Akosombo Dam

The Akosombo Dam, also known as the Volta Dam, is a hydroelectric dam on the Volta River in southeastern Ghana in the Akosombo gorge and part of the Volta River Authority.[1] The construction of the dam flooded part of the Volta River Basin and led to the subsequent creation of Lake Volta. Lake Volta is the largest man-made lake in the world by surface area. It covers 8,502 square kilometres (3,283 sq mi), which is 3.6% of Ghana's land area. With a volume of 148 cubic kilometers, Lake Volta is the world's third largest man-made lake by volume; the largest being Lake Kariba which contains 185 cubic kilometers of water.[2]

Akosombo Dam
Akosombo Dam as seen from the Volta Hotel
Akosombo Dam is located in Ghana
Akosombo Dam
Location of the Akosombo Dam in Ghana
LocationAkosombo, Ghana
Coordinates6°17′59″N 0°3′34″E
StatusOperational
Construction began1961
Opening date1965
Construction cost£130 million
Owner(s)Volta River Authority
Dam and spillways
Type of damEmbankment, rock-fill
ImpoundsVolta River
Height (foundation)114 m (374 ft)
Length660 m (2,170 ft)
Width (base)366 m (1,201 ft)
Dam volume7,900,000 m3 (280,000,000 cu ft)
SpillwaysTwin gate-controlled
Spillway capacity34,000 m3/s (1,200,000 cu ft/s)
Reservoir
CreatesLake Volta
Total capacity148 km3 (120,000,000 acre⋅ft)
Surface area8,502 km2 (3,283 sq mi)
Maximum length400 km (250 mi)
Power Station
Hydraulic head68.8 m (226 ft) (max)
Turbines6 x 170 MW (230,000 hp) Francis-type
Installed capacity1,038 MW (1,392,000 hp)
Website
www.vra.com/our_mandate/akosombo_hydro_plant.php

The primary purpose of the Akosombo Dam was to provide electricity for the aluminium industry.[3] The Akosombo Dam was called "the largest single investment in the economic development plans of Ghana."[4] The dam is significant for providing the majority of both Togo and Benin's electricity, although the construction of the Adjarala Dam (on Togo's Mono River) hopes to reduce these countries' reliance on imported electricity.[5] The dam's original electrical output was 912 megawatts (1,223,000 hp), which was upgraded to 1,020 megawatts (1,370,000 hp) in a retrofit project that was completed in 2006.[6]

The flooding that created the Lake Volta reservoir displaced many people and had a significant impact on the local environment,[7] including seismic activity that led to coastal erosion; a changed hydrology caused microclimatic changes with less rain and higher temperatures. The soil surrounding the lake is less fertile than the soil under it, and heavy agricultural use has required the use of fertilizers, which in turn has led to eutrophication, which caused, among others, the explosive growth of an invasive weed that renders water navigation and transportation difficult, and form a habitat for the vectors of water-borne illnesses such as bilharzia, river blindness and malaria. Resettlement of the displaced inhabitants proved complex and in some cases unsuccessful; traditional farming practices disappeared and poverty increased.

Design

The dam was conceived in 1915 by geologist Albert Kitson, but no plans were drawn until the 1940s.[8] The development of the Volta River Basin was proposed in 1949, but because funds were insufficient, the American company Volta Aluminum Company (Valco) lent money to Ghana so that the dam could be constructed. President Kwame Nkrumah adopted the Volta River hydropower project.[4]

The dam is 660 m (2,170 ft) long and 114 m (374 ft) high, comprising a high rock-fill embankment dam. It has a base width of 366 m (1,201 ft) and a structural volume of 7,900,000 m3 (10,300,000 cu yd). The reservoir created by the dam, Lake Volta, has a capacity of 148 km3 (120,000,000 acre⋅ft) and a surface area of 8,502 km2 (3,283 sq mi). The lake is 400 km (250 mi) long. Maximum lake level is 84.73 m (278.0 ft) and minimum is 73.15 m (240.0 ft).[9] On the east side of the dam are two adjacent spillways that can discharge about 34,000 m3/s (1,200,000 cu ft/s) of water. Each spillway contains six 11.5-metre (38 ft)-wide and 13.7-metre (45 ft)-tall steel floodgates.[10][11]

The dam's power plant contains six 170-megawatt (230,000 hp) Francis turbines. Each turbine is supplied with water via a 112–116-metre (367–381 ft) long and 7.2-metre (24 ft) diameter penstock with a maximum of 68.8 m (226 ft) of hydraulic head afforded.[9]

The final proposal outlined the building of an aluminum smelter at Tema, a dam constructed at Akosombo to power the smelter, and a network of power lines installed through southern Ghana. The aluminum smelter was expected to eventually provide the revenue necessary for establishing local bauxite mining and refining, which would allow aluminum production without importing foreign alumina. Development of the aluminum industry within Ghana was dependent upon the proposed hydroelectric power.[4] The proposed project's aluminum smelter was overseen by the American company Kaiser Aluminum and is operated by Valco. The smelter received its financial investment from Valco shareholders, with the support of the Export-Import Bank of the United States. However, Valco did not invest without first requiring insurances from Ghana's government, such as company exemptions from taxes on trade and discounted purchases of electricity. The estimated total cost of the project was $258 million.[4]

Construction

Akosombo dam with open spillways

In May 1960, the Ghana government called for tenders for construction of the hydroelectric dam. In 1961, an Italian consortium, Impregilo which had just completed the Kariba Dam, won the contract. In 1961, the Volta River Authority (VRA) was established by Ghana's Parliament through the passage of the Volta River Development Act. The VRA's fundamental operations were structured by six Board members and Nkrumah as chairman. The VRA's primary task is to manage the development of the Volta River Basin, which included the construction and supervision of the dam, the power station and the power transmission network. The VRA is responsible for the reservoir impounded by the dam, fishing within the lake, lake transportation and communication, and the welfare of those surrounding the lake.[2]

The dam was built between 1961 and 1965.[9] Its development was undertaken by the Ghanaian government and funded 25% by the International Bank for Reconstruction and Development of the World Bank, the United States, and the United Kingdom.[12] Impreglio carried out the dredging of the river bed and dewatering of the channel, and completed the dam a month earlier than scheduled despite flooding of the Volta River in 1963 which delayed work over three months. Between 1961 and 1966, 28 workers of Impregilo died during the construction of the dam. Memorials in Akosombo township and St. Barbara Catholic Church have been put up in their honor.

The construction of the Akosombo Dam resulted in the flooding of part of the Volta River Basin and its upstream fields, and in the creation of Lake Volta which covers 3.6% of Ghana's total land area.[2] Lake Volta was formed between 1962 and 1966 and necessitated the relocation of about 80,000 people, who represented 1% of the population.[13] People of 700 villages were relocated into 52 resettlement villages two years prior to the dam's completion; the resettlement program was under the direction of the VRA.[2][3][7][14] Two percent of the resettlement population were riparian fishers, and most were subsistence farmers.[3] The Eastern Region of Ghana and the populations incorporated within its districts were most subject to the project's effects.[15]

Akosombo Dam on the reverse of a 2007 1 Cedi specimen banknote

Power generation

The dam provides electricity to Ghana and its neighboring West African countries, including Togo and Benin.[15] Initially 20% of Akosombo Dam's electric output (serving 70% of national demand) was provided to Ghanaians in the form of electricity, the remaining 80% was generated for Valco. The Ghana government was compelled, by contract, to pay for over 50% of the cost of Akosombo's construction, but the country was allowed only 20% of the power generated. Some commentators are concerned that this is an example of neocolonialism. In recent years the production from the Valco plant has declined with the vast majority of additional capacity in Akosombo used to service growing domestic demand.[16]

Initially, the dam's power production capabilities greatly overreached the actual demand; while, the demand since the dam's inception has resulted in the doubling of hydropower production.[17] Ghana's industrial and economic expansion triggered a higher demand for power, beyond the Akosombo's power plant capabilities. By 1981, a smaller dam was built at Kpong, downstream from Akosombo, and further upgrades to Akosombo have become necessary for maintaining hydropower output.[2]

Increasing demands for power exceed what can be provided by the current infrastructure. Power demands, along with unforeseen environmental trends, have resulted in rolling blackouts and major power outages.[2][17] An overall trend of lower lake levels has been observed, sometimes below the requirement for operation of the dam.[17]

In the beginning of 2007, concerns were expressed over the electricity supply from the dam because of low water levels in the Lake Volta reservoir.[18] During the latter half of 2007, much of this concern was abated when heavy rain fell in the catchment area of Volta River.[19] In 2010, the highest-ever water level was recorded at the dam. This necessitated the opening of the flood gates at a reservoir elevation of 84.45 m (277 ft), and for several weeks, water was spilled from the lake, causing some flooding downstream.[20]

Impacts

The hydroelectric power plant on Lake Volta

The Akosombo Dam benefited some industrial and economic activities from the addition of lake transportation, increased fishing, new farming activities along the shoreline, and tourism.[7]

Biological habitat

Lake Volta from space

In the time following the construction of the dam, there has been a steady decline in agricultural productivity along the lake and the associated tributaries.[7] The land surrounding Lake Volta is not nearly as fertile as the formerly cultivated land residing underneath the lake, and heavy agricultural activity has since exhausted the already inadequate soils. Downstream agricultural systems are losing soil fertility without the periodic floods that brought nutrients to the soil before the natural river flow was halted by the dam.[17] The growth of commercially intensive agriculture has produced a rise in fertilizer run-off into the river. This, along with run-off from nearby cattle stocks and sewage pollution, has caused eutrophication of the river waters.[7] The nutrient enrichment, in combination with the low water movement, has allowed for the invasion of aquatic weeds (Ceratophyllum). These weeds have become a formidable challenge to water navigation and transportation.[2]

Human welfare

The presence of aquatic weed along the lake and within the tributaries has resulted in even greater detriment to local human health. The weeds provide the necessary habitat for black-fly, mosquitoes and snails, which are the vectors of water-borne illnesses such as bilharzia, river blindness and malaria.[7][21] Since the installation of the dam, these diseases have increased remarkably. In particular, resettlement villages have shown an increase in disease prevalence since the establishment of Lake Volta, and a village's likelihood of infection corresponds to its proximity to the lake.[3] Children and fishermen have been especially hard hit by this rise of disease prevalence.[3] Additionally, the degradation of aquatic habitat has resulted in the decline of shrimp and clam populations.[2] The physical health of local communities has been diminished from this loss of shellfish populations, as they provided an essential source of dietary protein. Likewise, the rural and industrial economies have experienced the financial losses associated with the decimation of river aquaculture.[7]

Increased human migration within the area has been driven by poverty and unfavorable resettlement conditions.[7][17] This migration enabled the contraction of HIV and has since led to its heightened prevalence within Volta Basin communities.[15] The districts of Manya Krobo and Yilo Krobo, which lie within the southwest portion of the Volta Basin, are predominantly indigenous communities that have attained a disproportionate prevalence of HIV.[15] The situation underlines the strength of the local factors upon these districts. Commercial sex work was established in response to the thousands of male workers that were in the area for building the dam.[15] Ten percent of the child-bearing females from these two districts migrated out of their districts during this time.[15] In 1986, "90% of AIDS victims in Ghana were women, and 96% of them had recently lived outside the country".[15]

Socioeconomics

The loss of land experienced by the 80,000 people forcibly relocated meant the loss of their primary economic activities from fishing and agriculture, loss of their homes, loss of their family grave sites, loss of community stability, and the eventual loss of important social values.[7] The resettlement program demonstrated the social complexities involved in establishing "socially cohesive and integrated" communities.[7] Insufficient planning resulted in the relocation of communities into areas that were not capable of providing for their former livelihoods and traditions.[7] The loss of the naturally fertile soils beneath Lake Volta essentially led to the loss of traditional farming practices.[7] The poor living conditions provided within the resettlement villages has been demonstrated by population reductions since resettlement. One resettlement village in particular experienced a greater than 50% population reduction in the 23 years following relocation.[7] Increased economic risks and experiences of poverty are associated with those communities most impacted by the Volta River's development.[2] The extensive human migration and degradation of natural resources within the Volta-basin area, are the products of poverty in conjunction with population pressure.[17]

Physical environment

Reservoir-induced seismicity has been recorded because of the crustal re-adjustments from the added weight of the water within Lake Volta.[7] There is an eastward shift of the river's mouth from the changes to the river's delta, and this has led to continuing coastal erosion. The changes in the river hydrology have altered the local heat budget which has caused microclimatic changes such as decreasing rain and higher mean monthly temperatures. All of these larger scale environmental impacts will all further compound the problems surrounding disruptions to local economic activities and associated, difficult human welfare conditions.[7] A case study by the International Federation of Surveyors has indicated that the dam has had a significant impact on the shoreline erosion of the barrier separating the Keta Lagoon from the sea. Dr. Isaac Boateng has calculated the reduction of fluvial sediment as being from 71 million cubic metres per year to as little as 7 million cubic metres per year.[22]

Spillage

Until 2023, the last time Akosombo dam community experienced flooding as a result of controlled spillage of the dam was in 2010.[23]

On September 15th 2023, the Volta River Authority (VRA) initiated a controlled spillage of water from the Akosombo and Kpong dams situated in the Eastern Region. This controlled spillage led to flooding in communities located along the lower Volta Basin leading to power interruptions. Many victims lost their belongings and livelihood due to the floods.[24] The losses include farmlands, houses and properties which were destroyed by the floods.[25] "My entire farm is under the water and so is my house. I was only able to take my clothes. It took me about 14 years to build this house - there is nowhere to go, there is no other land to build on," according to one victim.[26]

Communities impacted by the flood includes; the districts of North, Central, and South Tongu in the Volta Region, as well as the Asuogyaman District in the Eastern Region. Large portions of Tefle, Wume, Sokpoe, and other riverbank communities have also been affected by the floods, and at least 500 people are now without a place to live. Other localities, such as Alikekope, Agorme, and Agbave, have completely disappeared.[27]

According to the BBC News, the cause of the flood was the heavy rainfall experienced in Ghana during 2023 leading to an increased volume of water in the two dams which in turn led to the Volta River Authority's initiation of controlled spillage of the dam in September 2023.[28]

See also

Notes

  1. "Akosombo Dam could serve Ghana for another 50 years if well maintained – Kweku Awotwi - MyJoyOnline.com". www.myjoyonline.com. Retrieved 18 May 2021.
  2. Fobil 2003
  3. Zakhary 1997
  4. "History of Akosombo dam". Ghana Home Page. Archived from the original on 16 May 2011. Retrieved 8 May 2011.
  5. Europa Publications (2014). Africa South of the Sahara 2014. Routledge. p. 112. ISBN 9781857436983.
  6. "Akosombo Hydro Power Plant Retrofit". Volta River Authority. Archived from the original on 8 August 2007. Retrieved 30 July 2007.
  7. Gyau-Boakye 2001
  8. Okoampa-Ahoofe, Kwame (16 July 2009). "The False Ghanaian History of Paa Kwesi Nduom". The Statesman. Archived from the original on 30 September 2011. Retrieved 11 October 2023.
  9. "Akosombo Hydro Power Plant". Volta River Authority. Archived from the original on 21 April 2007. Retrieved 26 March 2007.
  10. "Akosombo Dam Brochure". Volta River Authority. Retrieved 30 May 2011.
  11. "Annex 3". Alterra. p. 46. Retrieved 30 May 2011.
  12. "Commonwealth Education". Archived from the original on 1 February 2002. Retrieved 15 December 2006.
  13. Matthew Davis (30 May 2003). "Eyewitness: Waking up to water crisis". BBC.
  14. Jackson, Iain; Uduku, Ola; Addo, Irene Appeaning; Opong, Rexford Assasie (19 May 2019). "The Volta River Project: planning, housing and resettlement in Ghana, 1950–1965". The Journal of Architecture. 24 (4): 512–548. doi:10.1080/13602365.2019.1643389. ISSN 1360-2365.
  15. Suave 2002
  16. Kwame Okoampa-Ahoofe (28 August 2007). "NPP cuts sod for Bui Dam". Statesman online. Archived from the original on 30 May 2012. Retrieved 13 October 2007.
  17. Van De Giesen 2001
  18. "Akosombo Dam To Be Shut Down?". Ghana web. 28 March 2007.
  19. "Flood destroys farmlands in Bongo District". 29 August 2007.
  20. "VRA ends spillage from Volta Dam". GhanaWeb. 30 November 2001. Retrieved 30 May 2011.
  21. Drisdelle R (2010). Parasites. Tales of Humanity's Most Unwelcome Guests. Univ of California press, 2010. p. 11f. ISBN 978-0-520-25938-6.
  22. Boateng, Isaac (2010). Spatial Planning in Coastal Regions: Facing the Impact of Climate Change. Copenhagen: International Federation of Surveyors.
  23. "Volta floods: Will the spillage end soon? - MyJoyOnline". www.myjoyonline.com. 19 October 2023. Retrieved 23 October 2023.
  24. GTonline (13 October 2023). "Akosombo Dam spillage: 7 districts hit by floods …farmlands, houses, other properties affected in Greater Accra, Eastern, Volta regions". Ghanaian Times. Retrieved 23 October 2023.
  25. GTonline (13 October 2023). "Akosombo Dam spillage: 7 districts hit by floods …farmlands, houses, other properties affected in Greater Accra, Eastern, Volta regions". Ghanaian Times. Retrieved 23 October 2023.
  26. "Draft:Akosombo Dam spillage", Wikipedia, 21 October 2023, retrieved 23 October 2023
  27. "Draft:Akosombo Dam spillage", Wikipedia, 21 October 2023, retrieved 23 October 2023
  28. "Ghana floods: 'My entire farm is under the water and so is my house'". BBC News. 18 October 2023. Retrieved 23 October 2023.

References

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.