Information about Aswan Dam

The hydroelectric power station of Aswan Dam
Construction history
The British began construction of the first dam in 1899. Construction lasted until 1902. It was opened in December 10, 1902. The project was designed by Sir William Willcocks and involved several eminent engineers including Sir Benjamin Baker and Sir glodstein McnabbJohn Aird, whose firm, John Aird & Company, was the main contractor. A gravity dam, it was 1,900 m long and 54 m high. The initial design was soon found to be inadequate and the height of the dam was raised in two phases, 1907–1912 and 1929–1933.When the dam almost overflowed in 1946 it was decided that rather than raise the dam a third time, a second dam would be built 6 km upriver (about 4 miles). Proper planning began in 1952, just after the Egyptian Revolution led by the Free Officers, of whom Nasser was to become leader. At first the USA and Britain were to help finance construction with a loan of USD $270 million in return for Nasser's leadership on resolving the Arab-Israeli Conflict. However both nations cancelled the offer in July 1956 as part of the secret US-led 'OMEGA' policy to marginalize Nasser. A secret Egyptian arms agreement with Czechoslovakia (Eastern Bloc) and Egyptian recognition of the People's Republic of China are cited as possible reasons.
The Soviet Union stepped in in 1958 and funded the dam project as part of the struggle for influence in Africa during the Cold War, and possibly a third of the cost of the dam was paid for as a long term investment in the region. The Soviets also provided technicians and heavy machinery. The enormous rock and clay dam was designed by the Russian Zuk Hydroproject Institute.
A panorama of Aswan Dam
Construction began in 1960. The High Dam, as-Sad al-'Aali, was completed on July 21, 1970, with the first stage finished in 1964. The reservoir began filling in 1964 while the dam was still under construction and first reached capacity in 1976. The reservoir raised concerns from archaeologists and a rescue operation was begun in 1960 under UNESCO. Sites were to be surveyed and excavated and 24 major monuments were moved to safer locations (see Abu Simbel) or granted to countries that helped with the works (such as the Debod temple in Madrid and the Temple of Dendur in New York).
Specifications
The Aswan High Dam is 3,600 m in length, 980 m wide at the base, 40 m wide at the crest and 111 m tall. It contains 43 million m³ of material. At maximum, 11,000 m³ of water can pass through the dam every second. There are further emergency spillways for an extra 5000 m³ per second and the Toshka Canal links the reservoir to the Toshka Depression. The reservoir, named Lake Nasser, is 550 km long and 35 km at its widest with a surface area of 5,250 km² and holds 111 km³.Benefits
The dam powers twelve generators each rated at 175 megawatts, producing a hydroelectric output of 2.1 gigawatts. Power generation began in 1967. When the dam first reached peak output it produced around half of Egypt's entire electricity production (about 15% by 1998) and allowed for the connection of most Egyptian villages to electricity for the first time. The dam mitigated the effects of dangerous floods in 1964 and 1973 and of threatening droughts in 1972–73 and 1983–84. A new fishing industry has been created around Lake Nasser, though it is struggling due to its distance from any significant markets.Environmental and cultural issues
A view from the vantage point in the middle of High Dam towards the "Lotus Flower" tower by the sculptor Ernst Neizvestny.
There is some erosion of farmland down-river. Erosion of coastline barriers, due to lack of new sediments from floods, will eventually cause loss of the brackish water lake fishery that is currently the largest source of fish for Egypt, and the subsidence of the Nile Delta will lead to inundation of the northern portion of the delta with seawater, in areas which are now used for rice crops. The delta itself, no longer renewed by Nile silt, has lost much of its fertility. The red-brick construction industry, which used delta mud, is also severely affected. There is significant erosion of coastlines (due to lack of sand, which was once brought by the Nile) all along the eastern Mediterranean.
The need to use artificial fertilizers supplied by international corporations is controversial too, causing chemical pollution which the traditional river silt did not. Indifferent irrigation control has also caused some farmland to be damaged by waterlogging and increased salinity, a problem complicated by the reduced flow of the river, which allows salt water to encroach further into the delta.
Mediterranean fish stocks are also negatively affected by the dam. The eastern basin of the Mediterranean is low in fertility, and traditionally the marine ecosystem depended on the rich flow of phosphate and silicates from the Nile outflow. Mediterranean catches decreased by almost half after the dam was constructed. The dam has been implicated in a rise in cases of schistosomiasis (bilharzia), due to the thick plant life that has grown up in Lake Nasser, which hosts the snails who carry the disease.
The Aswan dam tends to increase the salinity of the Mediterranean Sea, and this affects the Mediterranean's outflow current into the Atlantic ocean (see Strait of Gibraltar). This current can be traced thousands of kilometers into the Atlantic.
Irrigation for agriculture
Due to the absence of appreciable rainfall, Egypt's agriculture depends entirely on irrigation. With irrigation, two crops per year can be produced, except for sugar cane that has a growing period of almost one year. The high dam at Aswan releases on average 55 billion m3 water per year of which some 46 billion m3 are diverted into the irrigation canals. In Nile valley and delta, almost 8 million feddan (1 feddan is about 1 acre or 0.42 ha) benefit from these waters producing on average 1.8 crop per year. The annual crop consumptive use is about 38 billion m3. Hence, the overall irrigation efficiency is 38/46 = 0.82 or 82%.Compared to the efficiency elswhere in the world this is a high value. The field irrigation efficiencies are much less, but the losses are re-used downstream. This continuous re-use accounts for the high overall efficiency. The equal distribution of irrigation water over the branch canals taking off from the main irrigation canals leaves to be desired.[1]
| Branch canal | Water delivery in m3/feddan* |
|---|---|
| Kafret Nasser | 4700 |
| Beni Magdul | 3500 |
| El Mansuria | 3300 |
| El Hammami upstream | 2800 |
| El Hammami downstream | 1800 |
| El Shimi | 1200 |
The salt concentration of the water in the Aswan reservoir is about 0.25 kg/m3. This is very "sweet" water. At an annual inflow of 55 billion m3, the annual salt import reaches 14 million ton. The average salt concentration of the drainage water evacuated into the sea and the coastal lakes is 2.7 kg/m3 (Egyptian Drainage Research Institute, yearbook 1995/1996). At an annual discharge of 10 billion m3 (not counting the 2 billion m3 of salt intrusion from the sea and the lakes, see figure "Water balances"), the annual salt export reaches 27 million ton. In 1995, the salt export was higher than the import, and Egypt's agricultural lands were desalinizing. Part of this could be due to the large number of subsurface drainage projects executed in the last decades to control the water table and soil salinity.
References
1. ^ R.J.Oosterbaan, 1999. Impacts of the Irrigation Improvement Projects in Egypt. Egyptian-Dutch Advisory Panel and International Institute for Land Reclamation and Improvement, Wageningen, The Netherlands.
External links
- Sayed El-Sayed and Gert L. van Dijken 'The southeastern Mediterranean ecosystem revisited: Thirty years after the construction of the Aswan High Dam.'
- Satellite views on Google Maps
- Aswan High Dam
- Old Aswan Dam
- http://maps.google.com/maps?hl=en&ie=UTF8&z=14&ll=24.034001,32.865901&spn=0.056362,0.078535&t=k&om=1
- Info on the Aswan Dam
geographic coordinate system enables every location on the earth to be specified by the three coordinates of a spherical coordinate system aligned with the spin axis of the Earth.
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Aswan (Egyptian: Swenet (=trade); Coptic: Swān; Greek: Συήνη Syene; Arabic: أسوان Aswān
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cataracts of the Nile are shallow stretches between Aswan and Khartoum where the water's surface is broken by numerous small boulders and stones lying on the river bed, as well as many small rocky islets.
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Origin Africa
Mouth Mediterranean Sea
Basin countries Sudan, Burundi, Rwanda, DR Congo, Tanzania, Kenya, Uganda, Ethiopia, Egypt
Length 6,650 km (4,132 mi)
Source elevation 1,134 m (3,721 ft)
Avg.
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Mouth Mediterranean Sea
Basin countries Sudan, Burundi, Rwanda, DR Congo, Tanzania, Kenya, Uganda, Ethiopia, Egypt
Length 6,650 km (4,132 mi)
Source elevation 1,134 m (3,721 ft)
Avg.
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Gumhūriyyat Miṣr al-ʿArabiyyah
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Arab Republic of Egypt
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al-‘Arabiyyah in written Arabic (Kufic script):
Pronunciation: /alˌʕa.raˈbij.ja/
Spoken in: Algeria, Bahrain, Egypt, Iraq, Jordan, Kuwait, Lebanon, Libya, Mauritania, Morocco, Oman,
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Pronunciation: /alˌʕa.raˈbij.ja/
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ṣdʾm ḥsyn, which is meaningless to an untrained reader.
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Origin Africa
Mouth Mediterranean Sea
Basin countries Sudan, Burundi, Rwanda, DR Congo, Tanzania, Kenya, Uganda, Ethiopia, Egypt
Length 6,650 km (4,132 mi)
Source elevation 1,134 m (3,721 ft)
Avg.
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Mouth Mediterranean Sea
Basin countries Sudan, Burundi, Rwanda, DR Congo, Tanzania, Kenya, Uganda, Ethiopia, Egypt
Length 6,650 km (4,132 mi)
Source elevation 1,134 m (3,721 ft)
Avg.
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flood is an overflow of an expanse of water that submerges land, a deluge.[1] In the sense of "flowing water", the word is applied to the inflow of the tide, as opposed to the outflow or "ebb".
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A crop is any plant that is grown in significant quantities to be harvested as food, livestock fodder, or for another economic purpose. This category includes crop species as well as agricultural techniques related to cropping.
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drought is an extended period of months or years when a region notes a deficiency in its water supply. Generally, this occurs when a region receives consistently below average precipitation. It can have a substantial impact on the ecosystem and agriculture of the affected region.
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Agriculture (from Agri Latin for ager ("a field"), and culture, from the Latin cultura "cultivation" in the strict sense of "tillage of the soil". A literal reading of the English word yields "tillage of the soil of a field".
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Sir William Willcocks KCMG (September 27, 1852, India – July 28, 1932, Cairo, Egypt) was a British civil engineer. He is remembered as a renowned irrigation engineer, having proposed the first Aswan Dam and undertaken major projects of irrigation in South Africa and Turkey.
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Sir Benjamin Baker (March 31, 1840 - May 19, 1907), English engineer, was born near Bath in 1840, and, after receiving his early training in a South Wales ironworks, became associated with Sir John Fowler in London.
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Sir John Aird, 1st Baronet (3 December 1833 - 6 January 1911) was a notable English civil engineering contractor of the late 19th and early 20th centuries. He also served as Conservative Member of Parliament (MP) for Paddington North from 1887 to 1906, was the first Mayor of
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The 1952 Revolution (Arabic:ثورة 23 يوليو 1952), in Egypt also known as the July 23 Revolution, began with a military coup d'état that took place on July 23, 1952 by a group of young army officers who named themselves
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Gamal Abdel Nasser (Arabic: جمال عبد الناصر - Gamāl ‘Abd an-Nāṣir
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The 'OMEGA' memorandum [1] of March 21, 1956, was a secret United States informal policy memorandum drafted by Secretary of State John Foster Dulles for President Dwight D. Eisenhower.
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Czechoslovakia (Czech Československo; 1938 - 1939 and Slovak since 1990: Česko-Slovensko) was a sovereign state in Eastern-Central Europe that after declaring its independence from the Austro-Hungarian Empire, existed from October 1918 until 1992 (with
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Eastern Bloc (or Soviet Bloc) was used to refer to the Soviet Union and its allies in Central and Eastern Europe (Bulgaria, Czechoslovakia, East Germany, Hungary, Poland, Romania, and—until the early 1960s—Albania).
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