Jump to content

Harsprånget hydroelectric power station

Coordinates: 66°53′04″N 19°49′27″E / 66.88444°N 19.82417°E / 66.88444; 19.82417
From Wikipedia, the free encyclopedia
Harsprånget
Harsprånget hydroelectric power station is located in Sweden
Harsprånget hydroelectric power station
Location of Harsprånget in Sweden
CountrySweden
LocationSouth of Porjus
Coordinates66°53′04″N 19°49′27″E / 66.88444°N 19.82417°E / 66.88444; 19.82417
StatusOperational
Construction began1918 Cancelled 1921
Restarted 1945
Opening date1951
Owner(s)Vattenfall
Dam and spillways
Type of damRock-fill dam
ImpoundsLule River
Height50 m (164 ft)
Length1,400 m (4,600 ft)
Dam volume6,000,000 m3 (210,000,000 cu ft)
Reservoir
CreatesHarsprånget Reservoir
Power Station
TypeConventional
Hydraulic head107 m
Turbines2*110 MW, 1*180 MW, 1*465 MW, 1* 110 MW idled. All of Francis-type
Installed capacity811 MW
Annual generation2,1 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]
The turbines are of Francis type with vertical axis and steel spirals.
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 normally dry waterfall downstream of the power plant, during a release of water from the dam.

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]
  1. ^ "Harsprånget". Vattenfall. Archived from the original on 2024-12-06.
  2. ^ "Harsprånget". Vattenfall. Archived from the original on 23 October 2014. Retrieved 13 June 2023.
  3. ^ "Vattenfall investerar 1,3 miljarder kronor i Sveriges största vattenkraftstation (Swedish)". Vattenfall. 2025-05-30. Archived from the original on 2025-06-15.
  4. ^ Hamberg, Axel (1906). "Öfversikt av Lule älfs geologi" (PDF). Geological Survey of Sweden. C (202): 9–10.
  5. ^ 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.