ASTM D2217 Soil Size Analysis & Determination of Soil Constants

ASTM D 2217 procedure entails wetting down soil samples that have been collected in the field to prepare them for particle-size analysis and soil constant determination.

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    ASTM D2217 Soil Size Analysis & Determination of Soil Constants

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    • Overview
    • Scope, Applications, and Benefits
    • Test Process
    • Specifications
    • Instrumentation
    • Results and Deliverables

    Overview

    ASTM D2217 describes procedures for wet preparation of soil samples before mechanical sieve analysis and hydrometer testing. Proper sample preparation is essential to ensure that particle aggregates are broken down without destroying individual particles, allowing accurate size analysis of fine-grained soils such as silts and clays.

    The method involves dispersing the soil in water using a dispersing agent and mechanical agitation, then washing the material through a 75 µm (No. 200) sieve to remove fines before the coarse fraction is dried and sieved. The fine fraction that passes the 75 µm sieve is used in subsequent hydrometer analysis. The soil constants (Atterberg limits) can also be determined in conjunction with this preparation to fully characterize the engineering behaviour of fine-grained soils.

    Scope, Applications, and Benefits

    Scope

    ASTM D2217 covers:

    • Wet preparation of soil samples for particle size analysis
    • Dispersal of cohesive fine-grained soils
    • Separation of coarse and fine fractions for analysis
    • Preparation for subsequent hydrometer testing
    • Determination of soil classification constants
    • Sample conditioning for engineering index property testing

    Applications

    • Geotechnical site investigation
    • Foundation design and evaluation
    • Soil classification for construction projects
    • Pavement subgrade characterization
    • Earthwork quality control
    • Environmental remediation soil assessment
    • Retaining wall and slope stability studies

    Benefits

    • Enables accurate particle size analysis of fine soils
    • Prevents misclassification from undispersed aggregates
    • Supports geotechnical design decisions
    • Provides data for USCS and AASHTO soil classification
    • Reduces testing errors from improper sample preparation
    • Facilitates consistent results across laboratories

    Test Process

    Sample Preparation

    Soil sample is broken down using water and a sodium hexametaphosphate dispersing agent.

    1

    Agitation

    Sample is mixed using a mechanical stirrer for the prescribed period.

    2

    Wet Sieving

    The dispersed slurry is washed through a 75 µm sieve; fines are collected for hydrometer analysis.

    3

    Drying & Sieving

    Coarse fraction retained on the 75 µm sieve is oven-dried and subjected to dry sieve analysis.

    4

    Technical Specifications

    ParameterDetails
    Applicable MaterialsNatural soils, silts, clays, mixed soil samples
    Specimen TypesField-collected soil samples
    Key Separation SievesNo. 10 (2.00 mm) / No. 40 (425 µm)
    Drying TemperatureMax. 60°C (140°F)
    Test EnvironmentControlled laboratory conditions
    Measured PropertyParticle-size distribution and soil constants

    Instrumentation Used for Testing

    • Mechanical stirrer/mixer
    • Calibrated test sieves (various sizes)
    • Oven for drying
    • Analytical balance
    • Hydrometer apparatus (for fine fraction)
    • Dispersing agent (sodium hexametaphosphate)

    Results and Deliverables

    • Particle size distribution curve
    • Percent fines (passing No. 200 sieve)
    • Coarse fraction sieve analysis data
    • Soil classification (USCS/AASHTO basis)
    • Geotechnical investigation reports

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    Frequently Asked Questions

    It is used for wet preparation of soil samples before conducting particle-size distribution and soil constant tests.

    The prepared sample is used for grain size analysis, liquid limit, plastic limit, and other soil constants.

    It is suitable for natural soils, fine-grained soils, silts, clays, and mixed soil samples.

    Wet preparation helps separate cohesive fines from coarse particles without altering the soil structure.

    The standard was withdrawn in 2007, but it may still be cited in older geotechnical reports and project documents.

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