Environmental Engineering Reference
In-Depth Information
Table 1.13 Mean, COV, and standard deviation for s u ,
σ p N, and q t σ v
Variable
μ
COV
σ
Undrained shear strength
s u
200 kPa
0.2
40 kPa
Preconsolidation stress
800 kPa
0.2
160 kPa
σ p
SPT blowcount
SPT-N value
20
0.3
6
Net cone tip resistance
2500 kPa
0.3
750 kPa
q t σ v
where μ's and σ's are the mean values and standard deviations, respectively, listed in Table
1.13 ; (X 1 , X 2 , X 3 , X 4 ) are individually standard normal. The mean values in Table 1.13 are
chosen such that s up
σ p P / /N0 (P a = 101.3 kPa is
the atmosphere pressure). These values are typical (e.g., Kulhawy and Mayne 1990). Let us
further assume the correlation matrix C for (X 1 , X 2 , X 3 , X 4 ) is
/
σ
′ ≈
0.
25
,(
q
σ
)
/
s
25
. ,
and (
)
.
t
v
u
1090507
09 10406
05 04 104
07 06 04
.
.
.
.
.
.
C =
(1.73)
.
.
.
.
.
.
1
Suppose site investigation yields the following information at a certain depth in a clay
layer: N = 10 and q t - σ v = 2000 kPa. On the basis of this information, the purpose is to
update the marginal distributions of s u and
σ p for the clay at the same depth. The uncon-
ditional distribution for s u is normal with mean = 200 kPa and COV = 0.2. The updated
(conditional) distribution for s u is expected to be different.
The effect of updating (or conditioning) can be explained by simulated data. A large
amount ( n = 2 × 10 6 ) of (, ,,
N − data are simulated. This can be done by first
simulating Z = normrnd(0, 1, n , 4). Then, the Cholesky factor is computed as u = chol( C ).
Finally, X T = Z T × u . The first column in X contains the X 1 samples; so, s u = μ 1 + σ 1 × X 1
will yield n = 2 × 10 6 samples of s u . The same procedure will yield n = 2 × 10 6 samples of ′
s
σ
q
σ
)
up
t
v
σ p
N, and q t - σ v . These samples are plotted as light-gray crosses in Figure 1.16 . It is clear that
( s u , N) are positively correlated, and so are ( s u , q t - σ v ). These are the unconditional samples
400
400
300
300
200
200
No info
100
100
No info
q t - σ v info
SPT-N info
Both info
Both info
0
0 0
0
10
20
N
30
40
2000
4000
6000
q t - σ v (kPa)
Figure 1.16 Illustration of conditioning using simulated ( s u , N, q t σ v ) samples.
 
 
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