Philippines - Binga
Key project features
Following commissioning in 1960, the Binga reservoir filled rapidly with sediment due to an underestimation of the sediment load and the absence of any sediment management strategy. When Binga hydropower plant was acquired by SN Aboitiz (SNAP) in 2008, it was not operational. Sediment management is crucial to keeping the plant operational as a run-of-river project.
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Three dams in a cascade complex on the Agno river supply water to the 105 MW Ambuklao, the 140 MW Binga and the 345 MW San Roque hydropower plants. Binga dam, located 19 km downstream from Ambuklao, is a rock-fill dam with an inclined clay core. At a height of 107.4 m, the dam crest elevation is 586 masl, and the dam originally impounded a volume of 95 Mm3. The maximum and minimum operating levels of the reservoir are 575 and 566 masl respectively.
The spillway is located at the left abutment, while the intake is on the right side leading to the underground powerhouse through an 800 m headrace tunnel. The design spillway discharge for a return period of 10,000 years is 10,521 m3/s. A location map is shown in figure 1.
Following its refurbishment in 2013, the 140 MW Binga plant now hosts four Francis vertical shaft turbines of 35 MW each. The net head is 156 m and the design discharge is 25 m3/s. The average annual generation is 238.43 GWh.
Hydrology and sediment
The catchment tributary of the Binga dam comprises 936 km2, of which 72 per cent is regulated by the Ambuklao dam upstream. Although the Ambuklao reservoir traps most of the sediment, the Binga tributaries, the Leboy, Adonot and Bisal Rivers, carry very high sediment loads. This is deposited in the upper section of the Binga delta, as shown by the white sediment deposits in figure 1.
The Philippines is one of the countries most exposed to tropical storms. Approximately 20 cyclones and typhoons hit the country each year. They are concentrated in the months of June to September, but can occur throughout the year.
Due to its geographical location, the Philippines also suffers from high magnitude earthquakes. Since the middle of the 20th century, there have been eight earthquakes above 7 points in magnitude. In 1990, the island of Luzon experienced a 7.8 magnitude earthquake.
As shown in figure 2, the water inflow to the Binga reservoir has increased over the years, with the peak flow reaching up to 2,000 m3/s in 2017.
Cyclones and typhoons cause major floods and landslides that increase water inflow and sediment load in the rivers. In combination with earthquakes, the sediment load in the rivers can be very high, and can contain heavy boulders that have the potential to seriously damage a power plant’s units.
The annual observed sediment load through the turbines at Binga is 2.2 million tons, while at Ambuklao it is 4.5 million tons. Hard mineral concentration is not an issue because this represents just 10 per cent of the sediment load.
Based on a traditional approach, the Binga reservoir was designed without any sediment management strategy. In addition, the sedimentation rate was underestimated due to the limited sediment data available at the time. After commissioning in 1960, the Binga reservoir rapidly filled up with sediment as shown in the storage capacity-elevation curve displayed in figure 3. By 1986, the reservoir had lost 35 per cent of its original capacity. In 2015, the storage volume was just 21 Mm3, equivalent to 22 per cent of the original storage capacity.
In 2008, SNAP acquired both the Ambuklao and Binga power plants for USD 325 million. Both plants required major refurbishment due to the damaged hydro-mechanical equipment. The Binga power plant was not operational and the sediment deposits almost reached the intake level.
Since the acquisition and refurbishment of Binga, the implementation of sediment management strategies is key to keeping the plant operational in the long term."
Due to the bathymetry of the Binga reservoir, the sediment has filled the dam and developed into a delta with a growing backwater effect, which could affect and bury the Ambuklao outlet. Figure 4 shows boulders and gravel in the backwater of the Binga reservoir.
An extreme precipitation event occurred in October 2009, following SNAP’s acquisition of the Ambuklao and Binga power plants. The peak inflow to the Binga reservoir reached 4,000 m3/s. Figure 5 shows the water inflow to the Ambuklao and Binga reservoirs due to the extreme flood.
This extreme flooding clogged up the waterways, and sediment deposits trapped in the Binga dam increased. The loss of storage limited Binga’s operational flexibility and therefore reduced the plant’s revenue. In the case of Ambuklao, the power plant had to shut down. A total of USD 280 million was required to rehabilitate both the Ambuklao and Binga plants, between 2010 and 2013.
Sediment management strategies
Since the acquisition and refurbishment of Binga, the implementation of sediment management strategies is key to keeping the plant operational in the long term. Due to the high rate of storage loss, the stabilisation of sediment inflow and outflow is crucial for operating Binga as a run-of-river project.
Any alternative approach to managing sediment requires changes in the operating rule of the flood gates. The operating rule, shown in figure 6, is based on the water level and does not include sediment routing during flood events greater than 500 m3/s.
Ongoing studies are looking at technically-feasible solutions to convert Binga into a run-of-river power plant. The proposed sediment management strategies will have to meet the following objectives:
Protect the intake from deposition and slide;
trap the suspended load during normal flood season operation;
flush deposited suspended load during floods;
provide passage of incoming bed load during floods;
maintain small reservoir for peaking/ancillary services;
maintain ability to delay and dampen flood peak; and
maintain dam safety and the integrity of the spillway.
A significant sediment management challenge is the high risk of clogging the current Binga intake, with an invert elevation of 555 masl. The longitudinal profile in figure 7 shows that sediment deposits are reaching that level.
Other challenges include maintaining the existing storage volume, avoiding backwater effect, the burying of the Ambuklao outlet, and maintaining dam safety when the bed load passes over the spillway to the downstream river reach.
Physical model studies include several sediment routing options and intake-level modifications to find a technically feasible solution and acceptable and implementable operational regime, which would provide for a reliable run-of-river operation in the long term.
Sediment management considerations are fundamental during the initial concept/design phase when building dams and hydropower plants. Without them, sediment is deposited in reservoirs, minimising a plant’s benefits, shortening its operational life, damaging the hydro-mechanical equipment and eventually losing sites for power generation and other benefits.
Monitoring and gathering sediment data taking account of the impact of natural disasters such as earthquakes and typhoons into the design is key to planning adequate sediment management strategies.
The annual cost of the research on sediment and sediment management at Binga is estimated to be around 2.5 per cent of the annual operation and maintenance costs, which are estimated at USD 2 million. Raising awareness of the benefits of regular monitoring and sediment management strategies in the operation and maintenance of a power plant could lead to an increase in the resources dedicated to sediment management.
Graphs and figures
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This is part of a series of sediment management case studies collated by the International Hydropower Association with support from the South Asia Water Initiative (SAWI), trust funds to the World Bank. For more case studies, visit www.hydropower.org/sediment-management.