The Aswan Dam is an embankment dam situated across the Nile River in Aswan, Egypt. Since the 1950s, the name commonly refers to the High Dam, which is larger and newer than the Aswan Low Dam, which was first completed in 1902. Following Egypt's independence from the United Kingdom, the High Dam was constructed between 1960 and 1970. It aimed to increase economic production by further regulating the annual river flooding and providing storage of water for agriculture, and later, to generate hydroelectricity. The dam has had a significant impact on the economy and culture of Egypt. Before the dams were built, the Nile River flooded each year during late summer, as water flowed down the valley from its East African drainage basin. These floods brought high water and natural nutrients and minerals that annually enriched the fertile soil along the floodplain and delta; this made the Nile valley ideal for farming since ancient times. Because floods vary, in high-water years, the whole crop might be wiped out, while in low-water years widespread drought and famine occasionally occurred. As Egypt's population grew and conditions changed, both a desire and ability developed to control the floods, and thus both protect and support farmland and the economically important cotton crop. With the reservoir storage provided by these dams, the floods could be lessened, and the water could be stored for later release.

Construction history
The earliest recorded attempt to build a dam near Aswan was in the 11th century, when the Iraqi polymath and engineer Ibn al-Haytham (known as Alhazen in the West) was summoned to Egypt by the Fatimid Caliph, Al-Hakim bi-Amr Allah, to regulate the flooding of the Nile, a task requiring an early attempt at an Aswan Dam. After his field work convinced him of the impracticality of this scheme, and fearing the Caliph's anger, he feigned madness. He was kept under house arrest from 1011 until al-Hakim's death in 1021, during which time he wrote his influential Book of Optics .

Aswan Low Dam
Following their 1882 invasion and occupation of Egypt, the British began construction of the first dam across the Nile in 1898. Construction lasted until 1902, and it was opened on 10 December 1902, by HRH the Duke of Connaught and Strathearn. The project was designed by Sir William Willcocks and involved several eminent engineers of the time, including Sir Benjamin Baker and Sir John Aird, whose firm, John Aird & Co., was the main contractor.

Aswan High Dam Politics and Funding
After the Low Dam was almost over-topped in 1946, the British administration decided that rather than raise the dam a third time, a second dam should be built some 7 km upriver. The post-war years saw major changes in Egypt, including the growth of nationalism, the abrogation of the Anglo-Egyptian Treaty of 1936, and the overthrow of the monarchy, led by the Free Officers Movement, and its ultimate leader, Gamal Abdel Nasser. Planning for the "High Dam" proper began in 1954, following the revolution, and changed development priorities. Initially, both the US and USSR were interested in the development of the dam, but this occurred in the increasingly tense readings of Cold War happenings, as well as growing intra-Arab rivalries. In 1955 Nasser was trying to portray himself as the leader of Arab nationalism, in opposition to the traditional monarchies, especially Hashemite Iraq following its signing of the 1955 Baghdad Pact. At that time the US feared that communism would spread to the Middle East, and saw Nasser as a natural leader of an anti-communist Arab league. The US and Britain offered to help finance construction of the high dam with a loan of US$270 million in return for Nasser's leadership in resolving the Arab-Israeli conflict. While opposed both to communism and imperialism, Nasser presented himself as a tactical neutralist, and sought to work with both the US and USSR for Egyptian and Arab benefit. After a particularly criticized raid by Israel against Egyptian forces in Gaza in 1955, Nasser realised that he could not legitimately portray himself as the leader of pan-Arab nationalism if he could not defend his country militarily against Israel. In addition to his development plans, he looked to quickly modernise his military, and turned first to the US. US Secretary of State John Foster Dulles and US President Dwight Eisenhower told Nasser that the US would supply him with weapons only if they were used for defensive purposes and accompanied by US military personnel for supervision and training. Nasser did not accept these conditions and then looked to the Soviet Union for support. Although Dulles believed that Nasser was only bluffing, and that the USSR would not aid Nasser, he was wrong; the USSR promised Nasser a quantity of arms in exchange for a deferred payment of Egyptian grain and cotton. On 27 September 1955, Nasser announced an arms deal, with Czechoslovakia acting as a middleman for the Soviet support. Instead of retaliating against Nasser for turning to the Soviets, Dulles sought to improve relations with him. This explains the later offer of December 1955, in which the US and UK pledged $56 and $14 million respectively towards the construction of the dam. Though the "Czech arms deal" actually increased US willingness to invest in Aswan, the British cited the deal as a reason for withdrawing their funding. What angered Dulles much more was Nasser’s recognition of communist China, which was in direct conflict with Dulles' policy of containment. There are several other reasons why the US decided to withdraw the offer of funding. Dulles believed that the Soviet Union would not fulfill its commitment to help the Egyptians. He was also irritated by Nasser’s neutrality and attempts to play both sides of the Cold War. At the time, other western allies in the Middle East, including Turkey and Iraq, were irritated that Egypt, a persistently neutral country, was being offered so much aid. In June 1956 the Soviets offered Nasser $1,120,000,000 at 2% interest for the construction of the dam. On 19 July the US State Department announced that it deemed American financial assistance for the High Dam "not feasible in present circumstances." On 26 July 1956, with wide Egyptian acclaim, Nasser announced the nationalization of the Suez Canal as well as fair compensation for the former owners. Nasser planned on the revenues generated by the canal helping to fund construction of the High Dam. The Suez War broke out, The United Kingdom, France, and Israel were mainly successful in attaining their immediate military objectives, but pressure from the US and the USSR at the United Nations and elsewhere forced them to withdraw. In 1958 the Soviet Union provided funding for the dam project. In the 1950s archaeologists began raising concerns that several major historical sites were about to be under water. A rescue operation began in 1960 under UNESCO. The Great Temple of Abu Simbel was preserved by relocating 22 monuments and architectural complexes to the shores of Lake Nasser under the UNESCO Nubia Campaign. Other monuments were granted to countries that helped with the works (such as the Debod temple in Madrid, the Temple of Taffeh in Leiden and the Temple of Dendur in New York). The remaining archeological sites have been flooded by Lake Nasser, among others the Buhen fort.

Construction and filling 1960-1976
The Soviets also provided technicians and heavy machinery. The enormous rock and clay dam was designed by the Soviet Hydroproject Institute along with some Egyptian engineers. 25 thousand Egyptian engineers and workers formed the backbone of the workforce required to complete this tremendous project which deeply changed many aspects in Egypt. On the Egyptian side, the project was led by Osman Ahmed Osman's Arab Contractors. The relatively young Osman underbid his only competitor by one-half.

1960: Start of construction on 9 January 1964: First dam construction stage completed, reservoir started filling 1970: The High Dam, as-Sad al-'Aali, completed on 21 July 1976: Reservoir reached capacity

The Aswan High Dam is 3,830 meters long, 980 meters wide at the base, 40 meters wide at the crest and 111 meters tall. It contains 43 million cubic meters of material. At maximum, 11,000 cubic meters per second of water can pass through the dam. There are further emergency spillways for an extra 5,000 cubic meters 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 square kilometers. It holds 111 cubic kilometers of water.

The main benefits of the High Dam are protection from floods and droughts, an increase in agricultural production and employment, electricity production and improved navigation that benefits tourism. The assessment of the costs and benefits of the dam remains a controversial issue decades after its completion. According to one estimate, the annual economic benefits of the High Dam right after its completion were Egyptian Pound (EP) 255 million (US$587m using the 1970 exchange rate of 2.3 US$ per EP): EP140 million from agricultural production, EP100 million from hydroelectric generation, EP10 million from flood protection, and EP5 million from improved navigation. At the time of its construction, total cost, including unspecified "subsidiary projects" and the extension of electric power lines, amounted to Egyptian EP450 million. Not taking into account the negative environmental and social impacts of the dam, its costs are thus estimated to have been recovered within only two years. One observer notes: "The impacts of the Aswan High Dam (...) have been overwhelmingly positive. Although the Dam has contributed to some environmental problems, these have proved to be significantly less severe than was generally expected, or currently believed by many people." Another observer disagrees and recommended that the dam should be torn down. Tearing it down would cost only a fraction of the funds required for "continually combating the dam's consequential damage" and 500,000 hectares of fertile land could be reclaimed from the layers of mud on the bed of the drained reservoir.

Drought protection, agricultural production and employment
The dams also protected Egypt from the droughts in 1972-1973 and 1983-1987 that devastated East and West Africa. The High Dam allowed Egypt to reclaim about 2 million feddan (840,000 hectares) from the in the Delta and along the Nile Valley, increasing the country's irrigated area by a third. The increase was brought about both by irrigating what used to be desert and by bringing under cultivation of 385,000 ha that were previously used as flood retention basins. About half a million families were settled on these new lands. In particular the area under rice and sugar cane cultivation increased. In addition, about 1 million feddan (420,000 hectares), mostly in Upper Egypt, were converted from flood irrigation with only one crop per year to perennial irrigation allowing two or more crops per year. On other previously irrigated land, yields increased because water could be made available at critical low-flow periods. For example, wheat yields in Egypt tripled between 1952 and 1991 and better availability of water contributed to this increase. Most of the 32 km³ of freshwater, or almost 40% of the average flow of the Nile that were previously lost to the sea every year could now be put to beneficial use. While about 10 km³ of the water saved is lost due to evaporation in Lake Nasser, the amount of water available for irrigation still increased by 22 km³.

Electricity production
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 most Egyptian villages to use electricity for the first time. The High Dam has also improved the efficiency and the extension of the Old Aswan Hydropower stations.

Other benefits
Flood protection. Periodic floods and droughts have affected Egypt since ancient times. The dam mitigated the effects of floods, such as in 1964, 1973 and 1988. Navigation and tourism. Navigation along the river has been improved, both upstream and downstream of the dam. Sailing along the Nile from Cairo to is a favorite tourism activity, which is mainly done during winter when the natural flow of the Nile would have been too low to allow navigation of cruise ships. Fishing in Lake Nasser. A new fishing industry has been created around Lake Nasser, though it is struggling due to its distance from any significant markets. The annual production was about 35 000 tons in the mid-90s. Factories for the fishing industry and packaging have been set up near the Lake.

Environmental and social impact
The High Dam had a number of environmental and social impacts. Some but not all impacts were anticipated, and the impacts were mitigated to different degrees. Among the impacts that were anticipated were the resettlement of the Nubian population in the area inundated by the reservoir, the saving of historic monuments, the loss of soil fertility, health impacts and coastal erosion. Some anticipated impacts materialized only gradually and were mitigated only after a long delay and at great cost, such as waterlogging and soil salinization. In the case of some other anticipated impacts, it is not clear if they have been mitigated or not, such as the impact on Mediterranean fisheries. Some anticipated impacts could simply not be mitigated, such as reservoir evaporation and sedimentation. Some anticipated impacts did not materialize, such as massive seepage from the reservoir, or were less severe than expected, such as river-bed erosion. There were also some impacts that were apparently not anticipated, such as the loss of arable land because the brick-making industry used alluvial deposits from existing lands instead of the annual sediment deposits.

Lake Nasser flooded much of lower Nubia and 100,000 to 120,000 people were resettled in Sudan and Egypt. The majority of the 50,000 Nubians resettled in Egypt were resettled three to ten kilometers from the Nile near Kom Ombo 45 kilometers downstream from Aswan in what was called " New Nubia". Housing and facilities were built for 47 village units whose relationship to each other approximated that in Old Nubia. Irrigated land was provided to grow mainly sugar cane. In Sudan 50,000 to 70,000 Sudanese Nubians were moved approximately 700 kilometers south to the semi-arid Butana plain near the town of Khashm el-Girba several hundred kilometers up the Atbara River. The climate there had a regular rainy season as opposed to their previous desert habitat in which virtually no rain fell. Unlike in Egypt, the host population included no Nubians. The government developed an irrigation project, called the New Halfa Agricultural Development Scheme to grow cotton, grains, sugar cane and other crops. The Nubians were resettled in 25 planned villages that included schools, medical facilities and other services including piped water and some electrification.

Loss of sediments and soil fertility
Before the construction of the High Dam the Nile deposited sediments of various particle size - consisting of fine sand, silt and clay - on fields in Upper Egypt through its annual flood, contributing to soil fertiliy. However, the nutrient value of the sediment has often been overestimated. 88% of the sediment was carried to the sea before the construction of the High Dam. The nutrient value added to the land by the sediment was only 6,000 tons of potash, 7,000 tons of phosphorous pentoxide and 17,000 tons of nitrogen. These amounts are insignificant compared to what is needed to reach the yields achieved today in Egypt's irrigation. Also, the annual spread of sediment due to the Nile floods occurred along the banks of the Nile. Areas far from the river are now being irrigated which never received the Nile floods before.

Waterlogging and increase in soil salinity
Before the construction of the High Dam, groundwater levels in the Nile Valley fluctuated 8-9m per year with the water level of the Nile. During summer when evaporation was highest, the groundwater level was too deep to allow salts dissolved in the water to be pulled to the surface through capillary action. With the disappearance of the annual flood and heavy year-round irrigation, groundwater levels remained high with little fluctuation leading to waterlogging. Soil salinity also increased because the distance between the surface and the groundwater table was small enough (1”“2 m depending on soil conditions and temperature) to allow water to be pulled up by evaporation so that the relatively small concentrations of salt in the groundwater accumulated on the soil surface over the years. Since most of the farmland did not have proper subsurface drainage to lower the groundwater table, salinization gradually affected crop yields. A total of 2.1 million hectares thus required subsurface drainage at a cost that exceeded the construction cost of the High Dam. Only 20 years after completion of the High Dam the problem was seriously addressed and a large-scale drainage program was initiated.

Coastal erosion
The High Dam has accelerated erosion of coastlines (due to lack of sediment, which was once brought by the Nile) in Egypt and, according to some sources even all along the eastern Mediterranean. Coastal erosion occurred and efforts to control it were made even before the construction of the High Dam. This erosion may to some extent have been caused by the limited trapping of sediments behind the Old Aswan Dam. The High Dam accelerated erosion and made the construction of further expensive coastal protection works in the Nile Delta necessary.

Health impact
The standing water in irrigation canals is a breeding ground for snails carrying the parasite bilharzia. The incidence of bilharzia increased due to the Aswan High Dam inhibiting the natural fluctuations in water height. Important factors contributing to the prevalence of schistosomiasis were poor sanitation and limited awareness of how the disease was transmitted. Provision of clean water, sanitation, health education and rural clinics has reduced the overall prevalences of schistosomiasis from more than 40 per cent during the pre-dam period to 10 per cent in 1995 and only 2% in 2002.

Historical monuments
A number of historical monuments were located in the area that was flooded by Lake Nasser. UNESCO and the Egyptian authorities transferred many of them to higher ground, including Abu Simbel, Philae, Kalabsha and Amada, which are important tourism attractions today.

Other impacts
Reservoir sedimentation. Sediment deposited in the reservoir is lowering the water storage capacity of Lake Nasser. The reservoir storage capacity is 162 km 3, including 31 km 3 dead storage at the bottom of the lake below 147m above sea level, 90 km 3 live storage, and 41 km 3 of storage for high flood waters above 175m above sea level. The annual sediment load of the Nile is about 134 million tons. This means that the dead storage volume would be filled up after 300”“500 years if the sediment accumulated at the same rate throughout the area of the lake. Obviously sediment accumulates much faster at the upper reaches of the Lake where sedimentation has already affected the live storage zone. It would take about another 900 years until the live storage zone would be completely sedimented and operation of the dam would become impossible some time before that. Reservoir evaporation. Evaporation from Lake Nasser is estimated at 10 km 3 per year, varying mainly as a function of the lake area. While the absolute amount of water lost to evaporation is enormous, it is only 11% of the average volume stored in the Lake and 18% of Egypt's share of the annual flow of the Nile. Aquatic weeds. Before the construction of the High Dam, the 50,000 km of irrigation and drainage canals in Egypt had to be dredged regularly to remove sediments. After construction of the dam, aquatic weeds grew much faster in the clearer water, helped by fertilizer residues. The total length of the infested waterways was about 27,000 km in the mid-90s. Weeds have been gradually brought under control by manual, mechanical and biological methods. Pollution from fertilizers. The increased use of artificial fertilizers in farmland below the dam has caused chemical pollution which the traditional river sediment did not do. Fishery in the Delta and the Mediterranean. Mediterranean fishing and brackish water lake fishery declined after the dam was finished because nutrients that used to flow down the Nile to the Mediterranean were trapped behind the dam. For example, the Sardine catch off the Egyptian coast declined from 18,000 tons in 1962 to a mere 460 tons in 1968, but then gradually recovered to 8,590 tons in 1992. A scientific article in the mid-1990s noted that " the mismatch between low primary productivity and relatively high levels of fish production in the region still presents a puzzle to scientist." Impact on currents and salinity in the Mediterranean. 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. River-bed erosion. A concern before the construction of the High Dam had been the potential drop in river-bed level downstream of the Dam as the result of erosion caused by the flow of sediment-free water. Estimates by various national and international experts put this drop at between 2 and 10 metres. Hoiwever, the actual drop has been measured at 0.3-0.7m, much less than anticipated. Brick industry. The red-brick construction industry, which consisted of hundreds of factories that used Nile sediment desposits along the river, has also been negatively affected. Deprived of sediment, they started using the older alluvium of otherwise arable land taking out of production up to 120 square kilometers annually, with an estimated 1,000 square kilometers destroyed by 1984 when the government prohibited, “with only modest success,” further excavation. According to one source, bricks are now being made from new techniques which use a sand-clay mixture and it has been argued that the mud-based brick industry would have suffered even if the dam had not been built. Algae growth. Because of the lower turbidity of the water sunlight penetrates deeper in the Nile water. Because of this and the increased presence of nutrients from fertilizers in the water, more algae grow in the Nile. This in turn increases the costs of drinking water treatment. Apparently few experts had anticipated that water quality in the Nile would actually decrease because of the High Dam.

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 which has a growing period of almost one year. The high dam at Aswan releases, on average, 55 km³ water per year of which some 46 km³ are diverted into the irrigation canals. In the Nile valley and delta, almost 33,600 square kilometres benefit from these waters producing on average 1.8 crops per year. The annual crop consumptive use of water is about 38 cubic kilometres. Hence, the overall irrigation efficiency is 38/46 = 0.82 or 82%. This is a relatively high irrigation efficiency. 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 following table shows that the equal distribution of irrigation water over the branch canals taking off from the main irrigation canals leaves much to be desired:

*) Data from the Egyptian Water Use Management Project (EWUP) Salt balance The salt concentration of the water in the Aswan reservoir is about 0.25 kg/m³, a very low salinity level. At an annual inflow of 55 km³, the annual salt import reaches 14 million tons. The average salt concentration of the drainage water evacuated into the sea and the coastal lakes is 2.7 kg/m³. At an annual discharge of 10 km³ (not counting the 2 km³ 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. Drainage Drainage through sub-surface drains and drainage channels is essential to prevent a deterioration of crop yields from waterlogging and soil salinization caused by irrigation. By 2003 more than 20000 square kilometres have been equipped with a subsurface drainage system and approximately 7.2 km 3 of water is drained annually from areas with these systems. The total investment cost in agricultural drainage over 27 years from 1973 to 2002 was about 3.1 billion US$ covering the cost of design, construction, maintenance, research and training. During this period 11 large scale projects were implemented with financial support from World Bank and other donors

Branch canal Water delivery in m³ Kafret Nasser 4700 Beni Magdul 3500 El Mansuria 3300 El Hammami upstream 2800 El Hammami downstream 1800 El Shimi 1200


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