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Movement of interface between fresh water and seawater in coastal aquifers caused by changes in seaward flow of fresh water is studied; approximate solutions to moving interface, its shape, position, and velocity of displacement are suggested; assuming that aquifer is relatively thin, Dupuit assumption is applied to flows in both fresh water region above and salt water region below interface; average specific discharges obtained are combined with continuity equation to yield partial differential equations for time-variable thickness of fresh water flow region.
Movement of interface between fresh water and seawater in coastal aquifers caused by changes in seaward flow of fresh water is studied; approximate solutions to moving interface, its shape, position, and velocity of displacement are suggested; assuming that aquifer is relatively thin, Dupuit assumption is applied to flows in both fresh water region above and salt water region below interface; average specific discharges obtained are combined with continuity equation to yield partial differential equations for time-variable thickness of fresh water flow region.
Moving interface in coastal aquifers
ASCE -- Proceedings (J Hyrualics Division)
1964
24 pages
Article (Journal)
English
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