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Hydrogeology And Hydrochemistry Of A Shallow Alluvial
Aquifer, Western
Saudi Arabia
Al-Shaibani, AM
SPRINGER, HYDROGEOLOGY JOURNAL; pp: 155-165; Vol: 16
King Fahd University of Petroleum & Minerals
http://www.kfupm.edu.sa
Summary
A hydrogeological and hydrochemical study was conducted on a shallow alluvial
aquifer, Wadi Wajj, in western Saudi Arabia to assess the influence of protection
measures on groundwater quality. The hydrochemistry was assessed up-gradient and
down-gradient from potential contamination sources in the main city in dry and wet
seasons prior to and after the installation of major drainage and wastewater facilities.
Wadi Wajj is an unconfined aquifer where water is stored and transmitted through
fractured and weathered bedrock and the overlying alluvial sediments. Natural
recharge to the aquifer is about 5% of rainfall-runoff. Hydrochemistry of the aquifer
shows temporal and seasonal changes as influenced by protection measures and
rainfall runoff. Both groundwater and runoff showed similar chemical signature,
which is mostly of chloride-sulfate-bicarbonate and sodium-calcium type.
Groundwater downstream of the city, though of poorer quality than upstream, showed
significant improvement after the installation of a concrete runoff tunnel and a
wastewater treatment plant. Concentrations of many of the groundwater quality
indicators (e.g., TDS, coliform bacteria, and nitrate) exceed US Environmental
Protection Agency drinking-water standards. Heavy metal content is, however, within
allowable limits by local and international standards. The chemical analyses also
suggest the strong influence of stream runoff and sewage water on the groundwater
quality.
References:
Copyright: King Fahd University of Petroleum & Minerals;http://www.kfupm.edu.sa
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©
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For pre-prints please write to: [email protected]
Copyright: King Fahd University of Petroleum & Minerals;http://www.kfupm.edu.sa