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Estimation of seawater intrusion front in a coastal karstified system using a density-dependent flow approach

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dc.contributor.author Papadopoulou, MP en
dc.contributor.author Dokou, Z en
dc.contributor.author Karatzas, GP en
dc.contributor.author Zahariadi, CI en
dc.date.accessioned 2014-03-01T02:52:40Z
dc.date.available 2014-03-01T02:52:40Z
dc.date.issued 2010 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/35982
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-84860233605&partnerID=40&md5=a5575d3f953c6985c66745f47993396c en
dc.subject.other Coastal aquifers en
dc.subject.other Contaminant transport en
dc.subject.other Density dependent flow en
dc.subject.other Density-dependent en
dc.subject.other Diffusion phenomena en
dc.subject.other Fault networks en
dc.subject.other Fluid densities en
dc.subject.other Hydraulic characteristic en
dc.subject.other Karstic en
dc.subject.other Model results en
dc.subject.other Numerical simulators en
dc.subject.other Subsurface Flow en
dc.subject.other Variable density en
dc.subject.other Aquifers en
dc.subject.other Computer simulation en
dc.subject.other Groundwater flow en
dc.subject.other Hydraulics en
dc.subject.other Salt water intrusion en
dc.subject.other Seawater en
dc.subject.other Groundwater geochemistry en
dc.title Estimation of seawater intrusion front in a coastal karstified system using a density-dependent flow approach en
heal.type conferenceItem en
heal.publicationDate 2010 en
heal.abstract The simulation of the contaminant transport to determine the penetration of seawater front is extremely complex due to the uncertainty related to the depth and orientation of the fault network and also due to the diffusion phenomenon associated with the variable density between fresh and salt water. Furthermore, the pumping activity which takes place in the aquifer is variable upon demand and affects significantly the hydraulic characteristics of the aquifer during the simulation period. In this paper, using the FEFLOW numerical simulator a subsurface flow and contaminant transport model that estimates the penetration of seawater intrusion front for a karstified coastal aquifer in Crete, Greece was developed. The model takes into consideration the geomorphologic characteristics of the karstic system and the density-dependent groundwater flow. The model results showed that the connectivity of the fractures and the fluid density effects are important factors that drive the seawater intrusion front asymmetrically inland. © 2010 Taylor & Francis Group, London. en
heal.journalName Environmental Hydraulics - Proceedings of the 6th International Symposium on Environmental Hydraulics en
dc.identifier.volume 2 en
dc.identifier.spage 631 en
dc.identifier.epage 636 en


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