Hydrostratigraphic decomposition of fluvio-deltaic sediments inferred from seismic geomorphology and geophysical well logs in the Pannonian Basin, Hungary

Ben Mahrez, Hana; Márton, Patrícia; Márton, Béla; Mádl Szőnyi, Judit; Kovács, József; Sztanó, Orsolya

doi:10.1016/j.gloplacha.2023.104285

Global and Planetary Change

2023

DOI: 10.1016/j.gloplacha.2023.104285

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Hydrostratigraphic decomposition of fluvio-deltaic sediments inferred from seismic geomorphology and geophysical well logs in the Pannonian Basin, Hungary

Hana Ben Mahrez,

Patrícia Márton,

Béla Márton

et al.

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Cited by 3 publications

References 73 publications

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Understanding the coupled evolution of orogens, sedimentary basins and their fluid-rock interactions

Nader,

Matenco,

Armitage

2023

Global and Planetary Change

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Understanding the coupled evolution of orogens, sedimentary basins and their fluid-rock interactions

Nader,

Matenco,

Armitage

2023

Global and Planetary Change

View full text Add to dashboard Cite

Influence of sedimentary architecture on static connectivity and geothermal doublet performance (Mezőberény, SE Hungary)

Budai,

Willems,

Colombera

et al. 2024

Marine and Petroleum Geology

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Re-interpreting renewable and non-renewable water resources in the over-pressured Pannonian Basin

Czauner,

Szijártó,

Sztanó

et al. 2024

Sci Rep

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With climate change, population growth and the resulting escalating water shortage, humanity is increasingly turning to non-renewable and even fossil groundwater resources, which poses a major challenge to sustainable water management. In this study, 2D basin-scale numerical simulations were carried out on the COMSOL Multiphysics ® finite element numerical platform to identify non-renewable water resources in the Central Pannonian Basin (Central Europe, Hungary) based on the lack of hydraulic connection to recharge areas. The concept and boundary conditions (fixed water table configuration at the top, pressure-elevation profiles on the lateral sides, and constant pressure on the bottom) were derived from a previous basin-scale hydraulic data evaluation study, while the hydrostratigraphic subdivision was based on seismic and well log interpretations. As a result, topography-driven groundwater flow systems fed by meteoric water infiltration were separated from a transition zone, which contains non-renewable groundwater resources and covers 85% area of the simulated 110 km long and roughly 1600 m deep cross-section what was previously thought to be fully renewable. Such complex flow pattern and re-interpretation of the renewable and non-renewable groundwater resources can be expected in any terrestrial sedimentary basin with over-pressured flow domains. Supplementary Information The online version contains supplementary material available at 10.1038/s41598-024-76076-8.

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Hydrostratigraphic decomposition of fluvio-deltaic sediments inferred from seismic geomorphology and geophysical well logs in the Pannonian Basin, Hungary

Cited by 3 publications

References 73 publications

Understanding the coupled evolution of orogens, sedimentary basins and their fluid-rock interactions

Understanding the coupled evolution of orogens, sedimentary basins and their fluid-rock interactions

Influence of sedimentary architecture on static connectivity and geothermal doublet performance (Mezőberény, SE Hungary)

Re-interpreting renewable and non-renewable water resources in the over-pressured Pannonian Basin

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