Figure 4: Modification relationships between variation of f
c
/ P
a
and ’ values
Table 8: Modification of Terzaghi et al (1996)
Terzaghi et al (1996)
Clayey layer of
Jakarta Central
c
u
/P
a
Range of
0.1 1.00 0.83 – 1.21
0.2 0.92 0.76 – 1.11
0.3 0.82 0.68 – 0.99
0.4 0.74 0.61 – 0.90
0.6 0.62 0.51 – 0.75
0.8 0.54 0.45 – 0.65
1.0 0.48 0.40 – 0.58
1.2 0.42 0.35 – 0.51
1.4 0.40 0.33 – 0.48
1.6 0.38 0.31 – 0.46
1.8 0.36 0.30 – 0.44
2.0 0.35 0.29 – 0.42
2.4 0.34 0.28 – 0.41
2.8 0.34 0.28 – 0.41
Note: Pa = atmospheric pressure 100 kPa
4 CONCLUSIONS
Study analysis investigations have indicated that
unit skin friction (f) in determining frictional
resistance (Q
s
) on clayey layers of Jakarta Central
reaches about ± 17 to 18 percent of the previous
studies (Nottingham & Schmertmann, 1975;
Schmertman, 1978). This matter, it can be shown in
Figure 4 and Table 8, where and or ’ values on
each modification has a certain range of these values.
However, in application it should be considered with
vertical effective stress (’
o
) and the undrained
cohesion (c
u
) from laboratory data for undisturbed
sample.
These values obtained were within ranges established
by governmental authority regulations. Pile unit
friction (f) showed significant changes during
instalation for any time period. and or ’ values of
CPT data proved more sensitive than c
u
values
changes for determining frictional resistance during
the pilling. Losses of unit friction (f) can increase with
pore water pressure around pile shaft.
ACKNOWLEDGEMENTS
This work was supported by Tambora Consultant
Company for Deep Foundation System Designer;
Tribina Wahana Cipta for Soil Investigation of CPT
data; Geotesting Utama Engineering for PDA data;
and the Central BPJS Office as the project Owner.
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