Geoscience Reference
In-Depth Information
Creep settlement (also called secondary compression) occurs as a change of
structure occurs.
Table 23.2 Types of movements.
Principal soil types
Type of movements
Immediate
Consolidation
Creep
Swell
Rock
Yes
No
No
Some
Gravels
Yes
No
No
No
Sands
Yes
No
No
No
Silts
Yes
Minor
No
Minor
Clays
Yes
Yes
Yes
Yes
Organic
Yes
Minor
Yes
Minor
Immediate and consolidation settlements are dependent on the applied load and
the foundation size.
Self weight settlement can also occur for fill constructed of the above materials.
The settlement will depend on the material type, level of compaction and height
of the fill.
23.3 Immediate to total settlements
The settlement estimates are usually based on the settlement parameters from the
oedometer test.
This is mainly for consolidation settlements, but may also be applied to elastic
settlements for overconsolidated soils.
For stiff elastic soils, a factor of safety of 2.5 is assumed.
Secondary settlement is neglected in this table. Saturated soil is assumed.
Table 23.3 Immediate, consolidation and total settlement ratio estimates (after Burland et al., 1978).
Type of soil
Immediate settlement,
Consolidation
Total settlement
Ratio
(undrained)
settlement
u /
ρ
ρ
ρ
= ρ
+ ρ
ρ
ρ
u
c
T
u
c
T
Soft yielding
0.1
1.1
10-15%
ρ
ρ
ρ
<
oed
oed
oed
Stiff elastic
0.6
0.4
33-67%
ρ
ρ
ρ
oed
oed
oed
ρ u / ρ T
70% for deep layers of overconsolidated clays.
ρ u / ρ T
25% for decreasing thickness of layer and increasing non homogeneity
and anisotropy.
23.4 Consolidation settlements
One - dimensional settlements
= ρ od
= ρ oed from the odeometer test
(refer
chapter 11).
 
 
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