1. Background

2. Design and operation

3. See also

4. External links

5. References

The Siah Bisheh Pumped Storage Power Plant ({{lang-fa|نیروگاه تلمبه ذخیره‌ای سیاه‌بیشه}}), also spelled Siyāhbisheh and Siah Bishe, is located in the Alborz Mountain range near the village of Siah Bisheh and {{Convert|48|km|mi|0|abbr=on}} south of Chalus in Mazandaran Province, Iran. The power plant uses the pumped-storage hydroelectric method to generate electricity during periods of high energy demand, making it a peaking power plant, intended to fulfill peak electricity demand in Tehran {{Convert|60|km|mi|0|abbr=on}} to the south. When complete it will have an installed generating capacity of {{convert|1040|MW}} and a pumping capacity of {{convert|940|MW}}. Planning for the project began in the 1970s and construction began in 1985. It was delayed from 1992 until 2001 and the first generator went online in May 2013. The remaining generators were commissioned by 1 September 2015.^[3] The power plant is the first pumped-storage type in Iran and will also use the country's first concrete-face rock-fill dam – two of them.^[2][5][6]

Background

A site was first identified for the power plant in the 1970s when a study was carried out on the water resources of the Albors Mountains by the Belgian firm Traksionel. Several sites for dams were identified including Siah Bisheh as a potential place for a pumped-storage power plant. In 1975, a feasibility report on the Siah Bisheh project was submitted to the Ministry of Energy. The Albors Mountains study concluded in 1977 and geologic studies began in 1978 but were halted in 1979 due to the Iranian Revolution. In 1983, Lahmeyer International was contracted to create designs for Phase II (underground excavation) which were completed in 1985, the same year construction on the dam's diversion tunnels began. Further designs for Phase I (superstructures) were developed and construction continued until 1992 when a lack of funding halted the project once again. Construction would not commence again until 2001. In 2002 and 2003, contracts for the dams and power plant were awarded and construction continued. The project was 90 percent complete as of April 2012.^{[4][5][6][7][8]} Both the upper and lower reservoir were complete and had finished impounding in January 2013.^[9] The first of four generators was commissioned in May 2013 and the remaining were operational by 1 September 2015.^[3][10][11]

Design and operation

The power plant operates using a lower and upper reservoir along with a power plant connected to both. Water is either pumped from the lower to the upper reservoir to serve as stored energy or released from the upper to the lower reservoir to generate electricity. Pumping occurs during low demand, cheap electricity, periods such as night and generating will occur during peak demand, expensive electricity, hours such as during the day. The pumping/generating process repeats as needed.^[4][7]

Both the upper and lower reservoirs are created by concrete-face rock-fill dams on the Chalus River which has an average inflow of {{Convert|67.1|m3/s|ft3/s}}.^[12] The upper dam is {{Convert|82.5|m}} tall and {{Convert|436|m|ft|0|abbr=on}} long. It contains {{Convert|1550000|m3|cuyd}} of fill (structural volume) and is {{Convert|12|m}} wide at its crest and {{Convert|280|m|ft|0|abbr=on}} wide at its base. Its reservoir has a storage capacity of {{Convert|4344220|m3|acre.ft}} (of which {{Convert|3500000|m3|acre.ft|0|abbr=on}} is active or usable) and a surface area of {{Convert|141|km2|mi2}}. The lower reservoir dam is the bigger of the two and is {{Convert|102|m|ft|0|abbr=on}} tall and {{Convert|332|m}} long. It contains {{Convert|2300000|m3|cuyd}} of fill and is {{Convert|12|m|ft|0|abbr=on}} wide at its crest and {{Convert|360|m}} wide at its base. Its reservoir has a storage capacity of {{Convert|6874709|m3|acre.ft|0|abbr=on}} (of which {{Convert|3600000|m3|acre.ft}} is active or usable) and a surface area of {{Convert|141|km2|mi2|0|abbr=on}}. Each of the dams are equipped with a chute staircase spillway. The upper dam's has a maximum discharge capacity of {{Convert|203|m3/s|ft3/s|0|abbr=on}} and the lower: {{Convert|198.25|m3/s|ft3/s}}. The normal elevation for the upper reservoir is {{Convert|2406.5|m|ft|0|abbr=on}} and the lower {{Convert|1905.4|m}} which affords a gross maximum hydraulic head of {{Convert|520|m|ft|0|abbr=on}} and normal of {{Convert|504|m}}.^[13]

Connecting the upper reservoir to the power station is an intake which feeds water into two {{Convert|5.7|m}} diameter head-race tunnels. Their length from the intake to two surge tanks (used to prevent water hammer) is {{Convert|2225|m}} (left tunnel) and {{Convert|2185|m}} (right tunnel). From the surge tanks the tunnels each turn into a {{Convert|680|m}} long penstocks which delivers water to the power station which is located underground near the lower reservoir. At the power station, each penstock bifurcates into two penstocks to supply the four Francis turbine pump-generators with water. The pump-generators have a generating capacity of 260 MW and pumping capacity of 235 MW. The generators can each discharge up to {{Convert|65|m3/s|ft3/s}} of water and the power is converted by transformers to 400 kV. After water is discharged by the generators, it proceeds down one of two tail-race tunnels ({{Convert|197|m}} and {{Convert|159|m}} in length) before being discharged into the lower reservoir. When pumping is required, the pump-generators reverse into pumps and send water back to the upper reservoir through the same water conduits. Each generator can pump up to {{Convert|50|m3/s|ft3/s|0|abbr=on}} of water.^[5][13]

AF-Consult Switzerland Ltd acted as Owner's Engineer (Lead Consultant) during the design and supervision.

See also

• List of pumped-storage hydroelectric power stations
• List of power stations in Iran

External links

• Siahbishe Project at Iran Water & Power Resources Development Co.

References

• 1773 Guatemala earthquake
• 1773 in Norway
• 1773 in paleontology
• 1773 in the United Kingdom
• 1773 in Wales
• 1773 Rumpelstilz
• 17744 Jodiefoster
• 17746 Haigha
• 17748 Uedashoji
• 1774 in Norway
• 1774 in the United Kingdom
• 1774 in Wales
• 1774 Kulikov
• 1774–75 papal conclave
• 1775-1782 North American smallpox epidemic
• 17759 Hatta
• 1775 in France
• 1775 in Norway
• 1775 in the United Kingdom
• 1775 in Wales
• 1775 (television pilot)
• 1775 (TV pilot)
• 1775 Zimmerwald
• (177625) 2004 JD
• 17764 Schatzman