Environmental Engineering Reference
In-Depth Information
g
()
θ
=
[
]
−
n
PgZ
,
θ
<
0
P
∗
(11.8)
f
FS
According to its definition, the normalized limit state function, denoted by G(Z,θ), can be
expressed by
Equation 11.9.
θ=
[
Z
θ
θ
g
g
,]
()
GZ
(,)
(11.9)
n
And
Equation 11.7
can be rewritten as
Equation 11.10
.
g
()
θ
=
1
=
n
Pg
[,]
Z
θ
−
<
0
P
G
[,]
Z
θ
<
P
∗
(11.10)
f
FS
FS
This means that 1/FS is the (1 − Pf∗)
f
∗
) percentile of the random variable G. The relationship
between FS and P
f
∗
can be determined using Monte Carlo simulation, drawing N samples
from Z and θ, and calculating the N values for G(i)
(i)
= G(Z
(i)
,θ
(i)
). For a chosen FS value, the
1
N
1
FS
≡
∑
ˆ
P
*
≈
IG
(i)
<
P
∗
(11.11)
f
f
Further details and discussion on this method can be found in the referenced paper
(Ching, 2009). The premise that the distribution of G(Z,θ) is invariant over the entire allow-
able design region D can be achieved only if the correct nominal limit state function g
n
(θ) is
found, which is usually a difficult undertaking, although finding a nominal limit state func-
tion for which the premise holds approximately is relatively simple, since g
n
(θ) = g(E(Z),θ) is
usually an acceptable choice.
It is important to note that for certain geotechnical problems, the FS can be defined in dif-
ferent ways. For instance, in shear problems (slope stability, sliding of a dam along its foun-
dation contact), the FS can be defined as the ratio between strength and stress, or resistance,
R, and loading, L. This is the case if limit equilibrium models are used (
Equation 11.12
)
.
R
L
(11.12)
FS
=
On the other hand, it is common that if finite-element models are used, the FS is defined
as the ratio between a value of a strength parameter, φ, and the ultimate value before failure,
ϕ
FS
=
(11.13)
ϕ
failure
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