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This study aims to characterize the transboundary aquifer of the Somes-Szamos River, located in Romania and Hungary. It examines the lithological cross-sections, observation and production wells, hydraulic head differences, and groundwater tables in the area. The SQUASH database is used for data analysis and querying.
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Common Characterization of the TransboundaryAquifer of Somes-Szamos River (Romania – Hungary) Alain DASSARGUES – University of Liege (Belgium) Radu DROBOT - Technical University of Civil Engineering Bucharest (Romania) Laszlo LENART – Univesity of Miskolc (Hungary) Serge BROUYERE – University of Liege (Belgium); Mihai BRETOTEAN – National Institute of Hydrology and Water Management (Romania); Marin MINCIUNA - National Institute of Hydrology and Water Management (Romania); Margit VIRAG–JUHASZNE,Lajos MIKO, Peter SZUCS – Univesity of Miskolc (Hungary); Atilla SZABO – Univesity of Miskolc (Hungary); Tamasz MADARASZ – Univesity of Miskolc (Hungary); Anca FILIP – National Institute of Hydrology and Water Management (Romania); Ileana Cristina POPESCU – University of Liege (Belgium); Felician NISTEA – Public Utility Satu-Mare (Romania); Anton SZENDREI – Public Utility Satu-Mare (Romania); Simona CURTEAN – Public Utility Satu-Mare (Romania)
Figure 1:Location of the Somes/Szamos basin in Romania and Hungary.
Figure 3: Romanian concept: Former lithological cross-section I-I’
Figure 4: Hungarian concept: Former lithological cross-section VIII-VIII’
Figure 5: Hungarian concept: Geological cross-section VIII-VIII’
Figure 6:Common concept: new lithological cross-section II-II’
Figure 7:Common concept: new lithological cross-section I-I’
Figure 8:Common concept: new lithological cross-section VI-VI’
Figure 9:Common concept: new lithological cross-section VI-VI’
Figure 10:Common concept: new lithological cross-section VI-VI’
Figure 11:Common concept: new lithological cross-section VI-VI’
Figure 12:Common concept: new lithological cross-section VI-VI’
Figure 8:Isolines of hydraulic head differences between the shallow and the deep aquifer
Figure 20: Example of queries for finding the piezometric level in April 2002