Okuyoshino Pumped Storage Power Station | |
---|---|
The Asahi Dam which forms the lower reservoir | |
Country | Japan |
Location | Totsukawa |
Coordinates | 34°7′4″N135°49′16″E / 34.11778°N 135.82111°E Coordinates: 34°7′4″N135°49′16″E / 34.11778°N 135.82111°E |
Status | Operational |
Construction began | 1971 |
Opening date | 1980 |
Owner(s) | Kansai Electric Power Company (KEPCO) |
Upper reservoir | |
Creates | Seto Reservoir |
Total capacity | 1,685,000,000 m3 (1,366,000 acre⋅ft) |
Lower reservoir | |
Creates | Asahi Reservoir |
Total capacity | 1,692,000,000 m3 (1,372,000 acre⋅ft) |
Power Station | |
Hydraulic head | 505 m (1,657 ft) [1] |
Pump-generators | 6 x 201 MW (270,000 hp) Francis pump-turbines [2] |
Installed capacity | 1,206 MW (1,617,000 hp) |
The Okuyoshino Pumped Storage Power Station (奥吉野発電所) is located 15 kilometres (9.3 mi) north of Totsukawa in Nara Prefecture, Japan. Using the pumped-storage hydroelectric method, the power plant has an installed capacity of 1,206 megawatts (1,617,000 hp). To accomplish power generation, the power station shifts water between two reservoirs, the lower Asahi Reservoir and the upper Seto Reservoir. Construction on both the Asahi and Seto Dams began in 1971 and was complete in 1978. The power station was commissioned in 1980. Due to heavy sediment and turbidity in the Seto Reservoir, caused by logging and landslides upstream, a sediment bypass tunnel was constructed between 1992 and 1998. [3]
Nara Prefecture is a prefecture in the Kansai region of Japan. The capital is the city of Nara. Nara Prefecture has the distinction of having more UNESCO World Heritage Listings than any other prefecture.
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation and if buried, may eventually become sandstone and siltstone.
Turbidity is the cloudiness or haziness of a fluid caused by large numbers of individual particles that are generally invisible to the naked eye, similar to smoke in air. The measurement of turbidity is a key test of water quality.
The lower reservoir is created by the Asahi Dam which is a 86.1 metres (282 ft) tall and 199.41 metres (654.2 ft) long arch dam on the Asahi River of the Shingu River system. Its catchment area covers an area of 39.2 square kilometres (15.1 sq mi) and the surface of the reservoir covers 52 hectares (130 acres). The lower reservoir's storage capacity is 1,685,000,000 cubic metres (1,366,000 acre⋅ft) of which 1,250,000,000 cubic metres (1,010,000 acre⋅ft) is active (or usable) for pumping up to the lower reservoir.
An arch dam is a concrete dam that is curved upstream in plan. The arch dam is designed so that the force of the water against it, known as hydrostatic pressure, presses against the arch, compressing and strengthening the structure as it pushes into its foundation or abutments. An arch dam is most suitable for narrow canyons or gorges with steep walls of stable rock to support the structure and stresses. Since they are thinner than any other dam type, they require much less construction material, making them economical and practical in remote areas.
The Asahi River is a river in Okayama Prefecture, Japan.
A drainage basin is any area of land where precipitation collects and drains off into a common outlet, such as into a river, bay, or other body of water. The drainage basin includes all the surface water from rain runoff, snowmelt, and nearby streams that run downslope towards the shared outlet, as well as the groundwater underneath the earth's surface. Drainage basins connect into other drainage basins at lower elevations in a hierarchical pattern, with smaller sub-drainage basins, which in turn drain into another common outlet.
Creating the upper reservoir in a valley above the lower is the Seto Dam. It is a 110.5-metre (363 ft) tall and 342.8-metre (1,125 ft) long rock-fill embankment dam with 3,740,000 cubic metres (4,890,000 cu yd) of fill. Its catchment area covers a much smaller area of 2.9 square kilometres (1.1 sq mi) and its surface covers 52 hectares (130 acres). The upper reservoir has a storage capacity of 1,692,000,000 cubic metres (1,372,000 acre⋅ft) of which 1,250,000,000 cubic metres (1,010,000 acre⋅ft) is useful for power generation down at the power station. [3] [4] [5]
An embankment dam is a large artificial dam. It is typically created by the placement and compaction of a complex semi-plastic mound of various compositions of soil, sand, clay, or rock. It has a semi-pervious waterproof natural covering for its surface and a dense, impervious core. This makes such a dam impervious to surface or seepage erosion. Such a dam is composed of fragmented independent material particles. The friction and interaction of particles binds the particles together into a stable mass rather than by the use of a cementing substance.
During periods of low demand when electricity is cheap, the power station pumps water from the lower reservoir to the upper. When energy demand is high, the water is released back down to the power station through the same tunnels to generate electricity. Additionally, the six 201 megawatts (270,000 hp) Francis pump-turbine-generators are reversible and serve to both pump water and generate electricity. [6] The pumping and generation process is repeated as needed and although the power station consumes more electricity pumping than it does generating, pumping occurs when electricity is cheap and generating when it is expensive; making the power station economical. The difference in elevation between the two reservoirs affords a hydraulic head of 505 metres (1,657 ft). [3]
Hydraulic head or piezometric head is a specific measurement of liquid pressure above a vertical datum.
To allow sediment to pass the lower Seto Reservoir, a bypass tunnel was constructed. The tunnel itself is hood-shaped and 2,350 metres (7,710 ft) long. It passes through rock on the north side of the reservoir. The intake for the tunnel is controlled by a 13.5 metres (44 ft) tall and 45 metres (148 ft) long weir located 2.5 metres (8 ft 2 in) upstream of the dam. The weir is used to divert sediment-laden river water into the tunnel or to let it flow into the reservoir. The tunnel can divert a maximum of 140 cubic metres per second (4,900 cu ft/s) of water and discharges downstream of the Seto Dam. [3]
A weir or low head dam is a barrier across the width of a river that alters the flow characteristics of water and usually results in a change in the height of the river level. There are many designs of weir, but commonly water flows freely over the top of the weir crest before cascading down to a lower level.
The Guangdong Pumped Storage Power Station or Guangzhou Pumped Storage Power Station is a pumped-storage hydroelectric power station near Guangzhou, Guangdong Province, China. Power is generated by utilizing eight turbines, each with a 300 megawatts (400,000 hp) capacity, totalling the installed capacity to 2,400 megawatts (3,200,000 hp). The generated power is sold to China Light and Power customers in Hong Kong. The power station was constructed in two stages, the first four turbines were completed in 1994 and the second four in 2000.
Tanbara Dam is a rock-fill embankment dam on a Tone River tributary in Gunma Prefecture of Japan. It is located 14 kilometres (8.7 mi) north of Numata. It creates the upper reservoir for the 1,200 megawatts (1,600,000 hp) Tamahara Pumped Storage Power Station (玉原発電所). Construction began in 1973 and the dam was complete in 1981 while the power station was commissioned in 1986. It is 116 metres (381 ft) tall and withholds a reservoir with a storage capacity of 14,800,000 m3 (11,999 acre⋅ft). Of that capacity, 13,000,000 cubic metres (11,000 acre⋅ft) is active for power generation. The lower reservoir for the pumped-storage power station is created by the Fujiwara Dam, located 4 km (2 mi) to the northwest on another Tone River tributary. Power is generated during periods of high energy demand and pumping occurs during times when energy demand is low such as at night. The power station contains four 300 megawatts (400,000 hp) reversible Francis turbine pump-generators which serve to both pump water and generate electricity. The upper Tamahara Reservoir is at an elevation of 1,177 metres (3,862 ft) and the lower Fujiwara Reservoir is at 651 metres (2,136 ft) which affords the power station an effective hydraulic head of 518 metres (1,699 ft). When pumping, the pump-generators can move up to 210 cubic metres per second (7,400 cu ft/s) of water and when generating, they discharge up to 276 cubic metres per second (9,700 cu ft/s).
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The Edolo Pumped Storage Plant is located along the Oglio River just downstream of Edolo, Brescia Province in the Lombardy region of Italy. Using the pumped-storage hydroelectric method, it has an installed capacity of 1,000 megawatts (1,300,000 hp). Its generators were commissioned between April 1984 and November 1985. Lake Avio was previously completed in 1929 and Lake Benedetto completed in 1940.
The Vianden Pumped Storage Plant is located just north of Vianden in Diekirch District, Luxembourg. The power plant uses the pumped-storage hydroelectric method to generate electricity and serves as a peaking power plant. Its lower reservoir is located on the Our River, bordering Germany, and the upper is elevated above on the nearby Saint Nicholas Mountain. Construction on the plant began in 1959 and the first pump-generators were commissioned in 1962. A tenth pump-generator was installed in 1976 bringing the plant's installed generating capacity to 1,096 megawatts (1,470,000 hp). The plant generates an average of 1,650 gigawatt-hours (5,900 TJ) annually but of course consumes even more. Generally the efficiency of this energy storage method is around 70-80%. The plant is owned by Société Electrique de l'Our and RWE. Construction on an eleventh pump-generator began in 2010 and it is expected to be commissioned in 2013, which will bring the plant's installed capacity to 1,296 megawatts (1,738,000 hp).
The Xiangshuijian Pumped Storage Power Station is a pumped-storage hydroelectric power station located 29 kilometres (18 mi) southwest of Wuhu City in Sanshan District of Anhui Province, China. Construction on the power station began on 8 December 2006 and the upper reservoir dam was completed in October 2010. The first unit was commissioned on 1 December 2011 and the last on 17 November 2012. The power station operates by shifting water between an upper and lower reservoir to generate electricity. The lower reservoir was formed with the creation of the Xiangshuijian Lower Dam in a valley. The Xiangshuijian Upper Reservoir is in another valley above the west side of the lower reservoir. During periods of low energy demand, such as at night, water is pumped from Xiangshuijian Lower Reservoir up to the upper reservoir. When energy demand is high, the water is released back down to the lower reservoir but the pump turbines that pumped the water up now reverse mode and serve as generators to produce electricity. The process is repeated as necessary and the plant serves as a peaking power plant.
The Tongbai Pumped Storage Power Station is a pumped-storage hydroelectric power station located 6 kilometres (3.7 mi) north of Tiantai city in Tiantai County of Zhejiang Province, China. Construction on the power station began in May 2000 and the first unit was commissioned in December 2005. The remaining three were operational by December 2006. The entire project cost US$904.10 million, of which US$320 million was provided by the World Bank. The power station operates by shifting water between an upper and lower reservoir to generate electricity. The lower reservoir was formed with the creation of the Tongbai Lower Dam on the Baizhang River. The Tongbai Upper Reservoir, which already existed before construction began, is in an adjacent valley above the east side of the lower reservoir on Tongbai Creek. During periods of low energy demand, such as at night, water is pumped from Tongbai Lower Reservoir up to the upper reservoir. When energy demand is high, the water is released back down to the lower reservoir but the pump turbines that pumped the water up now reverse mode and serve as generators to produce electricity. The process is repeated as necessary and the plant serves as a peaking power plant. The power station is operated by Shenergy Company.
The Yixing Pumped Storage Power Station is a pumped-storage hydroelectric power station located Yixing city of Jiangsu Province, China. Construction on the power station began in 2003 and the first unit was commissioned in 2007, the last in 2008. The entire project cost US$490 million, of which US$145 million was provided by the World Bank. The power station operates by shifting water between an upper and lower reservoir to generate electricity. The lower reservoir was formed with the existing Huiwu Dam at the foot of Mount Tongguan. The Yixing Upper Reservoir is located atop Mount Tongguan which peaks at 530 metres (1,740 ft) above sea level. During periods of low energy demand, such as at night, water is pumped from Huiwu Lower Reservoir up to the upper reservoir. When energy demand is high, the water is released back down to the lower reservoir but the pump turbines that pumped the water up now reverse mode and serve as generators to produce electricity. Water from the nearby Huangtong River can also be pumped into the lower reservoir to augment storage. The process is repeated as necessary and the plant serves as a peaking power plant. The power station is operated by East China Yixing Pumped Storage Co Ltd.
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