Simulated results of the coupled freshwater-saltwater sharp interface and convective-dispersive numerical models are compared by using steady-state cross-sectional simulations. The results indicate that in some aquifers the calculated sharp interface is located further landward than would be expected.
|Publication Subtype||Journal Article|
|Title||A comparison of coupled freshwater-saltwater sharp-interface and convective-dispersive models of saltwater intrusion in a layered aquifer system|
|Series title||Developments in Water Science|
|Contributing office(s)||Office of Ground Water|
|Google Analytics Metrics||Metrics page|