RIO MADEIRA RUN-OF-RIVER HYDRO PROJECTSSOME EXAMPLES OF RUN-OF-RIVER HYDRO PROJECTS • In France on...
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RIO MADEIRA RUN-OF-RIVERHYDRO PROJECTS
SEDIMENT TRANSPORT MANAGEMENT
Sultan AlamIndependent Consultant
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MAIN CHARACTERISTICS OFRUN-OF-RIVER HYDRO PROJECTS
• Water and sediment transport through the upper pool is very similar to the initial river flow conditions
• Practically no stagnation zone in themain channel
• Ensure long project life without any significant sedimentation in the upper pool unlike large dams and reservoirs
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SOME EXAMPLES OF RUN-OF-RIVERHYDRO PROJECTS
• In France on the Rhône River and its tributaires there are 22 run-of-river projets built 20 to 50 years ago with 10 to 50 m head
• Pak Mun in Thailand was built 25 years ago
• Sidney A. Murray off the Mississippi River in Louisiana was built 16 years ago
• All of them are operatingsatisfactorily
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PARTICLE SIZE DISTRIBUTION
Composição granulométrica da carga Sedimentar do rio Madeira na região dos AHE Santo Antônio e Jirau
%
85
141
Argila e SilteAreia Fina (< 1 mm)Areia Média e Grossa (< 2 mm)
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SEDIMENT TRANSPORT MECHANISM
• Under existing conditions andwith the proposed hydro projectssilt and clay component of thesediment materials are alwaysmoving in suspension
• This means that sands depositedon the river bed will always benon cohesive and will be put intosuspension as soon as the local shear velocity is adequate
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C0NTINUOUS SEDIMENT SAMPLING
• Since 1991 a continuous sedimentsampling installation is being used atOld River Complex on the LowerMississippi River and at Sidney A. Murray run-of-river hydro station
• These installations have enabled us to obtain precise information on thetotal sediment transport process ofthe Mississippi River at this location
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0
5 000
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01/01
/8201
/02/82
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/82
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/05/82
01/06
/8201
/07/82
01/08
/82
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/8201
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/12/82
Data
Vazõ
es (m
³/s)
Guajará-MirimAbunãAbunã - Guajará-MirimPorto Velho
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0
500
1.000
1.500
2.000
2.500
3.000
3.500
4.000
0 5.000 10.000 15.000 20.000 25.000 30.000 35.000 40.000 45.000 50.000
Descarga Líquida (m³/s)
Con
cent
raçã
o (m
g/l)
ANA FURNAS (Segunda Campanha)
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0
5 000
10 000
15 000
20 000
25 000
30 000
35 000
40 000
45 000
50 000
01/01
/8201
/02/82
01/03
/82
01/04
/8201
/05/82
01/06
/8201
/07/82
01/08
/82
01/09
/8201
/10/82
01/11
/8201
/12/82
Data
Vazõ
es (m
³/s)
Guajará-MirimAbunãAbunã - Guajará-MirimPorto Velho
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Shear velocity u* = (ghi)0.5
• In computing the shear velocities we have used the energy gradient i correspondingto steady flow conditions.
• For variable flow with the increasing flood discharge the instantaneous value of i andconsequently u* will be much more andsand particles will go into suspension earlier with lesser discharges
• So the values of w/u* in the report are rather conservative
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FLUSHING OF FINE SANDS
• Non cohesive fine sand can beflushed very quickly as shown by the continuous recording of thesediment concentration at theauxiliary sediment diversion channel at the Old River Complexof the lower Mississippi River
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CONCLUSION
• The sediment transport patterns of Rio Madeira will not be radically modified due to the construction of the proposed lowhead run-of-river hydro projects
• Annual sediment deposition and erosionwill continue to occur as at present and a new equilibrium of sediment transport from upstream to downstream will beestablished
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• As sediment and hydrologicalcharacteristics are the same at bothSant Antônio and Jirau projects theywill be subjected to same kind ofevolution with minimum negativeenvironmental impacts
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PLANTA DO RESERVATÓRIO DA AHE JIRAU
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MITIGATION MEASURES
• Necessary site specific measureswould have to be developed to mitigate local drainage and floodingproblems
• In the long run a new main channelcross section will be established withbankfull flow conditions
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STATE-OF-THE-ARTHYDRAULIC MODELLING
• ADEQUATE HYDRAULIC MODEL STUDIES MUST BE CARRIED OUT TO ESTABLISH THE BEST PROJECT LAYOUT AGAINST SEDIMENTATION NEAR THE STRUCTURES
• TO DEFINE OPTIMUM FLOATING DEBRIS HANDLING ARRANGEMENT
• TO AVOID AIR ENTRAINING VORTEX FORMATION
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MANY THANKS