Geoscience Reference
In-Depth Information
10.4 Soil variability from laboratory testing
The density of soils can be accurately tested.
There is a high variability on the shear strength test results of clays and the Plasticity
Index.
Table 10.4 Variability from laboratory testing (Poon and Kulhawy, 1999).
Test
Property
Soil type
Coefficient of variation (%)
Range
Mean
Atterberg tests
Plasticity index
Fine grained
5-51
24
Triaxial compression
Effective angle of friction
Clay, silt
7-56
24
Direct shear
Shear strength, C u
Clay, silt
19-20
20
Triaxial compression
Shear strength, C u
Clay, silt
8-38
19
Direct shear
Effective angle of friction
Sand
13-14
14
Direct shear
Effective angle of friction
Clay
6-22
14
Direct shear
Effective angle of friction
Clay, silt
3-29
13
Atterberg tests
Plastic limit
Fine grained
7-18
10
Triaxial compression
Effective angle of friction
Sand, silt
2-22
8
Atterberg tests
Liquid limit
Fine grained
3-11
7
Unit weight
Density
Fine grained
1-2
1
Table 10.5 Guidelines for inherent soil variability (Poon and Kulhawy, 1999).
Test type
Property
Soil type
Coefficient of variation (%)
Range
Estimated mean
Lab strength
UC
Shear strength, C u
Clay
20-55
40
CIUC
20-40
30
UU
10-30
20
Lab strength
Effective angle of friction
Clay and sand
5-15
10
Standard penetration test
N-value
25-50
40
Pressuremeter test
P L
Clay
10-35
25
Sand
20-50
35
E PMT
Sand
15-65
40
Dilatometer
A
Clay
10-35
25
B
A
Sand
20-50
35
B
I D
Sand
20-60
40
K D
20-60
E D
15-65
Pressuremeter
P L
Clay
10-35
25
Sand
20-50
35
E PMT
Sand
15-65
40
Cone penetrometer test
q c
Clay
20-40
30
Sand
20-60
40
Vane shear test
Shear strength, C u
Clay
10-40
25
Lab index
Natural moisture content
Clay and silt
8-30
20
Liquid limit
6-30
Plastic limit
6-30
 
 
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