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Soil Classification

On this page · 6 sections
  1. The AASHTO System
  2. The Unified Soil Classification System
  3. Visual Description in the Field
  4. Calculator
  5. Comparing the Two Systems
  6. Standard Test Methods

Soil classification sorts soils into groups that behave alike, so that a designer or inspector can predict how a soil will act from a few simple tests. Two systems are used on U.S. highway work:

  • the AASHTO system (AASHTO M 145), written for highway subgrades and embankments, and
  • the Unified Soil Classification System (USCS, ASTM D2487), used in geotechnical and foundation work.

Both start from the same two pieces of information: the soil's gradation from a sieve analysis, and its plasticity from the liquid limit and plasticity index, together called the Atterberg limits. Neither system measures strength or stiffness directly. A classification tells you what kind of soil you have; tests such as the California Bearing Ratio or resilient modulus tell you how well it supports a pavement (Christopher et al., 20061).

Basic soil terms (gravel, sand, silt, clay) are defined in AASHTO Soil Terminology and ASTM Aggregate and Soil Terminology. The two systems draw the gravel–sand boundary at different sieves, so a soil's description can change slightly between them.

The AASHTO System

The AASHTO system places a soil in one of seven main groups, A-1 through A-7, several with subgroups. The first split is on the amount of material passing the 0.075 mm (No. 200) sieve:

  • Granular materials have 35 percent or less passing the 0.075 mm sieve. They are groups A-1, A-3 and A-2.
  • Silt–clay materials have more than 35 percent passing. They are groups A-4 through A-7.

Within each half, the liquid limit and plasticity index decide the group. The limits below follow the FHWA soils reference manual (Samtani and Nowatzki, 20062). To classify a soil, work from left to right through the groups and take the first one whose limits the soil meets.

Table 1. AASHTO soil classification limits (after Samtani and Nowatzki, 20062)

GroupPassing 2.00 mm (No. 10), %Passing 0.425 mm (No. 40), %Passing 0.075 mm (No. 200), %Liquid limitPlasticity indexTypical material
A-1-a50 max30 max15 max—6 maxStone fragments, gravel and sand
A-1-b—50 max25 max—6 maxGravel and sand
A-3—51 min10 max—NonplasticFine sand
A-2-4, A-2-5——35 max40 max / 41 min10 maxSilty gravel and sand
A-2-6, A-2-7——35 max40 max / 41 min11 minClayey gravel and sand
A-4——36 min40 max10 maxSilty soils
A-5——36 min41 min10 maxSilty soils
A-6——36 min40 max11 minClayey soils
A-7-5, A-7-6——36 min41 min11 minClayey soils

A-7 soils split on how the plasticity index compares with the liquid limit: A-7-5 has a plasticity index no greater than the liquid limit minus 30, and A-7-6 has a plasticity index greater than that. A-7-5 soils tend to be elastic silty clays that rebound under load; A-7-6 soils are the highly plastic clays that shrink and swell most (see Shrinking and Swelling Soils).

In general, the further a soil sits to the right of the chart, the poorer it is as a subgrade. A-1 and A-3 soils are usually rated excellent to good; A-4 through A-7 soils are usually rated fair to poor.

Group Index

The group index refines the rating within a group. It is an empirical number that rises as the fines content and plasticity rise:

GI=(F−35)[0.2+0.005(LL−40)]+0.01(F−15)(PI−10)GI = (F - 35)\left[0.2 + 0.005(LL - 40)\right] + 0.01(F - 15)(PI - 10)

where:

  • GIGI = group index, rounded to the nearest whole number
  • FF = percent passing the 0.075 mm (No. 200) sieve
  • LLLL = liquid limit
  • PIPI = plasticity index

Each bracketed term is set to zero when it would be negative, and a negative group index is reported as zero. For the A-2-6 and A-2-7 subgroups only the plasticity-index term is used. The group index is written in parentheses after the group, for example A-6(12). A group index of 0 marks a good subgrade within its group; values of 20 or more mark a very poor one (Samtani and Nowatzki, 20062).

The Unified Soil Classification System

The USCS gives each soil a two-letter symbol. The first letter names the main soil type and the second describes it:

  • G gravel, S sand, M silt, C clay, O organic, Pt peat
  • W well graded, P poorly graded, L low plasticity, H high plasticity

A soil is coarse grained when more than half of it is retained on the 0.075 mm (No. 200) sieve. It is a gravel when more than half of that coarse fraction is retained on the 4.75 mm (No. 4) sieve, and a sand otherwise. What follows depends on the fines:

  • Less than 5 percent fines: the second letter comes from the shape of the gradation curve (W or P), using the coefficients of uniformity and curvature below.
  • More than 12 percent fines: the second letter comes from the plasticity of the fines (M or C), read from the plasticity chart.
  • 5 to 12 percent fines: the soil gets a dual symbol, such as SW-SM.
Cu=D60D10Cc=(D30)2D10 D60C_u = \frac{D_{60}}{D_{10}} \qquad C_c = \frac{(D_{30})^2}{D_{10}\,D_{60}}

where:

  • CuC_u = coefficient of uniformity
  • CcC_c = coefficient of curvature
  • D10,D30,D60D_{10}, D_{30}, D_{60} = particle sizes at which 10, 30 and 60 percent of the sample passes

A gravel is well graded (GW) when CuC_u is at least 4 and CcC_c is between 1 and 3; a sand (SW) needs CuC_u of at least 6 with the same CcC_c range (Samtani and Nowatzki, 20062).

A soil is fine grained when half or more passes the 0.075 mm sieve. Its symbol comes from the plasticity chart, a plot of plasticity index against liquid limit. The "A-line" on that chart separates clays (above) from silts (below):

PI=0.73 (LL−20)PI = 0.73\,(LL - 20)

A liquid limit below 50 gives L (low plasticity) and 50 or more gives H (high plasticity), so the four common fine-grained groups are CL, ML, CH and MH. A small zone just above the A-line at low plasticity (a plasticity index of about 4 to 7) is given the dual symbol CL-ML.

Visual Description in the Field

Laboratory classification takes a day or more. In the field, inspectors describe soils by eye and feel using the visual-manual procedure (ASTM D2488): estimating the percentages of gravel, sand and fines, and judging dry strength, dilatancy and toughness by hand. A visual description is useful for logging test pits and spotting a change in material, but it is not a substitute for laboratory classification when a specification or design depends on the group (Samtani and Nowatzki, 20062).

Calculator

Soil classification (AASHTO and USCS)

AASHTO M 145 · ASTM D2487

Classifies the material finer than 75 mm (3 in.) from its sieve analysis and Atterberg limits.

Percent passing
Atterberg limits (minus No. 40 fraction)

Optional for a nonplastic soil that is mostly coarse.

Grain sizes (for coarse soils with little fines)

Needed only when 12 % or less passes the No. 200 sieve.

Example values: a sandy lean clay. Rules follow FHWA NHI-06-088, chapter 4.

Comparing the Two Systems

The two systems often agree in broad terms but not group for group. A soil with 40 percent fines is an A-4 to A-7 "silt–clay" under AASHTO, but still a coarse-grained SM or SC under USCS, because the USCS split is at 50 percent fines rather than 35. Specifications usually name the system they mean; when a project report gives only one, don't convert between them without the underlying gradation and limits.

Standard Test Methods

  • AASHTO M 145: Classification of soils and soil–aggregate mixtures for highway construction
  • ASTM D2487: Classification of soils for engineering purposes (Unified Soil Classification System)
  • ASTM D2488: Description and identification of soils by the visual-manual procedure
  • AASHTO T 88, T 89 and T 90: particle-size analysis, liquid limit and plastic limit of soils

Teaching this? Figures and worked examples are free to use with credit. Course reading lists

Cite this page

APA

Pavement Interactive. (2026, November 1). Soil classification. HeadLight. Retrieved [the date you read it], from https://pavementinteractive.org/reference-desk/testing/soil-tests/soil-classification/

ASCE

Pavement Interactive. (2026). “Soil Classification.” HeadLight, <https://pavementinteractive.org/reference-desk/testing/soil-tests/soil-classification/> ([the date you read it]).

BibTeX

@misc{pavint-soil-classification,
  author = {{Pavement Interactive}},
  title = {Soil Classification},
  year = {2026},
  publisher = {HeadLight},
  howpublished = {\url{https://pavementinteractive.org/reference-desk/testing/soil-tests/soil-classification/}},
  note = {Accessed [date]}
}
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Sources (2)
  1. Christopher, B.R.; Schwartz, C. and Boudreau, R. (2006). Geotechnical Aspects of Pavements Reference Manual. FHWA-NHI-05-037. National Highway Institute, Federal Highway Administration. Washington, D.C. www.fhwa.dot.gov/engineering/geotech/pubs/05037/05037.pdf ↩
  2. Samtani, N.C. and Nowatzki, E.A. (2006). Soils and Foundations Reference Manual, Volume I. FHWA-NHI-06-088. National Highway Institute, Federal Highway Administration. Washington, D.C. www.fhwa.dot.gov/engineering/geotech/pubs/nhi06088.pdf ↩ ↩ ↩ ↩ ↩
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