an investigation on the bulging phenomenon in the clay...
TRANSCRIPT
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Associate Professor, Civil Engineering Department
M. Sc. in Geotechnical Engineering, A
Ph. D. Student, Geotechnical Engineering, A
The Masjed Soleyman dam is a central clay core rockfill dam with the height of 177 meter and
490m long center core. Throughout the dam construction, reservoir impounding and operation
comprehensive monitoring had been
dam behavior was based on measurement data of instruments installed on the dam body and
foundation. This research present research
the first impounding and summarize
instruments are in the field of stresses
rotation of the principal stresses direction had been investigated. The rota
points were generally constant, but slight increases in the angles after full impoundment ha
observed in the downstream side of the core. This
would lead to bulging of the cor
permeability of the clay material, the dissipating process of the pore water pressure hadn’t been
continuing with notable progress (in the past 13 years after the first impounding). So the clay
behavior as an undrained material and volume change is not significant especially in the center
area of core. This is the main reason for developing the lateral deformation in the clay core which
called bulging.
Keywords: Rockfill dam, clay core,
1- INTRODUCTION
The Masjed Soleilman (MES
rockfill dam (Engineering Report of MES dam
power plant was commenced in December 1994 and the embankment of the main dam was
completed in November 2000. The reservoir impounding was
2000 and the reservoir water level reached at el. 371 m on July 2002.
the first impounding of dam reservoir can lead to changing of dam safety
the importance the monitoring after
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Bali, Indonesia, June 1ST
– 6TH
, 2014
the bulging phenomenon in the clay core of rockfill dam
based on the stress and pore water pressure data
Associate Professor, Civil Engineering Department, Ferdowsi University of Mashhad, Mashhad
in Geotechnical Engineering, Abpooy Consulting Engineers, Mashhad, Iran
Geotechnical Engineering, Abpooy Consulting Engineers, Mashhad, Iran
ABSTRACT The Masjed Soleyman dam is a central clay core rockfill dam with the height of 177 meter and
center core. Throughout the dam construction, reservoir impounding and operation
comprehensive monitoring had been carried out to verify the dam behavior. The monitoring of the
dam behavior was based on measurement data of instruments installed on the dam body and
This research present research presents an overall review of the dam behavior
summarizes the recorded measurement of major instruments. These
instruments are in the field of stresses and pore water pressure in the clay core. Also substantial
rotation of the principal stresses direction had been investigated. The rotating angles of respective
points were generally constant, but slight increases in the angles after full impoundment ha
observed in the downstream side of the core. This is an indicative of a progressing shear zone and
would lead to bulging of the core in the lower level. In the clay core due to the
permeability of the clay material, the dissipating process of the pore water pressure hadn’t been
continuing with notable progress (in the past 13 years after the first impounding). So the clay
avior as an undrained material and volume change is not significant especially in the center
area of core. This is the main reason for developing the lateral deformation in the clay core which
ockfill dam, clay core, Masjed Soleyman dam, bulging, pore water pressure
MES) dam is a 177 m high and 490 m long center core type
Engineering Report of MES dam, 1993). Construction of the dam
power plant was commenced in December 1994 and the embankment of the main dam was
completed in November 2000. The reservoir impounding was commenced on 19 December
2000 and the reservoir water level reached at el. 371 m on July 2002. Deformations due
first impounding of dam reservoir can lead to changing of dam safety, which implies
the monitoring after the first impounding (Soroush and Araei,
the bulging phenomenon in the clay core of rockfill dam
based on the stress and pore water pressure data
Mashhad, Iran
, Mashhad, Iran
, Mashhad, Iran
The Masjed Soleyman dam is a central clay core rockfill dam with the height of 177 meter and
center core. Throughout the dam construction, reservoir impounding and operation
carried out to verify the dam behavior. The monitoring of the
dam behavior was based on measurement data of instruments installed on the dam body and
overall review of the dam behavior during
of major instruments. These
and pore water pressure in the clay core. Also substantial
ting angles of respective
points were generally constant, but slight increases in the angles after full impoundment has been
indicative of a progressing shear zone and
due to the very low
permeability of the clay material, the dissipating process of the pore water pressure hadn’t been
continuing with notable progress (in the past 13 years after the first impounding). So the clay
avior as an undrained material and volume change is not significant especially in the center
area of core. This is the main reason for developing the lateral deformation in the clay core which
, pore water pressure.
) dam is a 177 m high and 490 m long center core type
dam body and
power plant was commenced in December 1994 and the embankment of the main dam was
ed on 19 December
Deformations due to
, which implies
, 2006).�
An investigation on the bulging phenomenon in the clay core of rockfill dam
based on the stress and pore water pressure data
J. Bolouri Bazaz
H. Gholami
M.T. Bolouri Bazaz
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Throughout the dam construction, reservoir impounding and operation comprehensive
monitoring had been carried out to verify the dam behavior so that stability and safety of
the dam were ensured (Engineering Report of MES dam, 1993). The monitoring of the
dam behavior was based on measurement data of instrument installed in the dam body and
foundation and geodetic survey results of the dam surface as well as daily visual
inspection.
Noticeable numbers of the instruments malfunctioned or damaged in the period of the
construction. It’s notable that, the surface settlement of the dam had been continuing and it
was still not evident that the settlement had gone into a stable state. The residual excess
pore pressure in the core was still high after 11 years from first impounding. Developed
excess pore water pressure in the clay core of zoned rockfill dams during the construction
period and first stage impounding, may lead to initiation or progression of hydraulic
fracturing. The ability to predict the development and dissipation of these pore pressures is
important in assessing the performance of such structures. This phenomenon also depended
on the arching effect status of the core zone due to difference in stiffness of materials.
(Maleki and far, 2004). In present study, the received data from stress and pore water
instruments (section 260) analysised to understand the dam’s deformation behavior. Also,
the graphs drew just for available data’ instrument. The symbols of instrument’s situation
are shown in table 1.
Table 1. Symbol of instrument’s situation
symbol Situation
U/C Upstream (in core)
CL Center of core
D/C Downstream (in core)
U/Filter Upstream (in filter)
D/Filter Downstream (in filter)
U/Shell Upstream (in shell)
D/Shell Downstream (in shell)
2- EARTH PRESSURE
The stress in dam body has been measured, using total pressure cells which are installed in
the core, downstream filter and downstream shell from the beginning of the embankment
(Figure 1.), The total pressure cells in the upstream side of the core and upstream filter
malfunctioning and data in these portions were not available.
Figure 1. Earth pressure gauges in one cluster
The Stress ratio was defined as a ratio of the actual vertical pressure to the apparent
pressure calculated from the embankment weight (γH) above the measuring point. The
Total pressure cell
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positions of the instrument that was workable are shown in table 2. Variation of the stress
ratio (σv/γH) at respective measuring section (CH. 260) are shown in figures 2 to 4. In these
graphs, RWL is the water level behind the dam. The stress ratio in the core was in a range
(0.6 -0.7) and that in the filter are (0.7-1.40). This phenomenon caused by arching in the
core zone.
Table 2. Situation of instrument in CH. 260
Instrument Elevation Situation
2103 230 CL
2104 230 D/C
2105 230 D/Filter
2107 230 D/S
2202 270 CL
2203 270 D/C
2304 310 D/C
2305 310 D/Filter
Figure 2.Vertical stress ratio at 230 elevation (CH. 260 m).
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Figure 3.Vertical stress ratio at 270 elevation (CH. 260 m).
Figure 4.Vertical stress ratio at 310 elevation (CH. 260 m).
Principle stresses in the dam body are calculated from the measurement data of the total
pressure cells at the respective measuring points. Variations of the effective stress paths in
the core expressed with relationship between 1 2( ) / 2p σ σ= + and 1 2( ) / 2q σ σ= − ,
together with the measured pore pressure (pu) in this equation '
up p p= − . The values are
shown in figure 5 to 7 which indicate a trace of Mohr’s stress circle peak. The strength
parameters in this failure criterion are soil cohesion and internal friction angle. The values
of them are 20 kN/m2 and 30° respectively. The points above the failure envelope show the
yielding condition.
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Figure 5. Effective stress path in (p'-q) space (Sec. 260, El. 230, Core CL)
Figure 6. Effective stress path in (p'-q) space (Sec, 260, EL230, Core D/S)
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Figure 7. Effective Stress Path in (p'-q) space (Sec. 260, EL270, Core CL)
Deviation of the orientation of the maximum stress from the vertical direction is presented
in Figures 8 and 9. These graphs pointed out substantial rotation of the principal stress
direction to the upstream in the core, which was indicative of a progressing shear zone and
would lead to bulging of the core.
Figure 8. Orientation of principal stress direction (Sec, 260, El. 230)
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Figure 9. Orientation of principal stress direction (Sec, 260, El. 230)
3. PORE WATER PRESSURE
Pore pressure in the dam body had been measured by using pore pressure gauge installed
in the center and downstream side of the core. The pore pressure gauges in the upstream
side of the core were malfunctioning data in these portions were not available.
A ratio of the pore pressure to the measured vertical earth pressure (letter M in graphs) and
to the principal stress (letter S in the graphs) are shown in figure 10-12. Variation of these
values indicates a dissipating process of pore water and air form the core. The level of the
pore pressure ratio after 11 years from the embankment completion was high. These had
been continuously decreasing since the full impoundment at a slow rate.
The ratio of the pore pressure in the lower portion of the core was still at the high values of
90%. Therefore, the measurement results were simply indicative that the dissipating
process of the pore pressure in the core of the MES dam was extremely slow.
Considering that the pore water pressure is an isotropic tension�and the main stress is also
zero in shear conditions. It can be concluded that the pore water pressure ratios calculated
on the principal stresses is closer to reality than base on the total stress.
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Figure 10. Pore Pressure ratio at 230 elevation (CH 260)
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Figure 11. Pore Pressure ratio at 270 elevation (CH 260)
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EP-2104(D/S,229.94m,S) RWL Embankment Level
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Figure 12. Pore Pressure ratio at 310 elevation (CH 260)
4. EFFECTIVE STRESS
Variation of the effective stress in the middle and downstream part of the core at 280
elevation are shown in figures 13-15. In these graphs, horizontal axis is the distance of the
left side to right side of the dam axis and the elevations of abtuments are shown. Effective
stress in the CH. 260 had been very little increased after impounding, this mater indicates
that the condition is undrained and the progressive of consolidation is very low. Also at
310 elevation in CH260 the effective stress have little increase after impounding (report on
monitoring of MS dam behavior, 2014).
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Figure 13. Effective stress in middle part of the core at 280 elevation along the axis' dam��
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ss (K
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Figure 14. Effective stress in downstream part of the core at 280 elevation along the axis' dam
Figure 15. Effective stress in downside of the core at 310 elevation along the axis' dam��
5. CONCLUSION
By considering the fact that the surface settlement had been continuing without notable
progress of consolidation and Pore pressure ratio for most sections of core is high (over
0.8). Also, the orientation of the stress to upstream was indicative of a progressing shear
zone and would lead to bulging of the core.
Bulging of the downstream part of the core is expected to occur at mid-height and below.
Such bulging will certainly lead to a deformational response of the adjacent part of the
filter and the downstream shell. This is the main reason for developing the lateral
deformation in the clay core. It’s notable that the settlement of the foundation not expected,
so it’s lead to mobilize the pressure to adjacent part of downstream of core and amplify the
deformation this part of dam body.
ACKNOWLEDGMENT
The present research has been commissioned by the Geotechnique Department of the Ab-
Pooy Consulting Engineers. This study was a part of the Stability Analysis of Masjed
Soleyman dam project.
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REFERENCES
Abpooy consulting engineers, (2014): report on monitoring of MS dam behavior.
Khalili, A. and F. Jafarzadeh, (2006): Evaluation of strength parameters of Masjed
Soleyman Dam clay core using CPTU.
Maleki, M. and A.A. Far, (2004): safety evaluation of masjed-e-soleyman rockfill dam,
during construction and first stage impounding, in Uncertainty in Safety Evaluation of
Embankment Dams.
Soroush, A. and Araei, A.A. (2006): Analysis of behaviour of a high rockfill dam,
Proceedings of the ICE-Geotechnical Engineering, 159: p. 49-59.
Lahmeyer International and Moshanir, (1993): MES Dam Design Report, Vol. 1.
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