Geoscience Reference
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Figure 6
Clod size distribution of the ready-for-use clay.
in which, c, fare the cohesion and internal friction angle of soil; l
i
is the length of
the slice base; W
i
is the self-weight of slice no. i; r
u
[
(u
i
b
i
/W
i
] is the pore
pressure ratio defined by Bishop (1955); u
i
is the pore pressure acting on
the base of slice no. i; T
i
is the reinforcement force (tension) acting on the base of
slice no. i.
A total of 12 cases was investigated. The input parameters and the
analytical results are summarized in
Table 4.
The predicted failure surfaces
for the aforementioned in-laboratory and in-situ soil specimens were used.
Note that in these cases the internal friction angles obtained in the triaxial
compression tests were multiplied by a factor of 1.1 to simulate the plane-
strain condition. In cases 3-A through 4-C, the cohesion of the clay was
neglected purposely.
Table 5
shows that the cohesion of the compacted clay
dominates the stability the clay wall. It also showed that using the tensile
strength at 10% of strain, that is, using F
T
¼
¼
3.3 on the ultimate strength
(T
i
¼
5.37 kN/m; see
Fig.3)
of the geogrid, or using a pore pressure ratio r
u
¼
0.1 yielded relatively small reduction in F
s
for cases 1-A through 2-C.
However, they yielded relatively large reductions for cases 3-A through 4-C
in which the cohesion of clay was not considered.
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