soilclassification-sivakugan.ppt

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1 Soil Classification N. Sivakugan Duration: 7 min. 20 s

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  • Soil ClassificationN. SivakuganDuration: 7 min. 20 s

    SIVACopyright 2001

    ObjectivesTo develop a systematic way to describe and classify soils;

    To assign symbols.

    To group soils of similar geotechnical characteristics; and

    SIVACopyright 2001

    Major Soil Groups

    Grain size (mm)BoulderClaySiltSandGravelCobbleFine grain soilsCoarse grain soilsGranular soils or Cohesionless soilsCohesive soils

    SIVACopyright 2001

    Grain Size DistributionTo know the relative proportions of different grain sizes.

    An important factor influencing the geotechnical characteristics of a coarse grain soil.

    Not important in fine grain soils.

    Significance of GSD:

    SIVACopyright 2001

    Grain Size DistributionIn coarse grain soils ... By sieve analysis

    Determination of GSD:In fine grain soils ... By hydrometer analysis

    Hydrometer Analysis

    SIVACopyright 2001

    Grain Size Distribution Curvecan find % of gravels, sands, fines

    define D10, D30, D60.. as above.

    Chart2

    0

    19.2

    37

    63.5

    70

    75.5

    81.5

    87.3

    100

    D

    30

    sieve

    hydrometer

    D10 = 0.013 mmD30 = 0.47 mmD60 = 7.4 mm

    sands

    gravels

    fines

    % Passing

    Grain size (mm)

    Sheet1

    0.0010

    0.119.2

    137

    1063.5

    1570

    2075.5

    2581.5

    3087.3

    37.5100

    &A

    Page &P

    Sheet1

    &A

    Page &P

    D

    30

    sieve

    hydrometer

    D10 = 0.013 mmD30 = 0.47 mmD60 = 7.4 mm

    sands

    gravels

    fines

    % Passing

    Grain size (mm)

    Sheet2

    &A

    Page &P

    Sheet3

    &A

    Page &P

    Sheet4

    &A

    Page &P

    Sheet5

    &A

    Page &P

    Sheet6

    &A

    Page &P

    Sheet7

    &A

    Page &P

    Sheet8

    &A

    Page &P

    Sheet9

    &A

    Page &P

    Sheet10

    &A

    Page &P

    Sheet11

    &A

    Page &P

    Sheet12

    &A

    Page &P

    Sheet13

    &A

    Page &P

    Sheet14

    &A

    Page &P

    Sheet15

    &A

    Page &P

    Sheet16

    &A

    Page &P

    SIVACopyright 2001

    Well or Poorly Graded Soils

    Well Graded SoilsPoorly Graded SoilsWide range of grain sizes presentGravels: Cc = 1-3 & Cu >4Sands: Cc = 1-3 & Cu >6Others, including two special cases:(a) Uniform soils grains of same size(b) Gap graded soils no grains in a specific size range

    SIVACopyright 2001

    Relative Density (Dr)

    Measure of how densely the grains are packed in a coarse grain soil in %.

    0100LoosestDensestAlso known as density index (ID).

    SIVACopyright 2001

    Granular Soil Consistencies

    As per AS1726 - 1993Relative Density (%)Consistency Term0-1515-3535-6565-8585-100Very looseLooseMedium denseDenseVery dense

    SIVACopyright 2001

    Atterberg Limits

    Border line water contents, separating the different states of a fine grained soil

    SIVACopyright 2001

    Atterberg Limits

    Liquid Limit (wL or LL):Clay flows like liquid when w > LLPlastic Limit (wP or PL):Lowest water content where the clay is still plasticShrinkage Limit (wS or SL):At w 50I = 35 < LL < 50L = LL < 35XAe.g., GPYBe.g., CHXYe.g., SMXA-XYe.g., GP-GC

    SIVACopyright 2001

    Summary

    Sieve analysis for coarse grain soils Hydrometer analysis - for fine grain soils

    Classifycoarse by GSD and

    fines from Atterberg limits (PI-LL chart).