Geoscience Reference
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Table 3 Anisotropic Model
Parameters for Strata 1 and 2
Parameters
Values
l
0.36
k
0.04
n
0.20
M c (M e )
1.20 (1.02)
R
3.4
C
0.4
s
2.0
C 1
5.0
C 2
1.0
C 3
5.0
W
2.0
A 0
1.0
adopted in the two-dimensional plane strain analysis are summarized in Table 4.
This equivalent model produced results within 5% error with the actual
axisymmetric idealization at 90, 180, and 360 days after load application (20 kPa
as step loading at t
0). The sand layer and dike fill were assigned a relatively
high coefficient of permeability—namely 200m/day—to simulate free drainage.
The initial stress states for the several soil layers in the underlying strata
were calculated using the given unit weights for saturated soils (see Fig. 2 ) , the
thickness of the layers and coefficient of earth pressure at rest K 0 , which was
assumed as 0.6 for all clay layers.
For the purpose of comparison of the proposed model with the isotropic
bounding surface model of Kaliakin and Dafalias (1990a,b), a finite-element
analysis was also conducted by assuming the clays to be isotropic and time-
independent by taking the material constant A 0 to be 0.0. Table 5 summarizes the
parameters for above two cases of analysis.
¼
Table 4 Coefficients of Permeability of Foundation
Coefficient of
permeability
( £ 10 2 3 m/day)
Strata 1
Strata 2A
With drains
No drains With drains
No drains
Strata 2B
Vertical
3.8
3.8
3.8
3.8
0.61
Horizontal
4.2
1.7
4.2
1.7
0.61
 
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