2019
DOI: 10.1002/hyp.13649
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Estimating groundwater recharge for a freshwater lens in an arid region: Formative and stability assessment

Abstract: The formation of subsurface freshwater lenses on top of brackish groundwater is a fascinating hydrologic phenomenon that creates groundwater supplies of great potential value in arid regions. Information on the recharge quantity and mechanism of these lenses is both scarce and uncertain. This study examines the formation and

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Cited by 7 publications
(4 citation statements)
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“…We simulated an island with an enhanced‐recharge area at the domain center, which can be caused by a lake or an artificial recharge trench (Bouchez et al., 2016; Bouwer, 2002, Tu et al., 2011). Table 1 lists the typical hydrogeologic and geometric parameters (Alrashidi & Bailey, 2019; Chui & Terry, 2015; Ketabchi et al., 2014). This domain is 600 × 150 m, and the size of each cell is 1 × 1 m. Two top corners are set as fixed head ( h = 0).…”
Section: Numerical Validationmentioning
confidence: 99%
“…We simulated an island with an enhanced‐recharge area at the domain center, which can be caused by a lake or an artificial recharge trench (Bouchez et al., 2016; Bouwer, 2002, Tu et al., 2011). Table 1 lists the typical hydrogeologic and geometric parameters (Alrashidi & Bailey, 2019; Chui & Terry, 2015; Ketabchi et al., 2014). This domain is 600 × 150 m, and the size of each cell is 1 × 1 m. Two top corners are set as fixed head ( h = 0).…”
Section: Numerical Validationmentioning
confidence: 99%
“…The longer time scales (12 and 24 months) used in this study are more suitable for characterizing drought impacts on groundwater resources. Groundwater aquifers respond slowly to rainfall shortages [48]; therefore, shorter drought analysis scales (e.g., 1-6 months) would certainly fail to present the true drought status given Kuwait's long annual zero-rainfall period, making their usage for drought analysis meaningless.…”
Section: Drought Forecasting In Hyper-arid Climatesmentioning
confidence: 99%
“…In addition, anthropogenic stresses to the groundwater reserves through abstraction in the study area are minimal. Previous studies estimated that the annual recharge volumes to Al-Rawdatain basin are in the order of millions of cubic meters while current withdrawals rates do not exceed 100,000 m 3 /year [22,[37][38][39][40]. On the other hand, at Umm-Al-Aish basin, there are no current withdrawals due to the lower quality of groundwater.…”
Section: Case Study Of Groundwater Aquifers In the State Of Kuwaitmentioning
confidence: 99%