Geoscience Reference
In-Depth Information
Table 11.2. Computation algorithm for the degraded bearing capacity and the seismic settlements
of strip foundations restingon the surface ofa clay crustover liquefiable subsoil
Design Requirements
FS deg FS o ( = 1 . 0 1 . 5 )
ρ = ρ st + ρ dyn ρ all
Degraded (end of shaking) Static Factor of Safety
FS deg = min 5 . 14 C u / q
FS c s
deg
1
2 γ BN
γ + γ HN q B
2 C u H γ HB +
FS c s
deg
=
qB
φ = tan 1 [ ( 1 U ) tan φ o ]
U = 0 . 50 1 + a
σ v o
σ vo + ∆ σ v
a = 1 250 ρ dyn
B
2 . 0
Seismic Settlements
1
FS c s
deg
2 . 50
ρ dyn = ρ o ·
a max T 2 Z liq · N
ρ o = 0 . 016 ·
Symbols
q = average contact pressure offooting
T
= predominant excitation period
ρ st = static settlement corresponding to q
N = number of cycles corresponding to a max
B = width of footing
Z liq = thickness of liquefiedsubsoil
σ vo = verticaleffectivegeostaticstressatdepth
equal to B below the soil crust
H = thickness of soil crust
γ = buoyant unit weight of subsoil (soil crust
and liquefiable soil)
σ v = additional vertical stress caused by sta-
tic loading (e.g. q ) at the same depth, on the
footing axis
ϕ o = friction angle of liquefiable soil (before
shaking)
N γ
, N q =
staticbearingcapacityfactorsforthe
liquefiedsoil(forthedegradedfrictionangle
)
a max = (effective)seismicgroundacceleration,
at the base of the liquefiable soil layer
ϕ
To provide insight to the beneficial effect of the clay crust, Figure 11.24 shows the
variation of seismic settlements and degraded factors of safety against the non-
dimensional thickness of the clay crust H
/
B , for a typical strip foundation with
=
.
=
B
3
0m, undrained shear strength of the clay C u
40kPa and the two different
 
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