Akosombo Dam Case Study Gcse At Home

Akosombo Dam

Akosombo Dam as seen from the Volta Hotel

Location of the Akosombo Dam in Ghana

LocationAkosombo, Ghana
Coordinates6°17′59″N0°3′34″E / 6.29972°N 0.05944°E / 6.29972; 0.05944Coordinates: 6°17′59″N0°3′34″E / 6.29972°N 0.05944°E / 6.29972; 0.05944
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-gontrolled
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 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. 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 is located between Zimbabwe and Zambia in Southern Africa and contains 185 cubic kilometers of water.[1]

The primary purpose of the Akosombo Dam was to provide electricity for the aluminium industry.[2] The Akosombo Dam was called "the largest single investment in the economic development plans of Ghana."[3] Its 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.[4]

The flooding that created the Lake Volta reservoir displaced many people and had a significant impact on the environment.[5]

History[edit]

The dam was conceived in 1915 by geologist Albert Ernest Kitson, but no plans were drawn until the 1940s.[6] The development of the Volta River Basin was proposed in 1949, but because funds were insufficient, the American company Volta Aluminum Company (Valco) loaned money to Ghana so that the dam could be constructed. Kwame Nkrumah adopted the Volta River hydropower project.[3]

The final proposal outlined the building of an aluminumsmelter 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.[3] 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 Washington, DC. 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, in its entirety, was estimated at $258 million.[3]

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. They 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.

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 Kwame 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, the fishing within the lake, lake transportation and communication, and the welfare of those surrounding the lake.[1]

The dam was built between 1961 and 1965.[7] 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.[8]

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.[1] Lake Volta was formed between 1962 and 1966, and necessitated the relocation of about 80,000 people, who represented 1% of the population.[9] People of 700 villages were relocated into 52 resettlement villages two years prior to the lake's completion; the resettlement program was under the direction of the VRA.[1][2][5] Two percent of the resettlement population were riparian fishers and most were subsistence farmers.[2] The Eastern Region of Ghana and the populations incorporated within its districts, were most subject to the project’s effects.[10]

In the beginning of 2007, concerns were expressed over the electricity supply from the dam due to low water levels in the Lake Volta reservoir.[11] Some sources said this was due to problems with drought that are a consequence of global warming.[12] During the latter half of 2007, much of this concern was abated when heavy rain fell in the catchment area of Volta River.[13] 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.[14]

Design[edit]

The dam is 660 m (2,170 ft) long and 114 m (374 ft), 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).[7] 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.[15][16]

Akosombo Power Station[edit]

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.[7]

Power distribution[edit]

The dam provides electricity to Ghana and its neighboring West African countries, including Togo and Benin. 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 the American-owned Volta Aluminum Company (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.[17]

Impacts[edit]

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.[5] The power generated has provided for primary interests within Ghana, while also supplying power to the neighboring countries of Togo and Benin.[10] 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 the town of Kpong, downstream from Akosombo and further upgrades to Akosombo have become necessary for maintaining hydropower output.[1] 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.[18] 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.[1][18] An overall trend of lower lake levels has been observed, sometimes below the requirement for operation of the Akosombo Dam.[18]

Biological habitat[edit]

In the time following the construction of the dam at Akosombo, there has been a steady decline in agricultural productivity along the lake and the associated tributaries.[5] 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 floodings that brought nutrients to the soil before the natural river flow was halted by the dam.[18] 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.[5] 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.[1]

Human welfare[edit]

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.[5] Since the installment 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.[2] Children and fishermen have been especially hard hit by this rise of disease prevalence.[2] Additionally, the degradation of aquatic habitat has resulted in the decline of shrimp and clam populations.[1] 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.[5]

Socioeconomics[edit]

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.[5] The resettlement program demonstrated the social complexities involved in establishing "socially cohesive and integrated" communities.[5] Insufficient planning resulted in the relocation of communities into areas that were not capable of providing for their former livelihoods and traditions.[5] The loss of the naturally fertile soils beneath Lake Volta essentially led to the loss of traditional farming practices.[5] 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.[5] Increased economic risks and experiences of poverty are associated with those communities most impacted by the Volta River’s development.[1] The extensive human migration and degradation of natural resources within the Volta-basin area, are the products of poverty in conjunction with population pressure.[18]

Disease[edit]

Increased human migration within the area has been driven by poverty and unfavorable resettlement conditions.[5][18] This migration enabled the contraction of HIV and has since led to its heightened prevalence within Volta Basin communities.[10] 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.[10] 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.[10] Ten percent of the child-bearing females from these two districts migrated out of their districts during this time.[10] In 1986, "90% of AIDS victims in Ghana were women, and 96% of them had recently lived outside the country".[10]

The Akosombo Dam and other dams of the Volta River Hydro Development Project increased substantially the conditions for the spread of schistosomiasis.[19]

Physical environment[edit]

Reservoir-induced seismicity has been recorded due to the crustal re-adjustments from the added weight of the water within Lake Volta.[5] There is an eastward shift of the river’s mouth from the changes to the river’s delta zone 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.[5] 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 m3/a[clarification needed] to as little as 7 million m3/a.[20]

See also[edit]

References[edit]

Bibliography[edit]

  • Fobil, J.N., D.K. Attaquayefio, and Volta Basin Research Project [VBRP]. 2003. Remediation of the environmental impacts of the Akosombo and Kpong dams. HORIZON Solutions Site: Public Health. Yale University Department of Biology: HORIZON International.
  • Gyau-Boakye, P. 2001. Environmental impacts of the akosombo dam and effects of climate change on the lake levels. Environment, Development and Sustainability 3(1): 17-29.
  • Suave, N., A. Dzokoto, B. Opare et al. 2002. The price of development: HIV infection in a semiurban community of Ghana. Journal of Acquired Immune Deficiency Syndrome [JAIDS] 20(4): 402-408.
  • Van De Giesen, N., M. Andreini, A. Van Edig and P. Vlek. 2001. Competition for water resources of the Volta basin. Regional Management of Water Resources. IAHS Publ. no. 268: 199-205.
  • Zakhary, K. 1997. Factors affecting the prevalence of schistosomiasis in the Volta region of Ghana. McGill Journal of Medicine 3: 93-101.

External links[edit]

Akosombo dam with open spillways
The hydroelectric power plant on Lake Volta

Case study: management of water usage in MEDCs

Elan Valley Water Transfer Scheme

Much of Birmingham's tap water comes from over 100 km away. There are five dams in the Elan Valley which can supply Birmingham with 160 million litres of water a day.

The Craig Goch Dam, Elan Valley.

Reasons for choosing the Elan valley location

  • Deep narrow valleys to hold the water in.
  • Impermeable rock means the water wouldn't leak away.
  • A high annual rainfall of 1830 mm.
  • The area is higher than Birmingham, so the water can flow using gravity rather than pumps.

Pen-Y-Garreg reservoir, Elan Valley

Future expansion of the scheme raises problems. The local environment would be damaged. There would be increased traffic and noise from the construction of dams to provide extra capacity. The river flow downstream would be affected, along with the wildlife. Also more land would be affected when pipes are run across it.

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