IS 1498:1970 is the Indian Standard (BIS) for classification and identification of soils for general engineering purposes. This standard covers the classification and identification of soils for general engineering purposes based on their index properties. It establishes a unified soil classification system categorizing soils into coarse-grained, fine-grained, and highly organic soils using both laboratory tests and field identification methods.
Provides a system for classification and identification of soils based on their engineering properties and behaviour for general engineering purposes.
Classification & identification of soils for engineering purposes. USCS-equivalent system used in Indian geotech reports.
| Reference | Value | Clause |
|---|---|---|
| Coarse-grained — gravel (G) | > 50 % retained on 4.75 mm | Cl. 4.2 (Table 2) |
| Coarse-grained — sand (S) | > 50 % retained on 75 μm + < 50 % > 4.75 mm | Cl. 4.2 (Table 2) |
| Fine-grained — silt/clay (M/C) | ≥ 50 % passes 75 μm | Cl. 4.2 (Table 2) |
| Well-graded gravel — symbol | GW | Cl. 4.2 (Table 2) |
| Poorly-graded gravel — symbol | GP | Cl. 4.2 (Table 2) |
| Silty gravel / clayey gravel | GM / GC | Cl. 4.2 (Table 2) |
| Well-graded sand — symbol | SW | Cl. 4.2 (Table 2) |
| Poorly-graded sand — symbol | SP | Cl. 4.2 (Table 2) |
| Silty sand / clayey sand | SM / SC | Cl. 4.2 (Table 2) |
| Inorganic silt low-plasticity | ML (LL < 35) | Cl. 4.3 |
| Inorganic silt intermediate-plasticity | MI (LL 35–50) | Cl. 4.3 |
| Inorganic silt high-plasticity | MH (LL > 50) | Cl. 4.3 |
| Inorganic clay low-plasticity | CL (LL < 35) | Cl. 4.3 |
| Inorganic clay intermediate-plasticity | CI (LL 35–50) | Cl. 4.3 |
| Inorganic clay high-plasticity | CH (LL > 50) | Cl. 4.3 |
| Organic silt — symbol | OL / OI / OH | Cl. 4.3 |
| Peat / highly organic — symbol | Pt | Cl. 4.3 |
| Coefficient of uniformity Cu (well-graded) | Cu > 4 (gravel) / > 6 (sand) | Cl. 4.2.4 |
| Coefficient of curvature Cc (well-graded) | 1 ≤ Cc ≤ 3 | Cl. 4.2.4 |
| A-line equation (PI vs LL)— separates clay from silt on plasticity chart | PI = 0.73 (LL − 20) | Fig. 1 |
| Black cotton soil — typical classification | CH (sometimes CI) | Annex |
| Laterite — typical classification | ML, MI, or SM (depends on weathering) | Annex |
IS 1498:1970 is the Indian Standard Classification and Identification of Soils for General Engineering Purposes — India's adaptation of the Unified Soil Classification System (USCS) originally developed by Casagrande. Every geotechnical investigation report in India tags soil samples per IS 1498: ML, CL, SP, SC, GW, etc.
Use it whenever you need to: - Bin soil samples from boreholes into one of 15 standard groups based on grain size + plasticity - Communicate soil type across designer / contractor / lab without long descriptive paragraphs - Choose appropriate design parameters — bearing capacity, settlement, permeability, compaction targets all key off classification - Specify backfill or borrow — tender specs reference IS 1498 groups (e.g., 'free-draining granular fill SP or SW')
The code is paired with IS 2720 Part 4 (grain-size analysis) and IS 2720 Part 5 (Atterberg limits — LL and PL) — these tests give you the inputs (% gravel, sand, fines; LL, PI) that drop the soil into a classification group.
Step 1 — Coarse vs fine: examine % passing 75-micron sieve. - < 50% passing → coarse-grained (gravel or sand) - ≥ 50% passing → fine-grained (silt or clay)
Step 2 — Sub-classify:
Coarse-grained — Gravels (G, > 50% of coarse fraction > 4.75 mm): - GW — Well-graded gravel (Cu ≥ 4, 1 ≤ Cc ≤ 3); excellent foundation, drains freely - GP — Poorly graded gravel (uniformly graded or gap-graded); good drainage, less stable - GM — Silty gravel (5-12% fines, fines are silty); fair drainage - GC — Clayey gravel (5-12% fines, fines are clayey); poor drainage
Coarse-grained — Sands (S, > 50% of coarse fraction < 4.75 mm): - SW — Well-graded sand; good for foundations, embankments - SP — Poorly graded sand; common in river beach deposits - SM — Silty sand; can be frost-susceptible - SC — Clayey sand; reduced drainage, may be expansive
Fine-grained — Silts and Clays (low compressibility, LL < 50): - ML — Inorganic silt of low compressibility - CL — Inorganic clay of low to medium plasticity - OL — Organic silt or clay of low plasticity
Fine-grained — High compressibility (LL ≥ 50): - MH — Inorganic silt of high compressibility (loess, micaceous) - CH — Inorganic clay of high plasticity (fat clay, black cotton soil) - OH — Organic clay or silt of high plasticity
Highly organic soils: - Pt — Peat, muck, highly organic soils (avoid for foundations)
Plasticity chart (Casagrande): plots LL on x-axis vs PI on y-axis. The 'A-line' (PI = 0.73(LL − 20)) separates clays (above A-line) from silts (below). The 'U-line' (PI = 0.9(LL − 8)) is an empirical upper bound — points above U-line are physically impossible and indicate test error.
Problem: From IS 2720 Part 4 sieve analysis: % passing 75 μm = 35%; % retained on 4.75 mm = 25%. From IS 2720 Part 5 Atterberg: LL = 32%, PL = 18%.
Step 1 — Coarse or fine? % passing 75 μm = 35% < 50% → coarse-grained ✓
Step 2 — Gravel or sand? Of the coarse fraction (100% − 35% fines = 65% coarse), how much is gravel vs sand? % retained on 4.75 mm (gravel) = 25% of total → 25/65 = 38% of coarse fraction is gravel → Less than half is gravel → sand-dominated coarse → S
Step 3 — Classify the fines: Fines content (35%) > 12% → fines content is significant; classify by Atterberg. PI = LL − PL = 32 − 18 = 14 Plot (LL=32, PI=14) on plasticity chart: A-line at LL = 32: PI = 0.73 × (32 − 20) = 8.76 Point (32, 14) is ABOVE A-line → fines are clayey → SC
Final classification: SC — Clayey sand
Design implications: - Drainage poor — provide weep holes if retained - Bearing capacity: refer to IS 6403 using c, φ from triaxial — not just SPT N (clayey sand has cohesion) - Compaction: target Modified Proctor density per IS 2720 Part 8, with moisture control at OMC ± 2% - Frost susceptibility: low (only relevant for Himalayan/high-altitude projects)
1. Misinterpreting Cu and Cc — Coefficient of Uniformity Cu = D60/D10; Coefficient of Curvature Cc = (D30)²/(D10 × D60). For well-graded soils: Cu ≥ 4 (sands) or ≥ 6 (gravels), AND 1 ≤ Cc ≤ 3. Both criteria must hold. Many reports tag SW without checking Cc.
2. Skipping the dual-symbol rule — when fines content is 5-12%, the soil is BORDERLINE coarse-grained. IS 1498 requires a dual symbol: SW-SM, SP-SC, GW-GC, etc. Reports that just give 'SW' for a 10%-fines sand are technically incomplete.
3. Treating black cotton soil as CL — Indian black cotton soil (regur) routinely shows LL > 50, PI > 25, plotting in CH zone. Classification matters because IS 1904, IS 2911 Part 3, and IS 13094 all treat CH (expansive clay) very differently from CL (medium-plasticity clay).
4. Forgetting organic matter — fresh-looking 'silt' from coastal Gujarat, Sundarbans, or back-bay Mumbai is often organic silt (OL or OH). Test: oven-dry LL vs natural LL. If oven-drying drops LL by > 25%, the soil contains significant organic matter — reclassify as O-prefix.
5. Using IS 1498 alone for design — classification tells you WHAT the soil is. It does NOT give you c, φ, N, or modulus E. Always pair classification with the appropriate IS 2720 strength/stiffness test. SC has wide internal variation — same group, different design parameters.
6. Confusing IS 1498 with AASHTO M 145 — pavement engineers sometimes use AASHTO M 145 group classification (A-1 through A-7). IRC 37:2018 references AASHTO for road subgrade. Don't mix — IS 1498 for general geotech, AASHTO for pavement subgrade.
IS 1498:1970 is 55 years old but remains entirely functional — the underlying Casagrande/USCS framework is timeless and globally consistent. India hasn't revised it because the international parent (ASTM D2487) hasn't materially changed either. Minor BIS amendments in 1987 added clarifications on dual-symbol rules; that's the latest substantive touch.
For routine site investigation reports in India: IS 1498 is universally accepted by structural reviewers, ULB authorities, NHAI, and private clients. Reports without IS 1498 classification get rejected.
For research-grade or large infrastructure projects (HSR, metros, port works): supplement with ASTM D2487 (latest edition) and consider additional sub-classification for problem soils — sensitivity classification per Skempton-Northey, swell potential per Holtz-Gibbs (specific to expansive CH soils), or organic content per ASTM D2974. IS 1498 alone is coarse for these.
One practical note: the 15-group system can mask important variations within a group. 'CH' includes both Maharashtra Vidarbha black cotton (PI 30-40, swell pressure 50-300 kPa) and Coastal Andhra marine clay (PI 30-40, soft, sensitive, but not swelling). Same group, very different design implications. Use IS 1498 as the first cut; always read the full sample description and lab test results.
| Parameter | IS Value | International | Source |
|---|---|---|---|
| Coarse/Fine Soil Boundary | 50% passing 75-micron IS Sieve | 50% passing 0.075-mm (No. 200) sieve | ASTM D2487 |
| Gravel/Sand Boundary | 4.75-mm IS Sieve | 4.75-mm (No. 4) sieve | ASTM D2487 |
| Fine-Grained Plasticity Division | Low (LL<35), Intermediate (35-50), High (LL>50) | Low (LL<50), High (LL≥50) | ASTM D2487 |
| A-Line Equation | PI = 0.73 (LL - 20) | PI = 0.73 (LL - 20) | ASTM D2487 |
| Criteria for Well-Graded Sand (SW) | Cu ≥ 6 and 1 ≤ Cc ≤ 3 | Cu ≥ 6 and 1 ≤ Cc ≤ 3 | ASTM D2487 |
| Symbol for Intermediate Plasticity Clay | CI | CL (as LL would be < 50) | ASTM D2487 |
| Symbol for Highly Organic Soil | Pt | PT | ASTM D2487 |
| Sand/Silt Boundary | 0.075 mm | 0.063 mm | ISO 14688-2 |