Arid
DOI10.7343/as-2019-378
Contribution to the hydrogeology of Six Hills sandstone aquifer in East El-Oweinat area, south Western desert, Egypt
Ghoubachi, Saad Younes
通讯作者Ghoubachi, SY
来源期刊ACQUE SOTTERRANEE-ITALIAN JOURNAL OF GROUNDWATER
ISSN1828-454X
出版年2019
卷号8期号:3页码:51-64
英文摘要El-Oweinat area is located in southwestern Egypt and is considered to be one of the new land reclamation projects in the Western Desert. The Nubian Sandstone aquifer has high potentiality and good groundwater quality. The results of geologic and hydrogeologic studies reveal that the Six Hills sandstone aquifer represents the sole groundwater resource used for all purposes (agriculture, drinking, domestic, livestock and poultry) in East El-Oweinat area. The Six Hills sandstone aquifer overlies directly the Precambrian basement rocks. The concerned aquifer exists under unconfined conditions as it is exposed on the surface. The hydrogeological cross sections show that the fully saturated thickness of the Six Hills sandstone aquifer ranges between 150.2 m and 651 m and increases towards the west. The groundwater generally flows towards the northeast direction with an average hydraulic gradient of 0.6 parts per thousand. The calculated groundwater volume of the Six Hills sandstone aquifer in East El-Oweinat area (4,340 km(2)) reaches 350 bcm of fresh water. The comparison of the depth to water in the same monitoring wells during 14 years (2003 and 2016) reveals that the head decline rate in groundwater depths were ranging between 5 cm/year and 80 cm/year. The pumping rate increased from 600,000 m(3)/day in year 2003 to 3,600,000 m(3)/day in 2016. The average transmissivity attains 2,060 m(2)/day reflecting the high potential of the Six Hills sandstone aquifer in East El-Oweinat area. The groundwater flow model (MODFLOW) has been used to investigate the impact of groundwater withdrawal on groundwater levels for sustainable groundwater management. Four scenarios were applied to predict the probable head changes in the Six Hills sandstone aquifer and their impact on the availability of groundwater. The fourth scenario is recommended in order to sustain the groundwater resources in the study area and keep the drawdown rates in the range of 0.66 m/year through reducing the present discharging rates (10,000 m(3)/day/well) by about 40 %.
英文关键词hydrogeology Six Hills sandstone aquifer El-Oweinat area
类型Article
语种英语
开放获取类型DOAJ Gold
收录类别ESCI
WOS记录号WOS:000504232500005
WOS类目Water Resources
WOS研究方向Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/334005
作者单位[Ghoubachi, Saad Younes] Desert Res Ctr, Div Water Resources, Dept Geol, Cairo, Egypt
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Ghoubachi, Saad Younes. Contribution to the hydrogeology of Six Hills sandstone aquifer in East El-Oweinat area, south Western desert, Egypt[J],2019,8(3):51-64.
APA Ghoubachi, Saad Younes.(2019).Contribution to the hydrogeology of Six Hills sandstone aquifer in East El-Oweinat area, south Western desert, Egypt.ACQUE SOTTERRANEE-ITALIAN JOURNAL OF GROUNDWATER,8(3),51-64.
MLA Ghoubachi, Saad Younes."Contribution to the hydrogeology of Six Hills sandstone aquifer in East El-Oweinat area, south Western desert, Egypt".ACQUE SOTTERRANEE-ITALIAN JOURNAL OF GROUNDWATER 8.3(2019):51-64.
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