Nubian Sandstone Aquifer System

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The transport of pipe segments for the Great Manmade River in the Sahara desert, Libya: a network of pipes that supplies water from the Nubian Sandstone Aquifer System, a fossil aquifer in the Sahara Desert of Libya. The Great Manmade River is the world's largest irrigation project.

The Nubian Sandstone Aquifer System (NSAS) is the world’s largest known fossil water aquifer system. It is located underground in the Eastern end of the Sahara Desert and spans the political boundaries of four countries in north-eastern Africa.[1] NSAS covers a land area spanning just over two million km2, including north-western Sudan, north-eastern Chad, south-eastern Libya, and most of Egypt. Containing an estimated 150,000 km3 of groundwater,[2] the significance of the NSAS as a potential water resource for future development programs in these countries is extraordinary. Recently the Great Man-made River Project (GMMR) in Libya began extracting substantial amounts of water from this aquifer, removing an estimated 2.37 km3 per year. This system is primarily used to supply water in the Kufra oasis.

Characteristics[edit]

Since 2001, the Nubian Sandstone aquifer situated between the Toshka and Abu Simbel areas of Egypt underwent intensive drilling and development as part of a land reclamation project. Drilling information was used to conduct a variety of studies regarding the hydrogeological setting of the area's aquifer. Results indicated that lithological characteristics and tectonic settings are having a substantial effect on groundwater flow patterns and the area's overall aquifer potentiality, which is considered relatively low when compared to neighboring areas in eastern Oweinat or Dakhla.

Geology[edit]

The aquifer is largely composed of hard ferruginous sandstone with great shale and clay intercalation, having a thickness that ranges between 140-230 meters. Groundwater type varies from fresh to slightly brackish (salinity ranges from 240-1300 ppm). The ion dominance ordering shows that sodium cation is most commonly predominating over calcium and magnesium - whereas chloride is predominant over sulfate and bicarbonate. The groundwater is of meteoric origin[3] (the term meteoric water refers to water that originated as precipitation; most groundwater is meteoric in origin). High concentrations of sodium, chloride, and sulfates reflect the leaching and dissolution processes of gypsiferous shales and clay, in addition to a lengthy duration of water residence.[4]

International development projects[edit]

Since 2006, the International Atomic Energy Agency has been working in cooperation with the four NSAS countries to help increase understanding of the aquifer's complexities through the IAEA-UNDP-GEF Nubian Project. Project partners include the United Nations Development Programme (UNDP)/Global Environment Facility (GEF), IAEA, United Nations Educational, Scientific and Cultural Organization (UNESCO) and government representatives from the NSAS countries. The project's long-term goal is establishing rational and equitable management of the NSAS as a productive way of advancing socio-economic development in the region and protecting biodiversity and land resources.[5]

References[edit]

  1. ^ International Atomic Energy Agency: NSAS Project
  2. ^ Center for Environmental and Development for the Arab Region and Europe (CEDARE) 2000
  3. ^ [1] Abd El Samie, S., and Sadek, M., 2001, Groundwater recharge and flow in the Lower Cretaceous Nubian Sandstone aquifer in the Sinai Peninsula, using isotopic techniques and hydrochemistry: Hydrogeology Journal, vol. 9, n. 4, p. 378-389
  4. ^ A Study of Hydrogeological Conditions of the Nubian Sandstone Aguifer in the Area between Abu Simbel & Toschka, Western Desert, Egypt. American Geophysical Union, Spring 2001
  5. ^ IAEA/UNDP/GEF Nubian Sandstone Aquifer System Medium Sized Project: Inception Meeting Report. November 9, 2006

Bibliography[edit]