Bearing Capacityqs = qu/F + γDf (F = factor of safety = 2.5-3)
Net Ultimate Bearing Capacityqnu = qu - γDf
Net Safe Bearing Capacityqns = qnu/F

9.4 Meyerhof's Shape Factors

Shapescsqsγ
Strip (L/B ≥ 5)1.01.01.0
Square1 + 0.2(B/L)1 + 0.2(B/L)1 - 0.4(B/L) = 0.6
Circular1.31.20.6
Rectangular1 + 0.2(B/L)1 + 0.2(B/L)1 - 0.4(B/L)

9.5 Depth Factors

Conditiondcdqdγ
Df/B ≤ 11 + 0.2(Df/B)1 + 0.2(Df/B)1.0
Df/B > 11 + 0.2√(Df/B)1 + 0.2√(Df/B)1.0

9.6 Inclination Factors (Load Inclination)

FactorFormula
icic = iq = (1 - α/90°)²
iγiγ = (1 - α/φ)²
  • α = inclination of load from vertical

9.7 Bearing Capacity of Layered Soils

  • Strong soil over weak soil: Use weaker layer parameters; punching shear analysis
  • Weak soil over strong soil: Use weighted average or Meyerhof's method

9.8 Bearing Capacity from SPT

Soil TypeFormula
Cohesionless (Terzaghi-Peck)qs (kPa) = 12N(B+0.3)²/B² for settlement ≤ 25 mm (B in m)
Cohesionless (IS:6403)qs (kPa) = 20N for B ≤ 1m; reduce for larger B

9.9 Pure Clay (φ = 0 condition)

ParameterFormula
Ultimate Bearing Capacityqu = cNc + γDf (Nc = 5.14 for strip)
Net Ultimate Bearing Capacityqnu = cNc
With Shape Factor (Square)qu = 1.3cNc + γDf

10. Slope Stability

10.1 Infinite Slope Analysis

ConditionFactor of Safety (F)
Dry or Moist Slope (c-φ soil)F = (c/γz sin β cos β) + (tan φ/tan β)
Cohesionless Soil (c = 0, dry)F = tan φ/tan β
Seepage Parallel to SlopeF = γ' tan φ/(γ tan β)
Submerged Slope (c = 0)F = γ' tan φ/(γ tan β)
  • β = slope angle; z = depth of slip surface

10.2 Finite Slope - Swedish Circle Method

Soil TypeFactor of Safety
Pure Clay (φ = 0)F = c × L/(W × x) where L = arc length, W = weight, x = moment arm
c-φ SoilF = Σ(c'l + N' tan φ')/ΣT where N' = effective normal force, T = tangential force

10.3 Friction Circle Method

  • Used for c-φ soils
  • Assumes resultant of normal forces passes through center of slip circle
  • Radius of friction circle: rf = R sin φ where R = radius of slip circle

10.4 Method of Slices (Fellenius)

ParameterFormula
Factor of SafetyF = Σ(c'b sec α + (W cos α - ub sec α) tan φ')/ΣW sin α
  • W = weight of slice; α = base angle of slice; b = width of slice; u = pore pressure
  • Assumes inter-slice forces are zero

10.5 Bishop's Simplified Method

ParameterFormula
Factor of SafetyF = Σ[c'b + (W - ub) tan φ']/mα / ΣW sin α
mαmα = cos α (1 + tan α tan φ'/F)
  • More accurate than Fellenius; considers inter-slice vertical forces
  • Iterative solution required

10.6 Taylor's Stability Number

ParameterFormula
Stability Number (Sn)Sn = c/(Fγh) for φ = 0 analysis
Factor of SafetyF = c/(Snγh)
  • h = height of slope; values from Taylor's charts based on slope angle and depth factor

10.7 Critical Circle Location

  • Toe circle: passes through toe of slope
  • Slope circle: passes through face of slope
  • Base circle: passes below toe (deep-seated failure)
  • For φ = 0: critical circle is toe circle
  • For φ > 0: critical circle location depends on φ and slope angle

10.8 Factor of Safety Values

  • F < 1.0: Unstable slope
  • F = 1.0: Limiting equilibrium
  • F = 1.3-1.5: Acceptable for permanent slopes
  • F = 1.2-1.3: Acceptable for temporary slopes

11. Soil Exploration and In-Situ Tests

11.1 Standard Penetration Test (SPT)

ParameterDescription
Hammer Weight63.5 kg (140 lb)
Drop Height750 mm (30 inches)
N-ValueBlows for 300 mm penetration after initial 150 mm seating
Corrected N-ValueN60 = (ER/60) × N where ER = energy ratio (%)
Overburden Correction(N1)60 = CN × N60 where CN = 1/√(σ'v/100) for σ' in kPa

11.2 SPT Correlations

ParameterCorrelation
Relative Density (Dr%)Dr ≈ √(N/0.23) for fine sand
Friction Angle (φ)φ ≈ √(12N) + 25° (Peck et al.)
Undrained Strength (cu)cu (kPa) ≈ 6N for clays

11.3 Cone Penetration Test (CPT)

ParameterDescription
Cone Apex Angle60°
Cone Base Area10 cm² (standard)
Cone Resistance (qc)Force on cone tip divided by base area
Sleeve Friction (fs)Friction on sleeve divided by sleeve area
Friction Ratio (Rf)Rf = (fs/qc) × 100%

11.4 Plate Load Test

ParameterFormula/Description
Plate Sizes300 mm, 450 mm, 600 mm, 750 mm diameter
Settlement Ratio (Clay)Sf/Sp = Bf/Bp (linear relationship)
Settlement Ratio (Sand)Sf/Sp = (Bf/Bp)² where Bf ≤ 2Bp
Modulus of Subgrade Reactionk = p/S (pressure/settlement)

11.5 Vane Shear Test

  • Undrained shear strength: cu = T/(πD²H/2 + πD³/6)
  • Standard vane: D = 50-65 mm, H/D = 2
  • Used for soft to medium stiff clays
  • Field vane more reliable than lab vane

11.6 Pressuremeter Test

  • Measures in-situ stress-strain behavior
  • Provides pressuremeter modulus (Ep) and limit pressure (pL)
  • Self-boring pressuremeter minimizes disturbance

11.7 Soil Consistency from N-Value

Clay ConsistencyN-Valuequ (kPa)
Very Soft< 2< 25
Soft2-425-50
Medium4-850-100
Stiff8-15100-200
Very Stiff15-30200-400
Hard> 30> 400

11.8 Sand Density from N-Value

DensityN-ValueRelative Density (%)
Very Loose< 4< 15
Loose4-1015-35
Medium10-3035-65
Dense30-5065-85
Very Dense> 50> 85

12. Special Topics

12.1 Liquefaction

ParameterDescription
DefinitionLoss of shear strength due to build-up of pore pressure under cyclic loading
Susceptible SoilsLoose saturated cohesionless soils with N < 15
ConditionsSaturated sand, cyclic loading (earthquakes), low relative density
PreventionDensification, drainage, ground improvement, use of stone columns

12.2 Soil Stabilization Methods

MethodApplication
Mechanical StabilizationCompaction, soil replacement, blending soils
Cement Stabilization2-10% cement by weight; increases strength and reduces plasticity
Lime Stabilization2-8% lime; effective for clayey soils; reduces plasticity, increases strength
Bitumen StabilizationWater-proofing granular soils
Chemical StabilizationSodium silicate, calcium chloride for specific applications

12.3 Ground Improvement Techniques

TechniquePurpose
PreloadingConsolidate soft clays by temporary surcharge
Vertical DrainsAccelerate consolidation (sand drains, PVD)
Stone ColumnsIncrease bearing capacity, reduce settlement, drain pore water
Dynamic CompactionDensify loose granular soils by dropping heavy weight
VibroflotationDensify granular soils using vibration
GroutingFill voids, reduce permeability, increase strength
Soil NailingStabilize slopes and excavations

12.4 Geosynthetics

TypeFunction
GeotextilesSeparation, filtration, drainage, reinforcement
GeogridsReinforcement of soil, increase bearing capacity
GeomembranesImpermeable barriers, liners
GeocompositesCombination of functions (drainage, reinforcement)

12.5 Expansive Soils

ParameterDescription
CharacteristicsHigh clay content, montmorillonite; swell on wetting, shrink on drying
Free Swell IndexFSI = [(Vd - Vk)/Vk] × 100% where Vd = distilled water volume, Vk = kerosene volume
TreatmentSoil replacement, lime stabilization, moisture barriers, under-reamed piles

12.6 Collapsible Soils

  • Lose strength and undergo large settlement upon wetting
  • Loess, residual soils with meta-stable structure
  • Treatment: compaction, prewetting, chemical stabilization

12.7 Dispersive Clays

  • Deflocculate in presence of relatively pure water
  • Prone to piping and erosion
  • Identified by pinhole test, crumb test
  • Treatment: lime treatment, use of non-dispersive filters

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FAQs on Cheatsheet Soil Mechanics - Civil Engineering SSC JE (Technical) - Civil Engineering

1. What are the key components of soil phase relationships?
Ans. Soil phase relationships involve the interactions between the solid, liquid, and gas phases within soil. The key components include the soil solids, water content, and air content. The total volume of soil can be expressed as the sum of the volumes of these three phases, often represented in terms of void ratio, degree of saturation, and moisture content.
2. How is soil classified according to the Unified Soil Classification System (USCS)?
Ans. The Unified Soil Classification System (USCS) classifies soil based on its particle size and plasticity characteristics. Soils are categorized into three major groups: coarse-grained soils (gravel and sand), fine-grained soils (silt and clay), and organic soils. Each group is further subdivided based on specific properties such as plasticity index and gradation.
3. What factors affect soil compaction and its effectiveness?
Ans. Soil compaction is influenced by several factors, including moisture content, soil type, compaction method, and the energy applied during compaction. The optimal moisture content is crucial for achieving maximum dry density. Different soils respond differently to compaction; granular soils typically compact better than cohesive soils. Methods such as vibration, kneading, and static loading can be employed to enhance compaction.
4. What is the significance of effective stress in soil mechanics?
Ans. Effective stress is a fundamental concept in soil mechanics that defines the stress carried by the soil skeleton. It is calculated as the total stress minus pore water pressure. Effective stress is crucial for understanding soil behaviour, as it influences shear strength, consolidation, and stability. It governs how soils respond to loading and drainage conditions, impacting foundation design and slope stability analyses.
5. How can the bearing capacity of soil be determined?
Ans. The bearing capacity of soil can be determined through several methods, including analytical approaches such as Terzaghi's bearing capacity equations, empirical correlations, and in-situ tests like the Standard Penetration Test (SPT) and Plate Load Test. Factors affecting bearing capacity include soil type, depth of the foundation, groundwater conditions, and the presence of nearby structures.
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