2020
DOI: 10.1016/j.jhydrol.2020.124641
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Evaluating dynamic mechanisms and formation process of freshwater lenses on reclaimed atoll islands in the South China Sea

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Cited by 14 publications
(17 citation statements)
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“…This assumption is reasonable for the rainfall intensity in a small area, but it is not realistic for the recharge of aquifers, because the process of infiltration is affected by geological characteristics such as topography, soil type and evapotranspiration, land use type, and human activities (Park et al., 2014; Werner et al., 2017). Field investigations have showed that the groundwater lens shape and thickness can be affected by spatially variable recharge rates induced by ridge topography (Ruppel et al., 2000), terrain and vegetation patterns (Schneider & Kruse, 2003, 2006), distribution of different soil types (Park et al., 2014) and heterogeneous hydrogeological properties including hydraulic conductivity, impermeable layer, and boundary conditions (Cellone et al., 2018; Holt et al., 2019; Rathore et al., 2018; Rathore, Lu & Luo, 2020; Sheng et al., 2020). In addition, the knowledge and insights on how the volume and shape of a groundwater lens change in response to spatially variable recharge rates can provide very useful information for determining the location and recharge rate of artificial recharge to control seawater intrusion (Bouwer, 2002; Rajasekhar et al., 2019; Senanayake et al., 2016).…”
Section: Introductionmentioning
confidence: 99%
“…This assumption is reasonable for the rainfall intensity in a small area, but it is not realistic for the recharge of aquifers, because the process of infiltration is affected by geological characteristics such as topography, soil type and evapotranspiration, land use type, and human activities (Park et al., 2014; Werner et al., 2017). Field investigations have showed that the groundwater lens shape and thickness can be affected by spatially variable recharge rates induced by ridge topography (Ruppel et al., 2000), terrain and vegetation patterns (Schneider & Kruse, 2003, 2006), distribution of different soil types (Park et al., 2014) and heterogeneous hydrogeological properties including hydraulic conductivity, impermeable layer, and boundary conditions (Cellone et al., 2018; Holt et al., 2019; Rathore et al., 2018; Rathore, Lu & Luo, 2020; Sheng et al., 2020). In addition, the knowledge and insights on how the volume and shape of a groundwater lens change in response to spatially variable recharge rates can provide very useful information for determining the location and recharge rate of artificial recharge to control seawater intrusion (Bouwer, 2002; Rajasekhar et al., 2019; Senanayake et al., 2016).…”
Section: Introductionmentioning
confidence: 99%
“…Previous studies indicated that the hydraulic properties of coral sand or fill materials exhibit highly spatial heterogeneity (Sheng et al., 2020; Werner et al., 2017). For example, Bailey et al.…”
Section: Discussionmentioning
confidence: 99%
“…It was reclaimed from August 2014 to September 2015, with the land area increased from less than 0.2 km 2 to 2.23 km 2 . The length is 3.71 km, and the maximum width is 0.99 km [26]. The topography is flat, with an elevation normally 3 to 4 m above the mean sea level.…”
Section: Study Areamentioning
confidence: 99%
“…PRP, the only source of fresh water on the coral islands, is mainly consumed by ET a , infiltration, and rainwater collection or water flowing into the sea. Storage changes within the unsaturated zone and surface runoff can be neglected [1,5] on coral islands due to the low water-binding capacity of gravelly and sandy soil texture, both for natural and for reclaimed islands [26,50]. In this study, the water budget analysis could be written as ∆V = PRP − Eta, where PRP is rainfall (mm); ET a is the actual evapotranspiration (mm), which contains E c , E s , and E i ; and ∆V is the total amount of infiltration, rainwater collection, and water flowing into the sea.…”
Section: Evapotranspiration Distribution On the Three Islandsmentioning
confidence: 99%
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