Advances in Water Resources and Hydraulic Engineering 2009
DOI: 10.1007/978-3-540-89465-0_29
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Numerical Simulation of Upconing and Freshwater Lens Breakage in a Coral Island

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“…The average annual rainfall is about 1,509 mm and the contact between the Holocene and underlying Pleistocene sediments occurs at 22 m below ground surface (shown as Figure 1b above). Other details on meteorology and hydrogeology of this field site are discussed in previous studies (Sheng et al., 2017; Zhou et al., 2009). The area of the original Yongxing Island was 2.13 km 2 and increased to 3.2 km 2 after land reclamation on the north of the island (Figures 11a and 11c).…”
Section: Discussionmentioning
confidence: 95%
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“…The average annual rainfall is about 1,509 mm and the contact between the Holocene and underlying Pleistocene sediments occurs at 22 m below ground surface (shown as Figure 1b above). Other details on meteorology and hydrogeology of this field site are discussed in previous studies (Sheng et al., 2017; Zhou et al., 2009). The area of the original Yongxing Island was 2.13 km 2 and increased to 3.2 km 2 after land reclamation on the north of the island (Figures 11a and 11c).…”
Section: Discussionmentioning
confidence: 95%
“…To further support the observations and findings from the laboratory and theoretical discussion above, numerical simulation was conducted in Yongxing Island, which is a typical coral island with land reclamation in the Xisha Islands, South China Sea (Figure 1). The measured thickness of the fresh groundwater lens is about 14–15 m before reclamation (Zhou et al., 2010). The average annual rainfall is about 1,509 mm and the contact between the Holocene and underlying Pleistocene sediments occurs at 22 m below ground surface (shown as Figure 1b above).…”
Section: Discussionmentioning
confidence: 99%
“…The results of the study showed that, when treating the transition zone between salt and fresh water as a sharp interface, the thickness of the freshwater lens calculated under hydrostatic equilibrium conditions is larger than the actual thickness and the evaluation of the total subsurface freshwater resources of the island is overestimated. Zhou [13,14] studied the formation and dynamic process of the freshwater lens on a coral island by using the Visual MODFLOW numerical model and put forward the reasonable development and protection strategy of freshwater lenses. Since then, many scholars have studied the formation, evolution and internal hydrodynamics of freshwater lenses by means of physical experiments and numerical simulations [15,16].…”
Section: Introductionmentioning
confidence: 99%