Executive Summary
The central section of the Umm er Radhuma- Dammam Aquifer System extends over a 400 km-wide structural platform that stretches across three Gulf States: Bahrain, Qatar and Saudi Arabia. In the western low-plateau areas, the aquifer system is dominated by the Umm er Radhuma, while in the eastern plains it becomes more complex as the Umm er Radhuma and the Dammam are separated by the Rus Formation and overlain by Neogene-Quaternary units. Limited recharge occurs mainly through the Umm er Radhuma outcrops. The general direction of groundwater flow in the aquifer system is from west to east in Saudi Arabia.
The aquifer system is heavily exploited for agricultural development projects in Saudi Arabia, with most water abstracted from the Dammam. The Dammam is also the main source of irrigation water in Bahrain, while the Umm er Radhuma supplies most of the water for domestic and industrial purposes. In Qatar, water is drawn from the Umm er Radhuma and Rus in the north. The Umm er Radhuma- Dammam Aquifer System in the Gulf region is increasingly threatened by salinization as a result of seawater intrusion and over-pumping.
Basin Facts
Riparian Countries | Bahrain, Qatar, Saudi Arabia |
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Alternative Names | Alat, Khobar, Dammam, Rus, Umm er Radhuma |
Renewability | Very low to low (0-20 mm/yr) |
Hydraulic Linkage with Surface Water | Weak |
Rock Type | Fissured/karstic |
Aquifer Type | Unconfined to confined |
Extent | ~281,000 km2 |
Age | Cenozoic (Paleogene) |
Lithology | Mainly limestone and dolomite, with some evaporites |
Thickness | Dammam: 35-180 m Umm er Radhuma: 240-500 m |
Average Annual Abstraction | Bahrain: Dammam: 97 MCM (2010) Umm er Radhuma: 54.3 MCM (2006)
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Storage | Bahrain: 90 MCM (safe yield) Qatar: 2.5 BCM Saudi Arabia: 235 BCM |
Water Quality | Fresh (mostly <1 g/L TDS) to hypersaline in some coastal areas |
Water Use | Mainly agricultural, also domestic, industrial and urban irrigational use |
Agreements | -- |
Sustainability | Over-exploitation and salinization |