Groundwater recharge dams in arid areas as tools for aquifer replenishment and mitigating seawater intrusion: example of AlKhod, Oman

• Published in: Environmental earth sciences Vol. 69; no. 6; pp. 1951 - 1962
• Main Authors: Abdalla, Osman A. E., Al-Rawahi, Abdullah S.
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer-Verlag 01-07-2013; Springer; Springer Nature B.V
• Subjects: Aquifers; Arid regions; Arid zones; Artificial recharge; Biogeosciences; Coastal aquifers; Coastal environments; Desalination; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Environmental Science and Engineering; Exact sciences and technology; Geochemistry; Geology; Groundwater; Groundwater depletion; Groundwater flow; Groundwater management; Groundwater recharge; Hydrogeology; Hydrology. Hydrogeology; Hydrology/Water Resources; Induced infiltration; Intrusion; Original Article; Piezometers; Pollution, environment geology; Reduction; Resource management; Saline water intrusion; Saline-freshwater interfaces; Sea water; Seawater; Terrestrial Pollution; Unconfined aquifers; Water resources; Water table; Water table rise; Water tables; Arabian Peninsula; Asia; Oman; ISW, Oman; Seawater intrusion; Arid areas; Oman; Recharge dam; salinity; rainfall; salt-water intrusion; ground water; water table; arid environment; ground-water recharge; dams; artificial recharge; pumping; percolation; water resources; aquifers; fluctuations; water resource management; electrical conductivity; unconfined aquifers; flow; wadis
• ISSN: 1866-6280; 1866-6299
• DOI: 10.1007/s12665-012-2028-x

Groundwater depletion and seawater intrusion constitute major challenges along coastal aquifers in arid areas. This paper assesses the role of groundwater recharge dams constructed to replenish aquifers and fight seawater intrusion with reference to AlKhod dam, Oman, sited 7 km from the coast on a gravely unconfined aquifer. Water table rise in piezometers located downstream from the dam shows regular patterns correlating with magnitude of wadi flow, whereas upstream piezometers show irregular patterns. Controlled release of water captured by the dam optimizes water percolation and enhances artificial recharge which was estimated in the wet years 1997, 2003 and 2005 as 15, 22 and 27 Mm
3
, respectively, using water table fluctuation method. Recharge contributed 40–60 % of the total annual abstraction. Groundwater salinity increased in the 1980s and 1990s and the saline/freshwater interface advanced inland, but has receded partially after 1997 (highest rainfall) and completely after 2005 indicated by reduction in electrical conductivity and thickening of freshwater lens. The recession is attributed to the dam’s induced recharge and reduction of pumping in 2004 following the commissioning of Barka desalination plant. Integrating artificial recharge with groundwater resources management is therefore an effective measure to replenish aquifers in arid areas and mitigate seawater intrusion along the coasts.