Main Report (ISBN : 983-3067-17-4)
Researchers:
Prof. Dr. Aminuddin Ab.
Ghani <redac02@eng.usm.my>
Prof Dr. Nor Azazi Zakaria <redac01@eng.usm.my>
Prof. Pierre Y. Julien
(Colorado State University, USA) <pierre@engr.colostate.edu>
Assoc. Prof. Dr. Rozi Abdullah
<cerozi@eng.usm.my>
Chang Chun Kiat <redac10@eng.usm.my>
Rosmaliza Ramli <redac05@eng.usm.my>
Joseph Dinor <joseph@usm.eng.my>
Asnol Adzhan Abd. Manap
<wev6516@yahoo.com>
Mohd Fazly Yusof
<redac07@eng.usm.my>
Project Summary:
The Flood
Control Remediation Plan (FCRP) has been reviewed with the
perspective to possibly enhance the proposed design. The
objectives of this review are: (1) ensure that design
cross-sections and alignment of the main river channel are
economic, effective and environmentally sound; (2) propose
alternative designs for identified locations to meet the above
requirements; and (3) examine the long term river
behaviour
through model studies to minimize expensive repair works in
future resulting from the new alignment.
The scope of
work of this report includes a review of:
(a) Rainfall
data in space and time leading to chosen flood events.
(b) Runoff
discharge and stage records of the chosen events;
(c) Computer
simulation of the flood events;
(d) Computer
simulation of long term river behaviour to determine stretches
prone to meandering, hence needing extra protection;
(e) Changes in
alluvial river geometry in terms of aggradation and degradation
as well as lateral channel migration as a result of the flood
events;
(f) Design
criteria used for the Flood Control Remediation Plan;
(g) Specific
design of the proposed structures including levee protection,
riverbank protection works and protection of bridge crossings
and other structures.
In an itemized
fashion, the main conclusions of this review are specifically:
(a)
There is
significant uncertainty in the determination of the three-day
rainfall rates in 2003. The watershed average rainfall
precipitation is difficult to ascertain from only four raingages.
However, the three-day watershed average rainfall precipitation
is found to be less than 300mm.
(b) The
analysis of a 44 year measured discharge record at Ladang
Victoria leads to a well defined 50-year flood peak discharge
around 1,270 cumecs. Similar results are obtained from
independent flood frequency analyses. This value is the most
reliable estimate of the 50 year flood peak discharge. The 2003
flood with a peak discharge of 1,340 cumecs is recommended for
the design of the FCRP. Comparatively, river stage records are
highly variable as a result of excessive sand and gravel mining
operations on Sg. Muda. Stage records should not be used to
estimate flood discharges.
(c) Computer simulations of the flood events with the model HEC-HMS
showed very good results for the calibration and validation of
the discharge hydrographs at Syed Omar in 2003 and 1998
respectively. However, there is a significant variability
(error of at least 100 cumecs) in both the calibrated and
validated results at Ladang Victoria. This appears to be due to
the limited number of raingages in the southern part of the
watershed where precipitation showed spatial variability. When
using the same high rainfall precipitation as JPZ, the HEC-HMS
results are very consistent with their design hydrographs.
However, as discussed above in (a), the three-day rainfall
precipitation of 350 mm used to determine a 50 year peak
discharge of 1,815 cumecs is viewed as excessively large. The
results of these rainfall-runoff models are highly variable and
less reliable than the measured flood discharges at Ladang
Victoria. It is concluded that the 50-year design hydrograph
with peak discharge of 1,815 cumecs is excessively large. The
value of peak discharge of 1,340 cumecs should be used for the
design. The design discharge reduction by 25% should results in
significant cost savings for the FCRP of Sg Muda.
(d) The model Fluvial 12 has been used for the lateral and vertical
elevation changes during the 2003 flood event. Most cross
sections are very stable and the vertical elevation changes are
small due to the low sediment transport rates of the bed
material. The sand and gravel mining operations are far
exceeding the natural sediment transport rates of the river.
These operations can cause serious problems to the stability of
the proposed structures of the FCRP. It is concluded that
in-stream sand and gravel mining operations should not be
allowed.
(e)
The model Fluvial 12 also highlighted potential lateral
migration changes near the sharp bends upstream of Merdeka
Bridge and near Lahar Tiang. It is concluded that channel
realignment near Merdeka Bridge and Lahar Tiang would minimize
potential lateral migration problems of Sg Muda. These
realignments should also result in better flood conveyance,
reduced roughness and backwater and lower bund elevation.
(f) The proposed bund height under Alternative 2 of JPZ appears to
be highly conservative and will pass flows with period of return
much in excess of 100 years. The proposed design criterion for
the FCRP is to add a one meter freeboard to the flood stage
calculated for the current channel cross sections, without
widening, using the 2003 flood peak of 1,340 cumecs. The
results obtained from the model HEC-RAS result in lowering the
proposed bunds by 30cm to 1m over the 43 km reach of Sg. Muda.
It is recommended not to widen the channel cross sections.
Channel widening will result in lower flood stages and lower
bund elevations, thus resulting in additional cost savings.
These cross sections were not available to us, but further
analysis should be carried out if channel widening is retained
as an option. In view of excessive sand and gravel mining of
the Sg Muda, the bridge pier footings at Ladang Victoria need
serious and immediate attention. Pumping stations for
irrigation canals have also been required on the Sg Muda as a
result of the continuing degradation of the river. The
degradation can be clearly attributed to the excessive sand and
gravel mining of the Sg Muda. For the bank stabilization
structures of the FCRP to be effective, it will be essential not
to allow any in-stream sand and gravel mining activities in the
future. It is proposed to allow off-stream sand and gravel
mining activities at a minimum distance of 50 m from the river
banks. The floodways to Sg. Merbok is not recommended because
it would bring additional water to areas that were readily
flooded in 1998 and 2003. The Merbok river diversion would also
require long bunds and an additional barrage, which cost will
not be economically justified. The potential diversion to Sg.
Korok can only be justified as an emergency measure to prevent
rupture of the proposed bunds designed in this FCRP. These
diversions may alleviate the problem of flood mitigation on the
Muda, but at the same time may exacerbate the flooding problems
in the upper watershed of Sg Perai.
Recommendations:
The Flood
Control Remediation Plan (FCRP) has been reviewed with the
perspective to possibly enhance the proposed design. The
conclusions of this report demonstrate the potential for
significant cost saving features as well as structural stability
measures. The specific recommendations for the FCRP include the
following:
(a) It
is proposed to reduce the design discharge from 1,815 cumecs to
the proposed discharge of 1,340 cumecs from the 2003 flood.
This design discharge reduction of about 25% should yield
significant cost reduction of the total cost of the FCRP. It is
recommended not to widen the channel. However, any widening of
the channel cross sections would result in further lowering the
bund elevation thus further reducing the cost of the FCRP. It
is recommended to run the HEC-RAS model with the proposed
widened cross sections for comparison with the current results
(these cross section were not available for this study). More
specifically, the effects of the excessive channel widening
downstream of the Muda barrage should be considered in terms of
bund height and also possible sediment accumulation near the
mouth of Sg. Muda.
(b) The suggested
channel realignment is expected to result in reduced roughness,
reduced backwater effects and thus lower bund elevations. It is
recommended to run the HEC-RAS model with consideration of the
proposed realignments. The results of these two measures should
result in a lower cost of the FCRP.
(c)
It is strongly
recommended to prohibit all in-stream sand and gravel mining
activities between Ladang Victoria and the Muda Barrage.
Off-stream mining activities should instead be allowed at a
minimum distance of 50 m from the channel. We recommend a more
detailed analysis of the locations and volumes of sand and
gravel that can be extracted under this proposal.
It is recommended to recalculate the bund height and provide a
more detailed estimate of the cost saving features discussed in
(a), (b), and (c).
Study Area: Sungai Muda Lower
Reach
Sungai Muda Catchment

New Barrage Under Construction
Bed Load Sampling @ Ladang
Victoria New Bridge

(a) Calibration
(b) Validation
Runoff Hydrograph at Ladang Victoria Discharge Station

Longitudinal Flood Profile for Sg Muda in HEC-RAS Model

Cross Sections for Sg Muda in HEC-RAS
Model

Comparison of 2003 Flood Water Level and Proposed Bund Height


(a) CH 23.0
(b) CH 21.9
Lateral Migration @ Kg Lahar
Tiang (FLUVIAL-12 Model)


(a) CH 15.4
(b) CH 13.1
Lateral Migration @ Bumbong Lima
(FLUVIAL-12 Model)
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