2006
DOI: 10.1016/j.jhydrol.2005.10.011
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Pathline-calibrated groundwater flow models of Nile Valley aquifers, Esna, upper Egypt

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Cited by 14 publications
(6 citation statements)
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“…The aquifer is highly productive and of good water quality. It is recharged mainly from irrigation water and seepage from irrigation canals through the Holocene aquitard (Abu-Zeid, 1995;Shamrukh et al, 2001;Shamrukh and Abdel-Wahab, 2008;Brikowski and Faid, 2006;Ahmed, 2003;Kamel, 2004). Discharge of this aquifer is through groundwater pumping for irrigation and drinking purposes and natural discharge towards the River Nile (RIGW/ IWACO, 1997;Shahin, 1991;Awad et al, 1997;Ahmed, 2003Ahmed, , 2009).…”
Section: The Quaternary Aquifermentioning
confidence: 99%
“…The aquifer is highly productive and of good water quality. It is recharged mainly from irrigation water and seepage from irrigation canals through the Holocene aquitard (Abu-Zeid, 1995;Shamrukh et al, 2001;Shamrukh and Abdel-Wahab, 2008;Brikowski and Faid, 2006;Ahmed, 2003;Kamel, 2004). Discharge of this aquifer is through groundwater pumping for irrigation and drinking purposes and natural discharge towards the River Nile (RIGW/ IWACO, 1997;Shahin, 1991;Awad et al, 1997;Ahmed, 2003Ahmed, , 2009).…”
Section: The Quaternary Aquifermentioning
confidence: 99%
“…The aquifer is highly productive of good water quality. It is recharged mainly from irrigation water and seepage from irrigation canals through the Holocene aquitard (Abu-Zeid 1995; Shamrukh et al 2001;Shamrukh and Abdel-Wahab 2008;Brikowski and Faid 2006;Ahmed 2003;Kamel 2004). Discharge of this aquifer is through groundwater pumping for irrigation and drinking purposes and natural discharge towards the River Nile (RIGW/IWACO 1997; Shahin 1991; Awad et al 1997;Ahmed 2003).…”
Section: Hydrogeologymentioning
confidence: 99%
“…The infiltration tests, according to (Barber and Carr, 1981;Abdel Moneim, 1988) were applied to estimate the infiltration rate of the top layer, the results indicated that the average infiltration rate is 2.5 m/day, this indicating that there is a good hydraulic connection between the upper and lower layer. (RIGW, 1994) In the study area the Quaternary aquifer is mainly recharged by the irrigation water and seepage from irrigation canal through the Holocene aquitard, secondary source of groundwater recharge is the under flow from rainfall during winter months each few years (Brikowski and Faid, 2006;Ahmed, 2003). In addition, seepage from irrigation of the new reclaimed areas at the desert fringes in the study area ( Figure 5).…”
Section: The Quaternary Aquifermentioning
confidence: 99%