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IS 1498 : 1970Classification and identification of soils for general engineering purposes

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ASTM D2487-17(2023) · ISO 14688-2 · BS 5930
CurrentEssentialCode of PracticeGeotechnical · Soil and Foundation
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OverviewValues7InternationalTablesFAQ4RelatedQA/QCNew

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.

Quick Reference — IS 1498:1970 Soil Classification

Classification & identification of soils for engineering purposes. USCS-equivalent system used in Indian geotech reports.

✓ Verified 2026-04-28
ReferenceValueClause
Coarse-grained — gravel (G)> 50 % retained on 4.75 mmCl. 4.2 (Table 2)
Coarse-grained — sand (S)> 50 % retained on 75 μm + < 50 % > 4.75 mmCl. 4.2 (Table 2)
Fine-grained — silt/clay (M/C)≥ 50 % passes 75 μmCl. 4.2 (Table 2)
Well-graded gravel — symbolGWCl. 4.2 (Table 2)
Poorly-graded gravel — symbolGPCl. 4.2 (Table 2)
Silty gravel / clayey gravelGM / GCCl. 4.2 (Table 2)
Well-graded sand — symbolSWCl. 4.2 (Table 2)
Poorly-graded sand — symbolSPCl. 4.2 (Table 2)
Silty sand / clayey sandSM / SCCl. 4.2 (Table 2)
Inorganic silt low-plasticityML (LL < 35)Cl. 4.3
Inorganic silt intermediate-plasticityMI (LL 35–50)Cl. 4.3
Inorganic silt high-plasticityMH (LL > 50)Cl. 4.3
Inorganic clay low-plasticityCL (LL < 35)Cl. 4.3
Inorganic clay intermediate-plasticityCI (LL 35–50)Cl. 4.3
Inorganic clay high-plasticityCH (LL > 50)Cl. 4.3
Organic silt — symbolOL / OI / OHCl. 4.3
Peat / highly organic — symbolPtCl. 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 ≤ 3Cl. 4.2.4
A-line equation (PI vs LL)— separates clay from silt on plasticity chartPI = 0.73 (LL − 20)Fig. 1
Black cotton soil — typical classificationCH (sometimes CI)Annex
Laterite — typical classificationML, MI, or SM (depends on weathering)Annex
⚠ Reaffirmed; remains the working standard for Indian soil classification. Cross-referenced by IS 6403 (bearing capacity), IS 1888 (plate load), and IS 2720 series.

Overview

Status
Current
Usage level
Essential
Domain
Geotechnical — Soil and Foundation
Type
Code of Practice
Amendments
Amendment 1 (1982); Amendment 2 (1987)
International equivalents
ASTM D2487-17(2023) · ASTM International (US)ISO 14688-2:2017 · ISO (International)BS 5930:2015+A1:2020 · BSI (UK)AS 1726-2017 · Standards Australia (AU)
Typically used with
IS 460
Also on InfraLens for IS 1498
7Key values2Tables7QA/QC templates2Handbook topics4FAQs
Practical Notes
! Always use the A-line chart in conjunction with liquid limit and plasticity index to accurately classify fine-grained soils into clays or silts.
! Dual symbols (e.g., SW-SM) must be used when a coarse-grained soil contains between 5% and 12% fines.
! Field identification methods like dilatancy (shaking test), toughness (threading test), and dry strength are critical for quick on-site preliminary classification.
Frequently referenced clauses
Cl. 3Division of SoilsCl. 4Laboratory Identification ProcedureCl. 5Field Identification ProcedureCl. 6Boundary Classifications
Pulled from IS 1498:1970. Browse the full clause & table index below in Tables & Referenced Sections.
Updates & Amendments2 amendments
1982Amendment 1 (1982)
1987Amendment 2 (1987)
Consolidated list per BIS. For the text of each amendment, refer to the BIS portal link above.
soilsandgravelclaysiltpeatearth

International Equivalents

Similar International Standards
ASTM D2487-17(2023)ASTM International (US)
HighCurrent
Standard Practice for Classification of Soils for Engineering Purposes (Unified Soil Classification System)
Provides a nearly identical classification system based on the same USCS principles and laboratory testing.
ISO 14688-2:2017ISO (International)
MediumCurrent
Geotechnical investigation and testing — Identification and classification of soil — Part 2: Principles for a classification
Defines international principles for soil classification but uses different particle size boundaries and plasticity divisions.
BS 5930:2015+A1:2020BSI (UK)
MediumCurrent
Code of practice for ground investigations
Comprehensive UK code for ground investigations which includes a soil classification system largely based on ISO 14688.
AS 1726-2017Standards Australia (AU)
MediumCurrent
Geotechnical site investigations
Australian standard for geotechnical investigations that includes a soil classification system similar to USCS but with some local variations.
Key Differences
≠IS 1498 subdivides fine-grained soils into three plasticity groups: Low (L) for LL < 35, Intermediate (I) for 35 ≤ LL ≤ 50, and High (H) for LL > 50. ASTM D2487 uses only two groups: Low (L) for LL < 50 and High (H) for LL ≥ 50.
≠ASTM D2487 provides more explicit and mandatory rules for the use of dual symbols for borderline classifications (e.g., soils with 5-12% fines like GW-GM), whereas IS 1498 is less prescriptive about their application.
≠The naming conventions for coarse-grained soils with secondary fractions (e.g., 'sandy gravel' vs 'gravel with sand') are more rigorously defined by specific percentage ranges in ASTM D2487 compared to the more general guidelines in IS 1498.
≠ASTM D2487 is frequently updated to incorporate new research and clarifications, while IS 1498:1970 has remained fundamentally unchanged since its publication, only being reaffirmed.
Key Similarities
≈Both standards are fundamentally based on the Unified Soil Classification System (USCS), using particle size distribution and plasticity characteristics as the primary classification criteria.
≈The boundary between coarse-grained and fine-grained soils is identical in both standards, defined at 50% of material passing the 75-micron (No. 200) sieve.
≈Both standards use the 4.75 mm (No. 4) sieve as the dividing line between gravel and sand fractions within coarse-grained soils.
≈The 'A-Line' on the plasticity chart, which separates clays from silts, is defined by the same equation in both standards: Plasticity Index (PI) = 0.73 * (Liquid Limit (LL) - 20).
≈The criteria for classifying coarse-grained soils as 'well-graded' (W) or 'poorly-graded' (P) based on the coefficients of uniformity (Cu) and curvature (Cc) are identical in both standards (e.g., Cu ≥ 4 and 1 ≤ Cc ≤ 3 for well-graded gravel).
Parameter Comparison
ParameterIS ValueInternationalSource
Coarse/Fine Soil Boundary50% passing 75-micron IS Sieve50% passing 0.075-mm (No. 200) sieveASTM D2487
Gravel/Sand Boundary4.75-mm IS Sieve4.75-mm (No. 4) sieveASTM D2487
Fine-Grained Plasticity DivisionLow (LL<35), Intermediate (35-50), High (LL>50)Low (LL<50), High (LL≥50)ASTM D2487
A-Line EquationPI = 0.73 (LL - 20)PI = 0.73 (LL - 20)ASTM D2487
Criteria for Well-Graded Sand (SW)Cu ≥ 6 and 1 ≤ Cc ≤ 3Cu ≥ 6 and 1 ≤ Cc ≤ 3ASTM D2487
Symbol for Intermediate Plasticity ClayCICL (as LL would be < 50)ASTM D2487
Symbol for Highly Organic SoilPtPTASTM D2487
Sand/Silt Boundary0.075 mm0.063 mmISO 14688-2
⚠ Verify details from original standards before use

Key Values7

Quick Reference Values
coarse grained soil boundary> 50% retained on 75-micron IS Sieve
fine grained soil boundary> 50% passing 75-micron IS Sieve
gravel sand boundary4.75 mm IS Sieve
low plasticity liquid limit< 35%
medium plasticity liquid limit35% to 50%
high plasticity liquid limit> 50%
dual symbol fines percentage5% to 12% fines
Key Formulas
Ip = 0.73(wL - 20) — Equation of the A-line for plasticity chart
Cu = D60 / D10 — Coefficient of uniformity
Cc = (D30)^2 / (D10 * D60) — Coefficient of curvature

Tables & Referenced Sections

Key Tables
Table 1 - Field Identification of Soils
Table 2 - Soil Classification based on Laboratory Tests
Key Clauses
Clause 3 - Division of Soils
Clause 4 - Laboratory Identification Procedure
Clause 5 - Field Identification Procedure
Clause 6 - Boundary Classifications

Related Resources on InfraLens

Cross-Referenced Codes
IS 460:2000Test Sieves: Part-I Wire Cloth Test Sieves
→
Handbook & Design Rules
Handbook Topics
📖Soil Classification (IS 1498)
→
📖Earthwork Bulking & Shrinkage Factors
→

Frequently Asked Questions4

What is the liquid limit boundary between low and medium plasticity soils?+
A liquid limit of 35%. Soils with less than 35% are low plasticity (L), and between 35% to 50% are medium plasticity (I).
When is a soil classified as coarse-grained?+
When more than 50% of the total material by weight is retained on a 75-micron IS Sieve.
What do the symbols 'CH' and 'SM' stand for?+
'CH' stands for Clay of High compressibility (liquid limit > 50%), and 'SM' stands for Silty Sand.
What are the grading criteria for a well-graded gravel (GW)?+
The coefficient of uniformity (Cu) must be greater than 4, and the coefficient of curvature (Cc) must be between 1 and 3.

QA/QC Inspection Templates

Code-Specific Templates for IS 1498
✅
Subgrade Inspection Checklist
checklist
Excel / PDF
✅
Excavation Inspection Checklist
checklist
Excel / PDF
📊
SPT (Standard Penetration Test) Report
test-report
Excel / PDF
📊
CBR (California Bearing Ratio) Test Report
test-report
Excel / PDF
📊
Atterberg Limits Test Report
test-report
Excel / PDF
📊
Grain Size / Sieve Analysis Report
test-report
Excel / PDF
📝
Excavation & Earthwork Method Statement
form
Excel / PDF