Soil Classification USCS AASHTO Calculator
Classify soil using both USCS and AASHTO systems from grain size distribution and Atterberg limits.
Soil Classification USCS AASHTO Calculator
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Formula: USCS: Based on grain size (>50% coarse or fine) + Atterberg limits. AASHTO: GI = (F-35)[0.2+0.005(LL-40)] + 0.01(F-15)(PI-10)
Worked example โ USCS: SC (Clayey sand), AASHTO: A-2-6
Formula
USCS: Based on grain size (>50% coarse or fine) + Atterberg limits. AASHTO: GI = (F-35)[0.2+0.005(LL-40)] + 0.01(F-15)(PI-10)
The USCS first divides soils by the percentage passing the No. 200 sieve (75 micron). Coarse-grained soils are further split by gravel vs sand predominance and fines character. Fine-grained soils are classified on the plasticity chart using the A-line equation PI = 0.73(LL-20). The AASHTO Group Index is a weighted function of fines content, liquid limit, and plasticity index that rates subgrade quality from 0 (excellent) to 20 (very poor).
Worked Examples
Example 1: Silty Sand Classification
Problem:Classify a soil with 15% gravel, 55% sand, 30% fines, LL = 35, PI = 12.
Solution:Fines < 50%, so coarse-grained Sand > Gravel, so sand group Fines > 12%, PI > 7: Clayey sand USCS: SC AASHTO: Fines = 30%, LL = 35, PI = 12 Group A-2-6 (clayey sand)
Result:USCS: SC (Clayey sand), AASHTO: A-2-6
Example 2: High Plasticity Clay
Problem:Classify a soil with 5% gravel, 10% sand, 85% fines, LL = 65, PI = 40.
Solution:Fines > 50%: fine-grained soil LL > 50: high plasticity PI = 40 > 0.73*(65-20) = 32.85: above A-line USCS: CH (Fat clay) AASHTO: A-7 with high Group Index
Result:USCS: CH (Fat clay), AASHTO: A-7
Frequently Asked Questions
What is the USCS soil classification system?
The Unified Soil Classification System (USCS) was developed by Arthur Casagrande in the 1940s and standardized as ASTM D2487. It classifies soils into groups based on grain size distribution and Atterberg limits. Coarse-grained soils (more than 50 percent retained on the No. 200 sieve) are subdivided into gravels (G) and sands (S), then further by gradation (W for well-graded, P for poorly-graded) or fines type (M for silt, C for clay). Fine-grained soils (more than 50 percent passing the No. 200 sieve) are classified by the Casagrande plasticity chart into clays (C), silts (M), and organics (O) with low (L) or high (H) plasticity.
How does the AASHTO classification system differ from USCS?
The AASHTO system was developed specifically for highway and pavement engineering by the American Association of State Highway and Transportation Officials. It classifies soils into groups A-1 through A-7, with A-1 being the best subgrade material and A-7 the worst. It uses a Group Index (GI) that combines fines content, liquid limit, and plasticity index into a single number indicating suitability as pavement subgrade. Lower GI values indicate better performance. Unlike USCS which focuses on engineering behavior, AASHTO is optimized for predicting road subgrade quality.
What is the Casagrande plasticity chart and how is it used?
The plasticity chart plots the plasticity index (PI) on the vertical axis against the liquid limit (LL) on the horizontal axis. The A-line, defined by PI = 0.73(LL - 20), separates clays (above the line) from silts (below the line). The U-line, PI = 0.9(LL - 8), represents the approximate upper bound for natural soils. Soils plotting to the left of LL = 50 are low plasticity (L suffix), while those to the right are high plasticity (H suffix). This chart is the primary tool for classifying fine-grained soils and provides insight into compressibility and swelling potential.
Why is soil classification important for engineering projects?
Soil classification provides a standardized language for engineers to communicate soil properties and expected behavior without detailed testing at every location. It helps predict drainage characteristics, bearing capacity, settlement potential, and suitability as construction material. For example, well-graded gravels (GW) make excellent foundation and road base material, while high-plasticity clays (CH) are problematic due to high compressibility and swelling. Classification guides preliminary design decisions, helps estimate construction costs, and determines what additional testing is needed for detailed analysis.
What exactly are the liquid limit, plastic limit and plasticity index?
They are water contents, expressed as a percentage of dry mass, that bound the range over which a fine soil behaves plastically. The liquid limit is the water content at which a groove cut in a soil pat in the Casagrande cup closes over 13 mm after 25 blows. The plastic limit is the water content at which a thread rolled to about 3 mm diameter just crumbles. The plasticity index is simply LL minus PL, the width of the plastic range, and it is the vertical axis of the classification chart.
How are the coefficients of uniformity and curvature used to tell well-graded from poorly graded?
Cu = D60 / D10 measures how wide the particle size spread is, and Cc = (D30 squared) / (D10 x D60) checks that the distribution has no gap. Under ASTM D2487 a clean gravel earns the W suffix when Cu is at least 4 with Cc between 1 and 3, while a clean sand needs Cu of at least 6 with the same Cc window. Failing either test makes the soil poorly graded, symbol P. Well-graded material compacts to higher density because small grains fill the voids between larger ones.
When does a soil get a dual symbol such as SW-SM?
Coarse-grained soils with fines between 5 and 12 percent fall in a deliberate transition band where neither the gradation criteria nor the fines character can be ignored, so both are reported: the first symbol records gradation and the second the type of fines, giving GW-GM, GP-GC, SW-SC and similar. A second dual case is the CL-ML zone on the plasticity chart, where the plasticity index sits between 4 and 7 and above the A-line. Dual symbols warn that ordinary test scatter could push the soil either way.
Which sieves define the gravel, sand and fines fractions?
The No. 200 sieve, with 75 micrometre openings, is the boundary between fines and coarse material and sets the 50 percent split that starts the whole USCS decision. Within the coarse fraction, the No. 4 sieve at 4.75 mm separates gravel above from sand below. Fines pass too readily to be dry sieved, so the sample is washed over the No. 200 sieve, and if the silt-clay split matters a hydrometer sedimentation analysis is run on the material finer than that.
How is an organic soil identified in the USCS?
Organic content is not measured by the grain size or plasticity inputs, so a separate check is used. The liquid limit is determined twice, once on the natural sample and once after oven drying at 110 degrees Celsius, and if the oven-dried value falls below 0.75 of the original the soil takes the O designation, giving OL or OH. Highly organic peat is classified separately as PT from its fibrous texture, dark colour and odour. Organic soils compress badly and are usually excavated rather than built on.
What does the AASHTO Group Index tell a pavement designer?
The Group Index condenses fines content, liquid limit and plasticity index into one subgrade penalty, rounded to the nearest whole number and written in parentheses after the group, as in A-6(12). Zero means the fines are neither abundant nor plastic enough to hurt support, while values approaching 20 indicate a soft, moisture-sensitive subgrade. Higher indices push the designer toward a thicker granular base, subgrade stabilisation with lime or cement, or removal and replacement, since the subgrade must carry the pavement year round.
References
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Reviewed for accuracy by Daniel Agrici, Founder & Lead Developer ยท Editorial policy
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