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Projekt Druckansicht

Hydrogeological and hydrochemical modelling of density-driven flow in the Tiberias Basin, in particular between Ha'on and Tiberias Regions, Jordan Valley

Fachliche Zuordnung Hydrogeologie, Hydrologie, Limnologie, Siedlungswasserwirtschaft, Wasserchemie, Integrierte Wasserressourcen-Bewirtschaftung
Förderung Förderung von 2013 bis 2020
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 232199240
 
Erstellungsjahr 2019

Zusammenfassung der Projektergebnisse

The aim of this research was the identification of regional and transboundary sources endangering Lake Kinneret (Lake Tiberias or Sea of Galilee) which is the most important fresh water reservoir of the area. The tasks are achieved by a multidisciplinary approach involving: (i) numerical modelling of densitydriven flow processes (i.e., coupled heat and lfow), (ii) hydrochemical studies, both supplemented by (iii) investigations of subsurface structures. (i) Numerical modelling is done by applying commercial software. The 3D regional-scale model of density-driven flow revealed the different interactions between fresh groundwater thermal flow and convective processes controlled by faults, (ii) Hydrochemical studies include major, minor and rare earth elements (REE) as well as isotope studies. Geochemical data interpretation and inverse modelling are supported by PHREEQC. Hydrochemical field investigations are carried out in the Kinnarot basin and ist framing Heights, i.e. the Golan, Eastern Galilee and northern Ajlun Mts to search for indications of the presence of deep, relic saline groundwater infested by the inferred Ha’on mother-brine. These approaches are supplemented by (iii) statistical data analysis and GIS software for the definition of the subsurface structures and fault patterns. The applied approaches support the hypothesis that a structural feature exists along the principle axis of the Lower Yarmouk Gorge, which may act as a complex conduit-barrier system that enhances axial fluid flow, inhibits perpendicular lateral fluxes, and drains them westwards, thus compartmentalizing the adjacent N–S and S–N flow systems of the Golan Heights and the Ajlun Plateau, respectively. This study highlighted the impact that structural features exert on transport processes and provide an example of multi-disciplinary investigation of complex aquifer systems, particularly in cases of existent heterogeneities, structural uncertainty and limited field accessibility. The results of this work are expected to establish suitable water-management strategies for the exploitation of freshwater from the lake and from the adjacent aquifers while reducing salinization processes induced by both local and regional brines.

Projektbezogene Publikationen (Auswahl)

 
 

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