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Brackish Karstic Springs Model: Application to Almiros Spring in Crete

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dc.contributor.author Maramathas, A en
dc.contributor.author Maroulis, Z en
dc.contributor.author Marinos-Kouris, D en
dc.date.accessioned 2014-03-01T01:18:45Z
dc.date.available 2014-03-01T01:18:45Z
dc.date.issued 2003 en
dc.identifier.issn 0017-467X en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/15171
dc.subject.classification Geosciences, Multidisciplinary en
dc.subject.classification Water Resources en
dc.subject.other Computer simulation en
dc.subject.other Discharge (fluid mechanics) en
dc.subject.other Hydrodynamics en
dc.subject.other Mathematical models en
dc.subject.other Rain en
dc.subject.other Reservoirs (water) en
dc.subject.other Brackish karstic springs en
dc.subject.other Springs (water) en
dc.subject.other brackish water en
dc.subject.other hydrochemistry en
dc.subject.other karst hydrology en
dc.subject.other numerical model en
dc.subject.other rainfall en
dc.subject.other spring water en
dc.subject.other Crete en
dc.subject.other Eurasia en
dc.subject.other Europe en
dc.subject.other Greece en
dc.subject.other Heraklion en
dc.subject.other Southern Europe en
dc.subject.other fresh water en
dc.subject.other rain en
dc.subject.other sea water en
dc.subject.other article en
dc.subject.other Greece en
dc.subject.other theoretical model en
dc.subject.other water flow en
dc.subject.other water supply en
dc.subject.other Fresh Water en
dc.subject.other Greece en
dc.subject.other Models, Theoretical en
dc.subject.other Rain en
dc.subject.other Seawater en
dc.subject.other Water Movements en
dc.subject.other Water Supply en
dc.title Brackish Karstic Springs Model: Application to Almiros Spring in Crete en
heal.type journalArticle en
heal.identifier.primary 10.1111/j.1745-6584.2003.tb02399.x en
heal.identifier.secondary http://dx.doi.org/10.1111/j.1745-6584.2003.tb02399.x en
heal.language English en
heal.publicationDate 2003 en
heal.abstract A mathematical model is proposed to simulate brackish karstic springs. Rainfall data constitutes model input information while output information is the discharge and the chloride concentration of the water versus time. The model was constructed by considering the mass and mechanical energy balance on the hydrodynamic analog, which includes three reservoirs outflowing in a tube that lies adjacent to the spring. Two reservoirs emulate the karstic system, and the third one emulates the sea. The discharge of the spring is given by the sum of the discharge of the reservoirs, and the chloride concentration by the solution of the mixing problem between the fresh and the salty water, which exists in the tube leading to the spring. The model is applied to the spring of Almiros at Heraklion, Crete, Greece. The agreement between model values and field measurements is very good for depletion periods and satisfactory for recharge periods. en
heal.publisher NATIONAL GROUND WATER ASSOC en
heal.journalName Ground Water en
dc.identifier.doi 10.1111/j.1745-6584.2003.tb02399.x en
dc.identifier.isi ISI:000185133900009 en
dc.identifier.volume 41 en
dc.identifier.issue 5 en
dc.identifier.spage 608 en
dc.identifier.epage 619 en


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