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have as result a steepening of the reservoir invert. Therefore, density current
venting might be a feasible option in the future. RESCON-2 indicated that a
reduction of the sedimentation by approximately 10% might be possible through
density current venting in the future.
RESCON-2 indicated that a standard hydraulic dredger with capacity of
115000 m³/a, which is within the technically feasible limits of dredging in reservoirs,
is the only technique that can sustain the active storage at the pre-impoundment
levels. The time path of reservoir gross and active storage is plotted in Fig. 3 with
the orange line. Dredging however is associated with high operation costs as well
as environmental considerations about the disposal of the dredged.
RESCON-2 calculated for flushing a Sediment Balance Ratio (SBR) of 3.1,
i.e. the sediment removal capacity of the specified flushing event will be
approximately 3 times higher than the expected annual sediment deposits. This
indicates that flushing is a technically feasible solution for Moragolla reservoir. The
Long-term Capacity Ratio (LTCR) will be 0.64, i.e. 64% of the reservoir gross
storage can be preserved sustainably. Its efficiency however drops to 50% with
regards to active storage. The time path of reservoir gross and active storage is
plotted in Fig. 3 with green lines. Environmental considerations associated with the
expected high sediment concentrations downstream of the reservoir that would
endanger the fish habitat of Mahaweli River together with the high energy
generation losses due to the necessary full water level drawdown had as result
that this technique was evaluated as not acceptable.
The unregulated part of the catchment area draining into Moragolla reservoir
is mostly forested or covered by tea gardens which are one of the major economic
activities in the project region. It was considered therefore, that measures such as
reforestation or change of the agricultural practices with purpose the reduction of
the surface erosion are not technically feasible. The effect of dispersed check
dams in the catchment area on the sediment inflow was not part of this study and
has to be investigated more in detail.
The evaluation of the river morphological features indicated that the reach of
Mahaweli River extending approximately 2 km upstream of the reservoir
headwaters is characterized by pronounced river meandering and sandy river bed.
Limited sand mining is already performed by the local communities at this location.
Numerical simulations with the one-dimensional model HEC-RAS indicated that
the construction of a relatively short check dam with height of approximately 2.5 m
would have as result an intensification of the retention of the sand particles in this
river reach. A sediment trap at this location can retain annually approximately
60,000 m³ of sediment, corresponding to 40 % of the expected total mean annual
sediment inflow into Moragolla reservoir. This can be translated as full retention of
the material transported as bedload and retention of the coarsest 20% of the
material transported in suspension. The necessary requirement for the above
described sediment trap performance is the regular and continuous restoration of
its trap efficiency by means of sand mining. The impact of this sediment inflow
reduction is that approximately 10% of the gross storage and 50% of the pre-
impoundment active storage is preserved sustainably. Except from the sediment
inflow reduction an important aspect is that the sediment entering now the reservoir
is finer since the coarsest part will be retained in the sediment trap. This has as
648
Book of Full Papers
Symposium Hydro Engineering
- Title
- Book of Full Papers
- Subtitle
- Symposium Hydro Engineering
- Author
- Gerald Zenz
- Publisher
- Verlag der Technischen Universität Graz
- Location
- Graz
- Date
- 2018
- Language
- English
- License
- CC BY-NC-ND 4.0
- ISBN
- 978-3-85125-620-8
- Size
- 20.9 x 29.6 cm
- Pages
- 2724
- Keywords
- Hydro, Engineering, Climate Changes
- Categories
- International
- Naturwissenschaften Physik
- Technik