soilclassification-sivakugan.ppt
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SoilClassification-Sivakugan.pptTRANSCRIPT
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Soil ClassificationN. SivakuganDuration: 7 min. 20 s
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ObjectivesTo develop a systematic way to describe and classify soils;
To assign symbols.
To group soils of similar geotechnical characteristics; and
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Major Soil Groups
Grain size (mm)BoulderClaySiltSandGravelCobbleFine grain soilsCoarse grain soilsGranular soils or Cohesionless soilsCohesive soils
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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:
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Grain Size DistributionIn coarse grain soils ... By sieve analysis
Determination of GSD:In fine grain soils ... By hydrometer analysis
Hydrometer Analysis
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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
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Sheet1
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D
30
sieve
hydrometer
D10 = 0.013 mmD30 = 0.47 mmD60 = 7.4 mm
sands
gravels
fines
% Passing
Grain size (mm)
Sheet2
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Page &P
Sheet3
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Sheet4
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Sheet5
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Sheet6
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Sheet7
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Sheet8
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Sheet9
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Sheet10
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Sheet11
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Sheet12
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Sheet13
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Sheet14
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Sheet15
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Sheet16
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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
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Relative Density (Dr)
Measure of how densely the grains are packed in a coarse grain soil in %.
0100LoosestDensestAlso known as density index (ID).
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Granular Soil Consistencies
As per AS1726 - 1993Relative Density (%)Consistency Term0-1515-3535-6565-8585-100Very looseLooseMedium denseDenseVery dense
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Atterberg Limits
Border line water contents, separating the different states of a fine grained soil
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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
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Summary
Sieve analysis for coarse grain soils Hydrometer analysis - for fine grain soils
Classifycoarse by GSD and
fines from Atterberg limits (PI-LL chart).