1989
DOI: 10.1080/07900628908722419
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Use of groundwater for irrigation in the Nile valley

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Cited by 6 publications
(4 citation statements)
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“…The depth of river penetration into the aquifer system determines the hydraulic connectivity between the river and the aquifer system. A good hydraulic connection between the river and the aquifer exists, due to the absence of low-permeable deposits below the riverbed (Attia, 1989). The hydraulic conductance for the Nile River bed layer ranges from 1 to 10 days as shown in Fig.…”
Section: Surface Water and Groundwater Interactionmentioning
confidence: 98%
“…The depth of river penetration into the aquifer system determines the hydraulic connectivity between the river and the aquifer system. A good hydraulic connection between the river and the aquifer exists, due to the absence of low-permeable deposits below the riverbed (Attia, 1989). The hydraulic conductance for the Nile River bed layer ranges from 1 to 10 days as shown in Fig.…”
Section: Surface Water and Groundwater Interactionmentioning
confidence: 98%
“…It includes potential soils where classifications indicated the suitability of the Wadi for agricultural development if irrigation water is available (Elewa, 2008). Previous studies on Wadi El Assiuti (Dawoud, et al, 2006;Yan, et al, 2004;MWRI, 2001;RIGW, 2000 andAshmawy andNassim, 1998) indicated the existence of two possible sources of replenishment to the shallow aquifer in the area: 1-Surface water infiltration along the runoff streams through transmission losses which is mainly developed in the Quaternary alluvium aquifer (Dawoud, 1997;Warner et al, 1991 andAttia, 1989), and 2-Deep groundwater upward discharge from the Nubian aquifer through deep major faults feeding the Quaternary alluvium aquifer (Yan, et al, 2004). Data collected from old production wells drilled by Assiut Governorate and recent observation wells drilled by the Research Institute for Groundwater (RIGW) were evaluated and assessed to calculate the groundwater potentiality.…”
Section: Introductionmentioning
confidence: 94%
“…Recharge from surplus irrigation application has been estimated by many authors and researchers using numerical modeling and water budget analysis as shown in Fig. 8 (Attia, 1989;Dawoud, 1997;RIGW, 2000). The recharge to the aquifer system ranges from 0.5 to 0.8 mm/day in the old agriculture land and ranges from 1.0 to 1.5 mm/day in the desert fringes for new reclaimed lands.…”
Section: Aquifer Rechargementioning
confidence: 99%
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