Actes du colloque - Volume 1 - page 567

586
Proceedings of the 18
th
International Conference on Soil Mechanics and Geotechnical Engineering, Paris 2013
Group 3
G
0
= 41,20
q
t
+ 0,37
G
v0
+ 0,88 OCR – 28,53
(9)
Figure. 9. Relationship between shear modulus G
0
DMT
and G
0
CPTU
Figure 10. Relationship between measured G
0
DMT
and G
0
CPTU
after the
calibration.
Figure 11. The model of subsoil stiffness calculated on the G
0
values
from CPTU, calibrated by SDMT results.
In order to obtain a continuous picture of changes in the shear
modulus G
0
the dependence of G
0
CPTU
was calibrated using
measured values of G
0
DMT
(Fig. 10). Moduli G
0
CPTU
determined
from this relationship may be used in the construction of a
model of rigidity for the subsoil composed of soils of varied
genesis. An example of such a model for the foundation of a
wind turbine is presented in Fig. 11. The model was constructed
using Inverse Distance Weighting Method (IDW) according to
Młynarek et al. (2007).
5
CONCLUDING REMARKS
On the basis of the conducted investigations it may be
concluded that the simultaneous use of CPTU and SDMT
provides a continuous picture of changes in rigidity of subsoil
composed of soils with diverse genesis. The effectiveness of
these methods is emphasized by the high statistical evaluation
for the dependence between deformation and shear strength
moduli from both tests. However, to determine this dependence
it is necessary to apply a calibration function. The calibration
function needs to be specified for the soils, which should be
grouped depending on their grain size, since this variable also
influences relationships between parameters measured in CPTU
and SDMT.
After calibration this relationship may be a useful tool in the
construction of a model for rigidity of subsoil based on shear
strength moduli G
0
or M
0
moduli.
6
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