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Soil Classification & Field Identification

Purpose of classification, particle-size and textural classification, Indian Standard Soil Classification System (IS 1498) — coarse-grained, fine-grained and highly organic soils, group symbols, plasticity chart and A-line, dual symbols; Unified (USCS) and AASHTO (HRB) systems with group index; field identification tests (dilatancy, toughness, dry strength) — with solved classification examples.

📑 Contents (7 sections)

Last reviewed 16 Sept 2026 · 6 min read

Why classify soils

Classification places a soil in a group of similar engineering behaviour using simple index properties (grain size and plasticity), so engineers can communicate, anticipate problems and choose tests and construction methods before detailed testing.

Particle-size and textural classifications

  • Particle-size classification names soil by size ranges (IS: gravel 4.75–80 mm, sand 0.075–4.75 mm, silt 0.002–0.075 mm, clay < 0.002 mm).
  • Textural classification (triangular chart of % sand, silt, clay, e.g. US Bureau of Public Roads/USDA) names soils such as sandy loam, silty clay — common in agriculture and highway work but ignores plasticity.

Indian Standard Soil Classification System (IS 1498:1970)

Based on the Unified system, with three plasticity divisions for fine-grained soils.

Major divisions

Division Criterion Primary letters
Coarse-grained soils More than 50% (by mass) retained on the 75 µm sieve G (gravel), S (sand)
Fine-grained soils More than 50% passing 75 µm M (silt), C (clay), O (organic)
Highly organic soils Fibrous, dark, odorous Pt (peat)

Gravel vs sand: if more than half of the coarse fraction is retained on the 4.75 mm sieve → gravel; otherwise sand.

Secondary letters

Letter Meaning
W Well graded
P Poorly graded
M With non-plastic/low-plastic fines (silty)
C With plastic fines (clayey)
L Low plasticity/compressibility ( < 35%)
I Intermediate ( 35–50%)
H High ( > 50%)

Coarse-grained soils — groups

Fines (passing 75 µm) Classification
Less than 5% GW / GP, SW / SP by and (well graded: gravel , sand , and )
More than 12% GM / GC, SM / SC by where the fines plot on the plasticity chart (below A-line or → M; above A-line and → C)
5% to 12% Borderline — dual symbols, e.g. GW-GM, SP-SC
between 4 and 7 above A-line Dual symbol such as SM-SC

Fine-grained soils — the plasticity chart

Plot plasticity index () against liquid limit ().

FormulaA-line and U-line
  • Above the A-line → clays (C); below → silts (M) or organic soils (O).
  • Vertical lines at = 35% and 50% separate L, I, H.

Groups: CL, CI, CH (inorganic clays); ML, MI, MH (inorganic silts); OL, OI, OH (organic silts and clays, identified by odour, colour and a sharp drop in LL after oven drying); Pt (peat).

The hatched zone just above the A-line with between 4 and 7 at low LL is designated CL-ML.

FigurePlasticity chart (IS 1498)

Liquid limit wL (%)IP (%)3550A-lineCLCICHML/OLMI/OIMH/OH

Scale: horizontal axis 0–100% liquid limit; the A-line meets the axis at = 20%.

Field identification of fine-grained soils

Test Procedure Clay Silt
Dilatancy (shaking) Shake a wet pat; watch water appear/disappear None to slow Quick reaction
Toughness Roll a thread near the plastic limit Tough, stiff thread Weak, crumbly
Dry strength Crush a dried lump between fingers High Low (powders easily)
Feel / washing Rub in water Smooth, sticky, hard to wash off Gritty, washes off

Organic soils: dark colour, musty odour, spongy feel.

Other classification systems

Unified Soil Classification System (USCS)

Same letter symbols as IS 1498, but fine-grained soils have only two plasticity divisions: L ( < 50%) and H ( ≥ 50%).

AASHTO (HRB) system — for highway subgrades

Soils are grouped A-1 to A-7 (A-1 best as subgrade; A-4 to A-7 silt–clay materials; A-8 peat) using sieve analysis (2 mm, 425 µm, 75 µm) and Atterberg limits. Within groups, the group index ranks quality:

FormulaGroup index
  • = % passing 75 µm in excess of 35 (0 to 40)
  • = % passing 75 µm in excess of 15 (0 to 40)
  • = liquid limit in excess of 40 (0 to 20)
  • = plasticity index in excess of 10 (0 to 20)

GI ranges from 0 (good subgrade) to 20 (very poor); higher GI → thicker pavement.

Worked examples

Worked ExampleExample 1 — coarse-grained soil

A soil has 3% passing 75 µm; 70% of the coarse fraction passes 4.75 mm; = 0.15 mm, = 0.40 mm, = 1.10 mm. Classify.

Solution. Coarse-grained (97% retained on 75 µm). More than half the coarse fraction passes 4.75 mm → sand. Fines < 5% → W or P.

(> 6); (< 1) → not well graded → SP (poorly graded sand).

Worked ExampleExample 2 — fine-grained soil

A soil has 78% passing 75 µm, = 45%, = 22%. Classify.

Solution. Fine-grained. . A-line at = 45: → 23 > 18.25 → above A-line → clay. between 35 and 50 → CI (clay of intermediate plasticity).

Worked ExampleExample 3 — group index

A subgrade soil: 60% passing 75 µm, = 48%, = 18%. Find GI.

Solution. ; (max); ; .

Frequently tested points

  • IS 1498: coarse-grained if > 50% retained on 75 µm; gravel vs sand at 4.75 mm on the coarse fraction.
  • Fines < 5%: W/P; > 12%: M/C; 5–12%: dual symbols.
  • A-line ; above = clay, below = silt/organic.
  • IS divisions L < 35%, I 35–50%, H > 50%; USCS uses only L/H at 50%.
  • Dilatancy quick for silts; dry strength high for clays.
  • ; AASHTO A-1 best, A-7 poorest (A-8 peat).
Common MistakeCommon mistakes
  • Using the whole sample (instead of the coarse fraction) to decide gravel vs sand.
  • Classifying fine soils by LL alone without checking the A-line.
  • Forgetting the limits (0–40, 0–20) on , , , in the group index.
Revision SummaryChapter summary
  1. Classification groups soils by grain size and plasticity.
  2. IS 1498 uses G, S, M, C, O, Pt with W, P, M, C, L, I, H qualifiers.
  3. The plasticity chart and A-line separate clays from silts.
  4. Field tests identify fine soils quickly; AASHTO and group index serve highway work.

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