Mark Szijarto

@elte.hu

Department of Geophysics and Space Science/Faculty of Science
Eötvös Loránd University

Mark Szijarto


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https://researchid.co/szijartomark
2022– research fellow, ELTE Faculty of Sciences, Department of Geophysics and Space Science
2021–2022 pre-doctoral researcher, ELTE Faculty of Sciences, Institute of Geography and Earth Sciences
2020–2021 gephysicist, ELGOSCAR-2000 Ltd.
2020 visiting researcher, Geological Survey of Finland (Espoo, Finland)
2018– lecturer, József and Erzsébet Tóth Hydrogelogy Endowed Chair
2017– co-owner, Hórukk Ltd.

EDUCATION

2017–2022: Ph.D. degree in earth science, Eötvös Loránd University
2015–2017: geophysicist (MSc), Eötvös Loránd University
2011–2015 physicist (BSc), Eötvös Loránd University

RESEARCH, TEACHING, or OTHER INTERESTS

Water Science and Technology, Earth and Planetary Sciences, Geophysics, Computers in Earth Sciences
13

Scopus Publications

244

Scholar Citations

8

Scholar h-index

8

Scholar i10-index

Scopus Publications

  • Numerical investigation of groundwater aging and thermal processes in confined-unconfined basins with asymmetric flow patterns: The Buda Thermal Karst, Hungary
    Márk Szijártó, Attila Galsa, Brigitta Czauner, Anita Erőss, Ádám Tóth, Judit Mádl-Szőnyi
    Hydrogeology Journal, 2025
    Groundwater temperature and age are crucial proxy data that play a fundamental role in understanding regional-scale groundwater flow systems and managing drinking and geothermal water resources. To investigate groundwater flow as well as heat and age mass transport processes in a complex hydrogeological system with deep carbonate sequences and adjoining sedimentary basins (DCSBs), numerical simulations were carried out in two-dimensional synthetic and two- and three-dimensional field-based conceptual environments. The simulations carried out for the Buda Thermal Karst (BTK), Hungary, revealed that the increasing asymmetry in the water table and the appearance of DCSB-type heterogeneity could affect the transition from advection-dominated to conduction- and diffusion-controlled transport processes in the models. However, simultaneously, both effects significantly influence the intensity of groundwater flow. Thermal buoyancy was superimposed on the water table-controlled forced convection (mixed convection), causing significant age mass accumulations in the closed convection cells. To quantify and track the changes in physical processes in the DCSB-type system, the simultaneous use of monitoring parameters calculated in the different parts of the model domain (e.g., unconfined vs confined), contours of groundwater age and temperature, and histograms of normalized groundwater age are presented. The numerical results from the preliminary three-dimensional model were compared to the 14C observation data in the BTK. The groundwater age calculated in the model was of the same order of magnitude as the results of 14C dating from samples taken at different depths in the unconfined and confined parts, and from the deeper mixing zone of the BTK.
  • Topothermohaline convection – from synthetic simulations to reveal processes in a thick geothermal system
    Attila Galsa, Márk Szijártó, Ádám Tóth, Judit Mádl-Szőnyi
    Hydrology and Earth System Sciences, 2025
    The water table topography, temperature, and solute content of groundwater all influence regional groundwater flow. Two-dimensional synthetic numerical calculations were performed to investigate the dynamic interaction between topography-driven forced convection and buoyancy-controlled free thermohaline convection. In the coupled topothermohaline model, the recharge and flow-through zones are dominated primarily by topography-driven regional groundwater flow, which drifts warm upwellings towards the discharge zone. Beneath the discharge zone, a dome with high temperature, salinity, and water age is formed in which time-dependent thermohaline convection develops. It was established that (1) increasing the water table gradient suppresses the thermohaline dome, resulting in a near-steady-state solution. (2) Increasing the bottom heat flux strengthens the warm upwellings, which ultimately leads to the break-up of the thermohaline dome, thus paradoxically reducing the average temperature. (3) Increasing the bottom salt concentration weakens the topography-driven groundwater flow, leading to the formation of a multi-layered thermohaline dome with extremely high temperature, salinity, and age. The operation of the topothermohaline model was demonstrated along a hydrogeological section crossing the Buda Thermal Karst (BTK) in Hungary. We found that the unconfined karstic areas are dominated by topography-driven water flow, while in the confined, deep reservoirs, thermohaline convection is the prevailing flow regime. The thermally and compositionally mixed water promotes karstification and reaches the surface near the Danube River, the main discharge area. In the eastern, confined areas of the BTK, significant amounts of heat may be retained on a geological timescale, making it a promising site for geothermal exploration.
  • Re-interpreting renewable and non-renewable water resources in the over-pressured Pannonian Basin
    Brigitta Czauner, Márk Szijártó, Orsolya Sztanó, Hana Ben Mahrez, John Molson, Soma Oláh, Judit Mádl-Szőnyi
    Scientific Reports, 2024
    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.
  • Correction to: Wetland Management in Recharge Regions of Regional Groundwater Flow Systems with Water Shortage, Nyírség Region, Hungary (Water, (2023), 15, 20, (3589), 10.3390/w15203589)
    Szilvia Simon, Judit Déri-Takács, Márk Szijártó, László Szél, Judit Mádl-Szőnyi
    Water Switzerland, 2024
    In the original publication [...]
  • Wetland Management in Recharge Regions of Regional Groundwater Flow Systems with Water Shortage, Nyírség Region, Hungary
    Szilvia Simon, Judit Déri-Takács, Márk Szijártó, László Szél, Judit Mádl-Szőnyi
    Water Switzerland, 2023
    Climate change and increasing human impacts are more emphasised in recharge regions, where the main flow direction is downward, resulting in negative water balance. Two wetlands located in the recharge position of regional groundwater flow systems were investigated in the Nyírség region, Hungary, as pilot areas for representing wetlands in similar hydraulic positions. Hydraulic data processes, chemical data evaluations, and numerical simulations revealed that the wetlands are fed via local flow systems, superimposing regional-scale recharge conditions in the area. The wetlands are discharge and flow-through types in connection with local flow systems. Nevertheless, in the case of significant regional water table decline—due to the high vulnerability of recharge areas to climate change—local flows are degraded, so they are not able to sustain the wetlands. To preserve the groundwater-dependent ecosystems in the areas, water retention at the local recharge areas of the wetlands may help in the mitigation of water level decline under present-day conditions. If the regional water table continues to decline, comprehensive water retention solutions are needed in the whole region. The results highlight that understanding the natural wetland–groundwater interactions at different scales is crucial for the preservation of wetlands and for successful water retention planning.
  • Infinite borehole field model—a new approach to estimate the shallow geothermal potential of urban areas applied to central Budapest, Hungary
    Kimmo Korhonen, Ábel Markó, Alan Bischoff, Márk Szijártó, Judit Mádl-Szőnyi
    Renewable Energy, 2023
    Deploying shallow geothermal solutions is critical for meeting energy demands while supporting decarbonisation targets. In densely populated areas, drilling large numbers of boreholes may lead to thermal interactions between closely located borehole heat exchangers. This paper presents a novel method termed the infinite borehole field model to estimate the technical shallow geothermal potential, especially in urban regions. The thermal interactions between boreholes are considered using finite element models simulating the operation of a single borehole in a larger field. Mathematical optimisation is used to find the amount of thermal energy that can be annually extracted while keeping the borehole wall temperature above freezing point of water. The method considers thermogeological details of geological formations including downward-increasing ground temperature, geothermal heat flux, thermal conductivity, heat capacity, porosity, density, and advective heat transfer. Results of our case study indicate that 100 m deep thermally independent boreholes can produce 14.20 MWh/a for 50 years on average. However, boreholes in an infinite borehole field spaced 20 m apart produce 7.80 MWh/a. A further investigation including advective heat transfer indicated that high velocity groundwater flow can significantly enhance borehole yield. Our method provides a generalised approach which can be beneficial prior to detailed site investigations.
  • The Significance of Groundwater Table Inclination for Nature-Based Replenishment of Groundwater-Dependent Ecosystems by Managed Aquifer Recharge
    Zsóka Szabó, Márk Szijártó, Ádám Tóth, Judit Mádl-Szőnyi
    Water Switzerland, 2023
    Managed aquifer recharge (MAR) is an increasingly popular technique; however, the significance of groundwater flow dynamics is rarely examined in detail regarding MAR systems. In general, a high hydraulic gradient is not favoured for MAR implementation, as it causes higher water loss and mixing of recharge water with native groundwater. However, during groundwater-dependent ecosystem (GDE) rehabilitation, these hydraulic gradient-driven flow processes can be taken advantage of. The aim of this research is to test this hypothesis by evaluating the effect of groundwater table inclination, topography, and other local characteristics on MAR efficiency from the perspective of GDE restoration. MAR efficiency was examined from recharge to discharge area in a simple half-basin based on theoretical flow simulations, using GeoStudio SEEP/W software. Different scenarios were compared to analyse the groundwater level increase and the infiltrated water volumes and to assess the efficiency of MAR based on these parameters in each scenario. The theoretical results were applied to a close-to-real situation of Lake Kondor, a GDE of the Danube-Tisza Interfluve (Hungary), which dried up in the past decades due to groundwater decline in the area. Based on the results, initial hydraulic head difference, model length, and hydraulic conductivity are the most critical parameters regarding water level increase at the discharge area. The water amount needed for increasing the water table is mainly influenced by the thickness of the unsaturated zone and the material properties of the aquifer. The findings can help better understand MAR efficiency in light of local groundwater flow processes and contribute to optimising MAR systems. The results of the study suggest that, if water is infiltrated at the local recharge area, the water table will also increase at the corresponding discharge area, which positively effects the connected GDEs. This approach can serve as a nature-based solution (NBS) to sustain sensitive ecosystems in changing climatic conditions.
  • Multimethodological Revisit of the Surface Water and Groundwater Interaction in the Balaton Highland Region—Implications for the Overlooked Groundwater Component of Lake Balaton, Hungary
    Ádám Tóth, Petra Baják, Márk Szijártó, Mia Tiljander, Kirsti Korkka-Niemi, Nina Hendriksson, Judit Mádl-Szőnyi
    Water Switzerland, 2023
    The hummocky Balaton Highland is located in western Hungary and is part of the Transdanubian Mountains, the most extensive carbonate aquifer system in Hungary. The study region also encompasses Lake Balaton, the biggest lake in central Europe, which is to the south of Balaton Highland. The surface water–groundwater interaction in the Balaton Highland–Lake Balaton region and the groundwater contribution to Lake Balaton are revisited in this paper. Hydrostratigraphic classification was performed first; then, groundwater flow directions by hydraulic head distribution were analysed, and baseflow indices of surface watercourses were calculated. Regarding hydrochemical characterisation, general hydrochemical facies were identified, natural tracers of temperature, chloride and uranium were applied, and the stable isotopic composition of oxygen and hydrogen was determined. Finally, groundwater flow and heat transport were simulated in a 2D numerical model. A high level of hydraulic interaction was evidenced between surface water and groundwater and the sub-regions of Bakony Mountains, Balaton Highland and Lake Balaton by physical and chemical parameters, numerical simulation and groundwater-flow-related natural manifestations, revealing hydraulic continuity in the study region. Based on the results, the division of legislative water bodies can be reconsidered, especially that surface water and groundwater should be regarded as interconnected, and Lake Balaton can be considered a groundwater-dependent ecosystem in any water-use planning in the region.
  • From basin-scale groundwater flow to integrated geofluid research in the hydrogeology research group of Eötvös Loránd University, Hungary
    Brigitta Czauner, Anita Erőss, Szilvia Szkolnikovics-Simon, Ábel Markó, Petra Baják, Tímea Trásy-Havril, Márk Szijártó, Zsóka Szabó, Katalin Hegedűs-Csondor, Judit Mádl-Szőnyi
    Journal of Hydrology X, 2022
    This review paper briefly summarizes the research results of the majority (∼70%) women team of the Hydrogeology Research Group of Eötvös Loránd University, Hungary, led by Judit Mádl-Szőnyi. The group had originally focused on basin-scale groundwater flow systems and the related processes and phenomena but extended its research activity to other geofluids in answer to global challenges such as the water crisis, climate change, and energy transition. However, the core concept of these studies remained the basin-scale system approach of groundwater flow, as these flow systems interact with the rock framework and all other geofluids resulting in a systematic distribution of the related environmental and geological processes and phenomena. The presented methodological developments and mostly general results have been and can be utilized in the future in any sedimentary basins. These cover the following fields of hydrogeology and geofluid research: carbonate and karst hydrogeology, asymmetric basin and flow pattern, geothermal and petroleum hydrogeology, radioactivity of groundwater, groundwater and surface water interaction, groundwater-dependent ecosystems, effects of climate change on groundwater flow systems, managed aquifer recharge.
  • Interaction of basin-scale topography- and salinity-driven groundwater flow in synthetic and real hydrogeological systems
    Attila Galsa, Ádám Tóth, Márk Szijártó, Daniele Pedretti, Judit Mádl-Szőnyi
    Journal of Hydrology, 2022
    Salinization of groundwater has endangered e.g. drinking water supply, agricultural cultivation, groundwater-dependent ecosystems, geothermal energy supply, thermal and hydrocarbon well production to a rising degree. In order to investigate the problem of coupled topography- and salinity-driven groundwater flow on a basin-scale, a systematic simulation set has been carried out in a synthetic numerical model. Detailed sensitivity analysis was completed to reveal the effect of the salinity, permeability, permeability heterogeneity and anisotropy, mechanical dispersivity and water table head on the salt concentration field and the flow pattern. It was established that a saline dome with slow inner convection formed beneath the discharge zone in the base model due to the topography-driven regional fresh groundwater flow. An increase in the salinity or the anisotropy or decrease in the water table variation weakens the role of the forced convection driven by the topography, thus facilitating the formation of a saline, dense, sluggish layer in the deepest zone of the basin. In the studied parameter range, the variation in permeability and dispersivity affects the shape of the saltwater dome to less degree. However, the decrease in permeability and/or the increase in dispersivity advantage the homogenization of the salt concentration within the saline zone and strengthen the coupling between the saltwater and freshwater zone by growing the relative role of diffusion and transverse dispersion, respectively. The interaction of the topography-driven forced and salinity driven free convection was investigated along a real hydrological section in Hungary. Simulation elucidated the fresh, brackish and saline character of the water sampled the different hydrostratigraphic units by revealing the connection between the topography-driven upper siliciclastic aquifer and the lower confined karstic aquifer through faults in high-salinity clayey aquitard. The current study improves the understanding of the interaction between the topography-driven forced and the salinity-driven free convection, i.e. topohaline convection, especially in basin-scale groundwater flow systems.
  • Numerical analysis of the potential for mixed thermal convection in the Buda Thermal Karst, Hungary
    Márk Szijártó, Attila Galsa, Ádám Tóth, Judit Mádl-Szőnyi
    Journal of Hydrology Regional Studies, 2021
  • Numerical investigation of the combined effect of forced and free thermal convection in synthetic groundwater basins
    Márk Szijártó, Attila Galsa, Ádám Tóth, Judit Mádl-Szőnyi
    Journal of Hydrology, 2019
  • Numerical sensitivity test of three-electrode laterolog borehole tool
    Márk Szijártó, László Balázs, Dezső Drahos, Attila Galsa
    Acta Geophysica, 2017

RECENT SCHOLAR PUBLICATIONS

  • Integration of time-series analysis, satellite data and machine learning in water balance assessment for the Kis-Balaton Water Protection System
    A Petneházy, M Szijártó, I Fórizs, G Czuppon, F Kapolcsi, ...
    EGU26 , 2026
    2026
  • The Effectiveness of Water Retention in Canals in the Danube-Tisza Interfluve Region, Hungary
    A Garas, A Berecz, M Szijártó, J Mádl-Szőnyi, A Kovács-Baksi, S Simon
    EGU26 , 2026
    2026
  • Topothermohaline convection–from synthetic simulations to reveal processes in a thick geothermal system
    A Galsa, M Szijártó, Á Tóth, J Mádl-Szőnyi
    Hydrology and Earth System Sciences 29 (17), 4281-4305 , 2025
    2025
  • Numerical investigation of groundwater aging and thermal processes in confined-unconfined basins with asymmetric flow patterns: The Buda Thermal Karst, Hungary
    M Szijártó, A Galsa, B Czauner, A Erőss, Á Tóth, J Mádl-Szőnyi
    Hydrogeology Journal 33 (4), 1047-1065 , 2025
    2025
    Citations: 1
  • Connections between Thermal Springs and Deep Geothermal Potential in the Buda Thermal Karst System
    T Tóthi, J Mádl-Szőnyi, Á Markó, L Ádám Csicsek, I Szilágyi, M Szijártó
    EGU General Assembly Conference Abstracts, EGU25-4392 , 2025
    2025
  • Nature-Based Managed Aquifer Recharge solutions for mitigating water shortage at Danube-Tisza Interfluve, Hungary
    S Simon, B Czauner, M Szijártó, I Erhardt, F Gyuris, I Hoffman, Á Györfi, ...
    EGU General Assembly Conference Abstracts, EGU25-19516 , 2025
    2025
  • Re-interpreting renewable and non-renewable water resources in the over-pressured Pannonian Basin
    B Czauner, M Szijártó, O Sztanó, H Ben Mahrez, J Molson, S Oláh, ...
    Scientific Reports 14 (1), 24586 , 2024
    2024
    Citations: 3
  • Geological Risk Analysis of Geothermal Developments—Case Study of the Hypogene Buda Thermal Karst
    Á Markó, T Tóthi, I Szilágyi, M Szijártó, T Trásy-Havril, J Mádl-Szőnyi
    International Conference on Eurokarst, 57-65 , 2024
    2024
  • Wetland management in recharge regions of regional groundwater flow systems with water shortage, Nyírség region, Hungary
    S Simon, J Déri-Takács, M Szijártó, L Szél, J Mádl-Szőnyi
    Water 15 (20), 3589 , 2023
    2023
    Citations: 17
  • Numerical investigation of the groundwater age and heat transport processes in asymmetric hydrogeological situations
    M Szijártó, Z Vatai, A Galsa
    EGU General Assembly Conference Abstracts, EGU-3840 , 2023
    2023
    Citations: 2
  • Geophysical survey of near-surface aquifers for the goals of Managed Aquifer Recharge in a settlement of the Danube-Tisza Interfluve, Hungary
    S Oláh, M Szijártó, F Visnovitz, J Mádl-Szőnyi
    EGU General Assembly Conference Abstracts, EGU-12862 , 2023
    2023
  • Infinite borehole field model—A new approach to estimate the shallow geothermal potential of urban areas applied to central Budapest, Hungary
    K Korhonen, Á Markó, A Bischoff, M Szijártó, J Mádl-Szőnyi
    Renewable Energy 208, 263-274 , 2023
    2023
    Citations: 13
  • Quantification of the scale of Miocene extension in the Danube Basin based on 2D balancing
    K Váradi, L Fodor, M Szijártó, L Bereczki
    EGU General Assembly Conference Abstracts, EGU-8328 , 2023
    2023
  • The significance of groundwater table inclination for nature-based replenishment of groundwater-dependent ecosystems by managed aquifer recharge
    Z Szabó, M Szijártó, Á Tóth, J Mádl-Szőnyi
    Water 15 (6), 1077 , 2023
    2023
    Citations: 23
  • Multimethodological revisit of the surface water and groundwater interaction in the Balaton Highland Region—implications for the overlooked groundwater component of Lake …
    Á Tóth, P Baják, M Szijártó, M Tiljander, K Korkka-Niemi, N Hendriksson, ...
    Water 15 (6), 1006 , 2023
    2023
    Citations: 16
  • Numerical modeling of Miocene dyke opening in the Cserhát Hills, Hungary
    D Juhász, C Lanzi, K Váradi, M Szijártó, L Fodor, F Sigmundsson
    EGU General Assembly Conference Abstracts, EGU-458 , 2023
    2023
  • From basin-scale groundwater flow to integrated geofluid research in the hydrogeology research group of Eötvös Loránd University, Hungary
    B Czauner, A Erőss, S Szkolnikovics-Simon, Á Markó, P Baják, ...
    Journal of Hydrology X 17, 100142 , 2022
    2022
    Citations: 14
  • Miocén extenziós szerkezetek vizsgálata a magyar-szlovák Kisalföldön.
    K Váradi, L Bereczki, M Szijártó, G Markos, L Fodor
    Hungarian Geophysics/Magyar Geofizika 63 (4) , 2022
    2022
  • Interaction of basin-scale topography-and salinity-driven groundwater flow in synthetic and real hydrogeological systems
    A Galsa, Á Tóth, M Szijártó, D Pedretti, J Mádl-Szőnyi
    Journal of Hydrology 609, 127695 , 2022
    2022
    Citations: 31
  • A köpenykonvekciótól a felszín alatti vízáramlás numerikus modellezéséig: In memoriam Cserepes László (1952–2002)
    A Galsa, M Herein, M Szijártó, B Süle, L Lenkey
    MAGYAR GEOFIZIKA 63 (4), 158-169 , 2022
    2022
    Citations: 1

MOST CITED SCHOLAR PUBLICATIONS

  • Numerical investigation of the combined effect of forced and free thermal convection in synthetic groundwater basins
    M Szijártó, A Galsa, Á Tóth, J Mádl-Szőnyi
    Journal of Hydrology 572, 364-379 , 2019
    2019
    Citations: 57
  • Numerical analysis of the potential for mixed thermal convection in the Buda Thermal Karst, Hungary
    M Szijártó, A Galsa, Á Tóth, J Mádl-Szőnyi
    Journal of Hydrology: Regional Studies 34, 100783 , 2021
    2021
    Citations: 40
  • Interaction of basin-scale topography-and salinity-driven groundwater flow in synthetic and real hydrogeological systems
    A Galsa, Á Tóth, M Szijártó, D Pedretti, J Mádl-Szőnyi
    Journal of Hydrology 609, 127695 , 2022
    2022
    Citations: 31
  • The significance of groundwater table inclination for nature-based replenishment of groundwater-dependent ecosystems by managed aquifer recharge
    Z Szabó, M Szijártó, Á Tóth, J Mádl-Szőnyi
    Water 15 (6), 1077 , 2023
    2023
    Citations: 23
  • Wetland management in recharge regions of regional groundwater flow systems with water shortage, Nyírség region, Hungary
    S Simon, J Déri-Takács, M Szijártó, L Szél, J Mádl-Szőnyi
    Water 15 (20), 3589 , 2023
    2023
    Citations: 17
  • Multimethodological revisit of the surface water and groundwater interaction in the Balaton Highland Region—implications for the overlooked groundwater component of Lake …
    Á Tóth, P Baják, M Szijártó, M Tiljander, K Korkka-Niemi, N Hendriksson, ...
    Water 15 (6), 1006 , 2023
    2023
    Citations: 16
  • From basin-scale groundwater flow to integrated geofluid research in the hydrogeology research group of Eötvös Loránd University, Hungary
    B Czauner, A Erőss, S Szkolnikovics-Simon, Á Markó, P Baják, ...
    Journal of Hydrology X 17, 100142 , 2022
    2022
    Citations: 14
  • Infinite borehole field model—A new approach to estimate the shallow geothermal potential of urban areas applied to central Budapest, Hungary
    K Korhonen, Á Markó, A Bischoff, M Szijártó, J Mádl-Szőnyi
    Renewable Energy 208, 263-274 , 2023
    2023
    Citations: 13
  • Numerical sensitivity test of three-electrode laterolog borehole tool
    M Szijártó, L Balázs, D Drahos, A Galsa
    Acta Geophysica 65 (4), 701-712 , 2017
    2017
    Citations: 7
  • Numerical investigation of the interaction of different driving forces on groundwater flow and temperature pattern in a theoretical basin and in the Buda Thermal Karst, Hungary
    M Szijártó, A Galsa, Á Tóth, L Lenkey, J Mádl-Szőnyi
    Geophysical Research Abstracts 21 , 2019
    2019
    Citations: 4
  • Re-interpreting renewable and non-renewable water resources in the over-pressured Pannonian Basin
    B Czauner, M Szijártó, O Sztanó, H Ben Mahrez, J Molson, S Oláh, ...
    Scientific Reports 14 (1), 24586 , 2024
    2024
    Citations: 3
  • Termohalin konverzió numerikus vizsgálata porózus közegmodellben
    M Szíjjártó, A Galsa
    Magyar Geofizika 61 (4), 177-190 , 2020
    2020
    Citations: 3
  • Existence of thermal convection in the Buda Thermal Karst: free or forced?
    M Szijártó
    Marine and Petroleum Geology 78, 738-749 , 2019
    2019
    Citations: 3
  • Interaction of topography-and salinity-driven groundwater flow in synthetic numerical models and a real geological situation.
    A Galsa, M Szijártó, Á Tóth, L Lenkey, J Mádl-Szőnyi
    Geophysical Research Abstracts 21 , 2019
    2019
    Citations: 3
  • Numerical investigation of the groundwater age and heat transport processes in asymmetric hydrogeological situations
    M Szijártó, Z Vatai, A Galsa
    EGU General Assembly Conference Abstracts, EGU-3840 , 2023
    2023
    Citations: 2
  • Interaction of temperature-and salinity-driven natural convection in homogeneous porous media
    M Szijártó, A Galsa
    EGU General Assembly, Sharing Geoscience Online, EGU2020-9896 , 2020
    2020
    Citations: 2
  • Managed Aquifer Recharge suitability mapping combined with field examination and numerical simulation in the Danube-Tisza Interfluve, Hungary
    Z Szabó, M Szijártó, M Masetti, D Pedretti, F Visnovitz, J Mádl-Szőnyi
    EGU General Assembly 2020, 1-2 , 2020
    2020
    Citations: 2
  • Numerical investigation of groundwater aging and thermal processes in confined-unconfined basins with asymmetric flow patterns: The Buda Thermal Karst, Hungary
    M Szijártó, A Galsa, B Czauner, A Erőss, Á Tóth, J Mádl-Szőnyi
    Hydrogeology Journal 33 (4), 1047-1065 , 2025
    2025
    Citations: 1
  • A köpenykonvekciótól a felszín alatti vízáramlás numerikus modellezéséig: In memoriam Cserepes László (1952–2002)
    A Galsa, M Herein, M Szijártó, B Süle, L Lenkey
    MAGYAR GEOFIZIKA 63 (4), 158-169 , 2022
    2022
    Citations: 1
  • Numerical investigation of the combined effect of different driving forces in the Buda Thermal Karst, Hungary
    M Szijártó, A Galsa, Á Tóth, L Lenkey, J Mádl-Szőnyi
    46th Annual Congress of the International Association of Hydrogeologists … , 2019
    2019
    Citations: 1