Geoscience Reference
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This may vary depending on the depth of the effective overburden and type of
coarse grained material.
Table 5.16 Preliminary sand strength from cone penetration tests.
Relative density Dr (%)
Cone resistance, q c (MPa)
Typical
φ
V. Loose
D r
15
2.5
30
<
<
<
Loose
D r
=
15-35
2.5-5.0
30-35
Med dense
D r
35-65
5.0-10.0
35-40
=
Dense
D r
65-85
10.0-20.0
40-45
=
V. Dense
D r
>
85
>
20.0
>
45
The cone may reach refusal in very dense/cemented sands, depending on the thrust
of the rigs.
Rigs with the CPT pushed though its centre of gravity are usually expected to
penetrate stronger layers than CPTs pushed from the back of the rigs.
Portable CPT variations have less push although added flexibility for some difficult
to access sites.
5.17 Soil type from dilatometer test
The soil type can be determined from the material index parameter (I D ).
Table 5.17 Soil description from dilatometer testing (Marchetti, 1980).
I D
0.6
0.6 - 1.8
1.8
<
>
Material type
Clayey soils
Silty soils
Sandy soils
5.18 Lateral soil pressure from dilatometer test
The DMT can be used to determine the lateral stress.
Lateral stress coefficient K o
=
effective lateral stress/effective overburden stress.
Table 5.18 Lateral soil pressure from dilatometer test (Kulhawy and Mayne, 1990).
Type of clay
Empirical
Lateral stress coefficient K o
parameter
β
k
Formulae
2
5
10
15
Insensitive clays
1.5
(K D /1.5) 0 . 47 - 0.6
0.5
1.2
1.8
2.4
Sensitive clays
2.0
(K D /2.0) 0 . 47 - 0.6
0.4
0.9
1.5
N/A
Glacial till
3.0
(K D /3.0) 0 . 47 - 0.6
N/A
0.7
1.2
1.5
Fissured clays
0.9
(K D /0.9) 0 . 47 - 0.6
N/A
1.6
2.5
3.2
Lateral Stress index K D
=
(p o -u 0 )/
σ
vo .
K D
2 indicates a possible slip surface in slope stability investigations (Marchetti
et al, 1993).
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