Geoscience Reference
In-Depth Information
5.4 Clean sand strength from SPT data
The values vary from corrected to uncorrected N values and type of sand.
The SPT - value can be used to determine the degree of compactness of a cohesion-
less soil. However, it is the soil friction angle that is used as the strength parameter.
Table 5.4 Strength from SPT on clean medium size sands only.
Description
Relative
SPT - N (blows/300 mm)
Strength
density D r
Uncorrected field value
Corrected value
Friction angle
V. Loose
15%
N
4
(N o ) 60
3
28
<
φ <
Loose
15-35%
N
=
4-10
(N o ) 60
=
3-8
φ =
28-30
Med dense
35-65%
N
10-30
(N o ) 60
8-25
30-40
=
=
φ =
Dense
65-85%
N
=
30-50
(N o ) 60
=
25-42
φ =
40-45
V. Dense
85%
N
50
(N o ) 60
42
45 -50
>
>
>
φ =
100%
(N o ) 60
60
50
=
φ =
φ
by 5
Reduce
for clayey sand.
by 5
Increase
φ
for gravely sand.
5.5 Fine and coarse sand strength from SPT data
Fine sands have reduced values from the table above while coarse sand has an
increased strength value.
The corrected N value is used in the table below.
Table 5.5 Strength from corrected SPT value on clean fine and coarse size sands.
Description
Relative
Corrected SPT - N (blows/300 mm)
Strength
density D r
Fine sand
Medium
Coarse sand
V. Loose
<
15%
(N o ) 60
3
(N o ) 60
3
(N o ) 60
3
φ <
28
Loose
15-35%
(N o ) 60
3-7
(N o ) 60
3-8
(N o ) 60
3-8
28-30
=
=
=
φ =
Med dense
35-65%
(N o ) 60
7-23
(N o ) 60
8-25
(N o ) 60
8-27
30-40
=
=
=
φ =
Dense
65-85%
(N o ) 60
23-40
(N o ) 60
25-43
(N o ) 60
27-47
40-45
=
=
=
φ =
V. Dense
85%
(N o ) 60
40
(N o ) 60
43
(N o ) 60
47
45-50
>
>
>
>
φ =
100%
(N o ) 60
=
55
(N o ) 60
=
60
(N o ) 60
=
65
φ =
50
Above is based on Skempton (1988):
-(N o ) 60 /D r =
55 for Fine Sands.
-(N o ) 60 /D r
=
60 for Medium Sands.
-(N o ) 60 /D r =
65 for Coarse Sands.
5.6 Effect of aging
The SPT in recent fills and natural deposits should be interpreted differently.
Typically the usual correlations and interpretations are for natural materials. Fills
and remoulded samples should be assessed different.
 
 
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