Harsprånget hydroelectric power station
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Harsprånget | |
---|---|
![]() | |
Country | Sweden |
Location | South of Porjus |
Coordinates | 66°53′04″N 19°49′27″E / 66.88444°N 19.82417°E |
Status | Operational |
Construction began | 1918 Cancelled 1921 Restarted 1945 |
Opening date | 1951 |
Owner(s) | Vattenfall |
Dam and spillways | |
Type of dam | Rock-fill dam |
Impounds | Lule River |
Height | 50 m (164 ft) |
Length | 1,400 m (4,600 ft) |
Dam volume | 6,000,000 m3 (210,000,000 cu ft) |
Reservoir | |
Creates | Harsprånget Reservoir |
Power Station | |
Type | Conventional |
Hydraulic head | 107 m |
Turbines | 2*110 MW, 1*180 MW, 1*465 MW, 1* 110 MW idled. All of Francis-type |
Installed capacity | 811 MW |
Annual generation | 2,1 TWh (2009) |
Harsprånget is a hydroelectric power station located on the Lule River in northern Sweden, just downstream of Porjus.
With a nameplate capacity of 811 MW[1], it is the largest hydroelectric power station in Sweden, and also among the largest in the Nordic countries. The name means "Hare Run" in Swedish. This was also the name of the now usually dry waterfall located downstream of the dam. Annual production is around 2131 GWh. Total hydraulic head is around 107 m.
History
[edit]Construction of the station started in 1918. However, recession after World War I cancelled the construction, which was not started again before 1945. It was opened in 1951, then with a nameplate capacity of 330 MW. In 1980, two new turbines were installed which increased the nameplate capacity to 945 MW. The rated power was later increased further to 977 MW[2].
Unit 3 has since then been idled, but will be returned to service after an extensive refurbishment, including a turbine and generator replacement[3].
Turbines
[edit]Units | 1 | 2 | 3 | 4 | 5 |
---|---|---|---|---|---|
Capacity | 110 MW | 110 MW | 110 MW | 180 MW | 475 MW |
Maximum water flow | 127 m³/s | 127 m³/s | 127 m³/s | 175 m³/s | 485 m³/s |
Revolutions/min | 166,7 r/min | 166,7 r/min | 166,7 r/min | 166,7 r/min | 107,1 r/min |
Cog diameter | 3,6 m | 3,6 m | 3,6 m | 4,2 m | 6,6 m |
Supplier | NOHAB | NOHAB | NOHAB | KMW | NOHAB |
Status | Active | Active | Idled | Active | Active |
Waterfall
[edit]The power plant exploits roughly half of the hydraulic head on a roughly 20 km stretch of the Lule river between Porjus and the downstream Ligga power plant that not only differs significantly from the rest of the river system in terms of geology and topography, but has few if any equivalents within the rest of the country with comparable flow rate. On this river stretch, the river dropped a total of 215 meters (207 meters after interventions) in a large series of waterfalls confined in a v-shaped, partly canyon-like river valley, sometimes over 40 meters deep, whose banks almost unequivocally consist of exposed bedrock, unlike the rest of the river system where the river banks mostly are made up of moraine[4]. At Harsprånget, the river becomes particularly narrow, sometimes just around 10 meters, and in its natural state, drops 75 meters over a distance of 3 km in what used to be a particularly violent series of waterfalls or rapids, characterized by two sharp turns, which are speculated to have given the former waterfall its name, as it would be likened to a fleeing hare. The maximum flow rate, according to the information sign at the location, was estimated at 1500 m3/s during spring flood.

The unusual river stretch and its waterfalls, including those at Porjus and Harsprånget, is believed to be geologically younger than the rest of the river system, and is thought to have been a result of the Lule river changing course after one, but not the most recent, ice age, before which it is believed to have flowed through the present Råne River valley. Through stream capture by the present right tributary Pakkojokk, which joins the Lule river just downstream of the Harsprånget canyon, the river carved its present course[5].
References
[edit]- ^ "Harsprånget". Vattenfall. Archived from the original on 2024-12-06.
- ^ "Harsprånget". Vattenfall. Archived from the original on 23 October 2014. Retrieved 13 June 2023.
- ^ "Vattenfall investerar 1,3 miljarder kronor i Sveriges största vattenkraftstation (Swedish)". Vattenfall. 2025-05-30. Archived from the original on 2025-06-15.
- ^ Hamberg, Axel (1906). "Öfversikt av Lule älfs geologi" (PDF). Geological Survey of Sweden. C (202): 9–10.
- ^ Lidmar-Bergström, Karna; Olvmo, Mats (2015). "Plains, steps, hilly relief and valleys in northern Sweden – review, interpretations and implications for conclusions on Phanerozoic tectonics". Geological Survey of Sweden. C: 20, 29, 36 – via Researchgate.