1977
DOI: 10.1016/0022-1694(77)90074-9
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Studies on salinization of groundwater, I

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Cited by 10 publications
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“…In these regions, intense water demand often forces local communities to rely on groundwater to supplement surface freshwater. Coastal aquifers are normally characterized by a freshwater‐seawater contact zone, in which seaward discharging freshwater overlies the landward movement of seawater due to its lighter density (Kishi & Fukuo, 1977). When the abstraction rate exceeds the natural freshwater recharge, the seaward hydraulic gradient drops, causing the landward advancement of saltwater in aquifers, known as SWI.…”
Section: Introductionmentioning
confidence: 99%
“…In these regions, intense water demand often forces local communities to rely on groundwater to supplement surface freshwater. Coastal aquifers are normally characterized by a freshwater‐seawater contact zone, in which seaward discharging freshwater overlies the landward movement of seawater due to its lighter density (Kishi & Fukuo, 1977). When the abstraction rate exceeds the natural freshwater recharge, the seaward hydraulic gradient drops, causing the landward advancement of saltwater in aquifers, known as SWI.…”
Section: Introductionmentioning
confidence: 99%