The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater management

Study Region: Pannonian Basin, Central and Eastern Europe. Study focus: This study, carried out by the geological surveys of Hungary, Slovenia, Austria and Slovakia, combines a joint characterization of a transboundary thermal groundwater system based on harmonised geological and hydrogeological dat...

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Main Authors: Teodora Szocs, Nina Rman, Ágnes Rotár-Szalkai, György Tóth, Andrej Lapanje, Radovan Černák, Annamária Nádor
Format: Article
Language:English
Published: Elsevier 2018-12-01
Series:Journal of Hydrology: Regional Studies
Online Access:http://www.sciencedirect.com/science/article/pii/S2214581817303658
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spelling doaj-4bef4396588c47acbd1f0ba05b2ff7032020-11-24T21:40:25ZengElsevierJournal of Hydrology: Regional Studies2214-58182018-12-0120128144The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater managementTeodora Szocs0Nina Rman1Ágnes Rotár-Szalkai2György Tóth3Andrej Lapanje4Radovan Černák5Annamária Nádor6Mining and Geological Survey of Hungary, Columbus utca 17–23, H-1145 Budapest, Hungary; Corresponding author.Geological Survey of Slovenia, Dimičeva ulica 14, SI-1000 Ljubljana, SloveniaMining and Geological Survey of Hungary, Columbus utca 17–23, H-1145 Budapest, HungaryMining and Geological Survey of Hungary, Columbus utca 17–23, H-1145 Budapest, HungaryGeological Survey of Slovenia, Dimičeva ulica 14, SI-1000 Ljubljana, SloveniaState Geological Institute of Dionýz Štúr, Mlynská dolina 1, SK-817 04 Bratislava 11, SlovakiaMining and Geological Survey of Hungary, Columbus utca 17–23, H-1145 Budapest, HungaryStudy Region: Pannonian Basin, Central and Eastern Europe. Study focus: This study, carried out by the geological surveys of Hungary, Slovenia, Austria and Slovakia, combines a joint characterization of a transboundary thermal groundwater system based on harmonised geological and hydrogeological data, with hydrodynamic modelling, delivering recommendations for authorities and policy makers on how they could improve the long term management of thermal groundwater. A porous, intergranular, multi-layered, Upper Pannonian aquifer system was the focus of this investigation. This deep sedimentary basin, up to 8000 m deep, has favourable conditions for geothermal exploitation, with centuries old thermal water usage and plans for increased utilization in all countries. New hydrological insights for the region: Cross border areas with significant transboundary flow rates were identified, which have decreased due to thermal water production, with flow direction reversal across the Hungarian-Slovakian border. Thermal water production causes significant transboundary effects with depression cones that can penetrate several tens of kilometres into the neighbouring countries. Simulated drawdowns at the state borders are in the range of 2–10 m. Thermal water should therefore be exploited using doublets.Nine benchmark indicators (monitoring status, best available technology, thermal efficiency, utilisation efficiency, re-injection rate, quality of discharged thermal water, over-abstraction, status of water balance assessment, public awareness) were defined and tested at different transboundary regions and are demonstrated to be highly effective in groundwater management. Keywords: Aquifer, Groundwater, Transboundary, Governance, Geothermal energy, Pannonian basinhttp://www.sciencedirect.com/science/article/pii/S2214581817303658
collection DOAJ
language English
format Article
sources DOAJ
author Teodora Szocs
Nina Rman
Ágnes Rotár-Szalkai
György Tóth
Andrej Lapanje
Radovan Černák
Annamária Nádor
spellingShingle Teodora Szocs
Nina Rman
Ágnes Rotár-Szalkai
György Tóth
Andrej Lapanje
Radovan Černák
Annamária Nádor
The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater management
Journal of Hydrology: Regional Studies
author_facet Teodora Szocs
Nina Rman
Ágnes Rotár-Szalkai
György Tóth
Andrej Lapanje
Radovan Černák
Annamária Nádor
author_sort Teodora Szocs
title The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater management
title_short The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater management
title_full The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater management
title_fullStr The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater management
title_full_unstemmed The upper pannonian thermal aquifer: Cross border cooperation as an essential step to transboundary groundwater management
title_sort upper pannonian thermal aquifer: cross border cooperation as an essential step to transboundary groundwater management
publisher Elsevier
series Journal of Hydrology: Regional Studies
issn 2214-5818
publishDate 2018-12-01
description Study Region: Pannonian Basin, Central and Eastern Europe. Study focus: This study, carried out by the geological surveys of Hungary, Slovenia, Austria and Slovakia, combines a joint characterization of a transboundary thermal groundwater system based on harmonised geological and hydrogeological data, with hydrodynamic modelling, delivering recommendations for authorities and policy makers on how they could improve the long term management of thermal groundwater. A porous, intergranular, multi-layered, Upper Pannonian aquifer system was the focus of this investigation. This deep sedimentary basin, up to 8000 m deep, has favourable conditions for geothermal exploitation, with centuries old thermal water usage and plans for increased utilization in all countries. New hydrological insights for the region: Cross border areas with significant transboundary flow rates were identified, which have decreased due to thermal water production, with flow direction reversal across the Hungarian-Slovakian border. Thermal water production causes significant transboundary effects with depression cones that can penetrate several tens of kilometres into the neighbouring countries. Simulated drawdowns at the state borders are in the range of 2–10 m. Thermal water should therefore be exploited using doublets.Nine benchmark indicators (monitoring status, best available technology, thermal efficiency, utilisation efficiency, re-injection rate, quality of discharged thermal water, over-abstraction, status of water balance assessment, public awareness) were defined and tested at different transboundary regions and are demonstrated to be highly effective in groundwater management. Keywords: Aquifer, Groundwater, Transboundary, Governance, Geothermal energy, Pannonian basin
url http://www.sciencedirect.com/science/article/pii/S2214581817303658
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