Soil Mechanics Quick Reference

IS 1498:1970   IS 2720  |  Bastukar.in Civil Engineering Reference

1. Soil Classification — IS 1498:1970 (Based on Unified Soil Classification)

SymbolFull NameKey PropertyCu / Cc Criteria
GWWell-graded GravelCoarse, <5% fines, D50>4.75mmCu≥4, 1≤Cc≤3
GPPoorly-graded GravelUniform or gap-graded gravelFails GW criteria
GMSilty GravelGravel with silt fines, PI<4Atterberg limits below A-line
GCClayey GravelGravel with clay fines, PI>7Atterberg limits above A-line
SWWell-graded SandSand, <5% fines, D50 0.075–4.75mmCu≥6, 1≤Cc≤3
SPPoorly-graded SandUniform sandFails SW criteria
SMSilty SandSand with silt fines, PI<4
SCClayey SandSand with clay fines, PI>7
MLInorganic Silt (Low plasticity)Fine, LL<50, below A-line
CLInorganic Clay (Low-Med plasticity)Fine, LL<50, above A-line, PI>7
OLOrganic Silt/Clay (Low plasticity)LL<50, organic odor
MHInorganic Silt (High plasticity)Fine, LL>50, below A-line
CHInorganic Clay (High plasticity)Fine, LL>50, above A-lineBlack cotton soil typical
OHOrganic Clay (High plasticity)LL>50, organic
PtPeat / Highly Organic soilDark colour, fibrous, organic >75%Not suitable for construction
Plasticity Chart (Casagrande): A-line: PI = 0.73(LL - 20)
U-line (upper boundary): PI = 0.9(LL - 8)
Cu = D60/D10    Cc = D30² / (D10 × D60)

2. Atterberg Limits — Definitions

LimitDefinitionTest MethodSignificance
Liquid Limit (LL)Water content at which soil transitions from plastic to liquid stateCasagrande cup (IS 2720 Pt.5) or Fall coneUpper bound of plasticity
Plastic Limit (PL)Minimum water content at which soil can be rolled into 3mm threadThread rolling (IS 2720 Pt.5)Lower bound of plasticity
Plasticity Index (PI)PI = LL – PLCalculatedRange of plastic behaviour
Shrinkage Limit (SL)Water content below which no volume change occurs on dryingIS 2720 Pt.6Volume stability
Liquidity Index (LI)LI = (w – PL) / PICalculatedLI>1: liquid; LI<0: semi-solid
Activity (A)A = PI / % clay fraction (<2μm)CalculatedA<0.75 inactive; 0.75–1.25 normal; >1.25 active (swelling)

3. Compaction Tests — IS 2720

ParameterStandard Proctor (IS 2720 Pt.7)Modified Proctor (IS 2720 Pt.8)
Mould volume944 cm³ (1000 mL)944 cm³ (1000 mL)
Rammer mass2.6 kg4.9 kg
Drop height310 mm450 mm
No. of layers35
Blows per layer2525
Compaction energy592 kJ/m³2700 kJ/m³
Equivalent field testLight compaction (AASHTO T99)Heavy compaction (AASHTO T180)
Maximum Dry Density: γd = G × γw / (1 + e)
Zero Air Void line: γd = G × γw / (1 + wG/Sr) [Sr=1 for ZAV]
Field compaction requirement: typically 95–98% of MDD

4. Bearing Capacity — Terzaghi's Equations

Footing TypeGeneral Bearing Capacity Formula
Strip Footingqu = c·Nc + q·Nq + 0.5·γ·B·Nγ
Square Footingqu = 1.3c·Nc + q·Nq + 0.4·γ·B·Nγ
Circular Footingqu = 1.3c·Nc + q·Nq + 0.3·γ·B·Nγ
Net Ultimate BCqnet,ult = qu – q = qu – γ·Df
Safe Bearing Capacityqsafe = qnet,ult / FOS + γ·Df   (FOS = 3 typically)
For φ=0 (pure clay)qu = 5.14·Cu + γ·Df   (Nc=5.14, Nq=1, Nγ=0)

5. Bearing Capacity Factors (Terzaghi)

φ (°)NcNq
05.141.000.00
56.491.570.45
108.352.471.22
1510.983.942.50
2014.836.405.39
2520.7210.6610.88
3030.1418.4022.40
3546.1233.3048.03
4075.3164.20109.41

6. SPT Correlation Table (IS 2131)

N-value (blows/300mm)Relative Density (Sand)Friction Angle φ (approx.)Consistency (Clay)Undrained Shear Strength Cu (kPa)
0 – 4Very Loose (<15%)<28°Very Soft<25
4 – 10Loose (15–35%)28° – 30°Soft25 – 50
10 – 30Medium Dense (35–65%)30° – 36°Medium Stiff50 – 100
30 – 50Dense (65–85%)36° – 41°Stiff100 – 200
>50Very Dense (>85%)>41°Very Stiff / Hard>200

7. Typical Shear Strength Parameters

Soil TypeCohesion c (kPa)Friction Angle φRemarks
Clean Gravel (GW/GP)032° – 40°
Clean Sand (SW)030° – 37°
Silty Sand (SM)0 – 528° – 34°
Inorganic Silt (ML)5 – 1526° – 32°
Low plasticity clay (CL)10 – 4020° – 28°Drained parameters
High plasticity clay (CH)20 – 8010° – 20°Black cotton: c=0, φ=0 (undrained)
Stiff fissured clay0 – 108° – 15°Residual strength

8. Permeability (k) — Typical Values

Soil Typek (m/s)Drainage Condition
Clean gravel10⁻² – 1Very freely draining
Coarse sand10⁻⁴ – 10⁻²Freely draining
Fine/medium sand10⁻⁶ – 10⁻⁴Draining
Silty sand10⁻⁷ – 10⁻⁶Poor drainage
Silt (ML)10⁻⁹ – 10⁻⁷Very poor drainage
Clay< 10⁻⁹Practically impermeable
Darcy's Law: v = k × i    Q = k × i × A
Hazen's formula: k (m/s) = 1.0 × 10⁻² × D10² (mm) [for loose clean sands only]

9. Consolidation Parameters — Typical Values

ParameterSymbolTypical RangeRemarks
Compression indexCc0.1 – 1.5Cc ≈ 0.009(LL–10) for NC clays
Swelling/recompression indexCsCc/5 to Cc/10For OC clays
Coefficient of consolidationCv10⁻⁸ – 10⁻⁶ m²/sHigher for sandy soils
Coefficient of volume compressibilitymv10⁻⁴ – 10⁻² m²/kN
Primary consolidation settlement: S = Cc × H / (1+e0) × log10[(p0 + Δp)/p0]
Time factor: Tv = Cv × t / Hdr²
For 90% consolidation: Tv = 0.848

10. IS 2720 Test Methods Summary

IS 2720 PartTest NamePurpose
Part 2Determination of moisture contentOven-drying at 105–110°C
Part 3Specific gravity (Pycnometer)Particle density
Part 4Grain size analysis (Sieve + Hydrometer)PSD curve, Cu, Cc
Part 5Atterberg limits (LL, PL)Plasticity classification
Part 6Shrinkage factorsShrinkage limit
Part 7Standard Proctor compactionMDD, OMC (light)
Part 8Modified Proctor compactionMDD, OMC (heavy)
Part 10Unconfined compressive strengthCu of cohesive soils
Part 11CBR (California Bearing Ratio)Pavement subgrade strength
Part 12Consolidation test (Oedometer)Cc, Cv, mv
Part 13Direct shear testc, φ (drained)
Part 14Triaxial test (UU, CU, CD)c, φ at different drainage conditions
Part 15Permeability (constant/falling head)k of soil
Part 16Swell indexExpansive soil potential