Environmental Engineering Reference
In-Depth Information
0.35
0.3
Posterior f μ ′′ φ )
0.25
Likelihood L φ )
0.2
Prior f μ φ )
0.15
0.1
0.05
0
10
15
20
25
30
35
40
45
50
μ φ (°)
Figure 5.2 Prior PDF of the mean friction angle, likelihood function describing the joint samples, and pos-
terior PDF of the mean friction angle. The likelihood function is scaled by [
µ ϕϕ 1
L
()
d
]
.
The difficulty in Bayesian updating stems from the need to compute the integral
X d Analytical solutions are available only for special cases, namely
for the so-called conjugate priors as discussed in Section 5.3.4. Efficient numerical integra-
tion using quadrature rules, as implemented in standard mathematical software, is appli-
cable only when the number of random variables in X is small, in the order of 3. For most
realistic problems, tailor-made numerical methods are required to solve the Bayesian updat-
ing problem. The most popular among these is the family of Markov chain Monte Carlo
(MCMC) methods, which allow sampling directly from ′′
Pr()
Z
=
L
() () .
xxx
f
−∞
f X without determining the con-
stant a, but many alternative methods have been proposed. Methods for the numerical solu-
tion are presented in Section 5.4.
Ultimately, the goal of the analysis is to make predictions on the performance of the geo-
technical system and, sometimes, on individual parameters of the model. In case the interest
is in the performance expressed through one or more failure events F , the prediction is in
terms of the updated Pr( F|Z ). This can be obtained through direct application of Equations
5.1 or 5.2 , which is the preferred approach for many problems and which is presented later
in Section 5.3.5. Alternatively, it is possible to first update the probability distribution of
the model parameters X to ′′
f X following Equation 5.3 and then perform a probabilistic reli-
ability analysis with ′′
f X . This approach is illustrated in the following.
illustration 2: Bayesian updating of the geotechnical reliability
We compute the reliability of a centrically loaded square footing with dimensions l = 3 m
and t = 1 m, illustrated in Figure 5.3. This example is modified from Oberguggenberger and
Fellin (2002). The footing will be in the silty soil described in Illustration 1, with a mean
friction angle μ φ and cohesion c = 0.
 
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