@article{MTMT:35473091,
	title = {Re-interpreting renewable and non-renewable water resources in the over-pressured Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/35473091},
	author = {Czauner, Brigitta and Szijártó, Márk and Sztanó, Orsolya and Ben Mahrez, Hana and Molson, John and Oláh, Soma and Mádlné Szőnyi, Judit},
	doi = {10.1038/s41598-024-76076-8},
	journal-iso = {SCI REP},
	journal = {SCIENTIFIC REPORTS},
	volume = {14},
	unique-id = {35473091},
	year = {2024},
	eissn = {2045-2322},
	orcid-numbers = {Czauner, Brigitta/0000-0001-6591-8611; Szijártó, Márk/0000-0001-5408-4092; Sztanó, Orsolya/0000-0003-0786-3653; Mádlné Szőnyi, Judit/0000-0002-5628-4386}
}

@article{MTMT:35320518,
	title = {Groundwater Flow Controlled Migration of Dissolved Microbial Gas in the Eastern Hungarian Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/35320518},
	author = {Czauner, Brigitta and Adonya, Romario Albert and Márton, Béla},
	doi = {10.1144/SP555-2023-186},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {555},
	unique-id = {35320518},
	issn = {0305-8719},
	abstract = {Formation of commercial microbial gas accumulations requires specific migration and accumulation conditions which can be effectively provided by groundwater flow systems. Namely, if microbial methane can be gathered and transported in aqueous solution over large lateral distances, great amount of free gas can be exsolved where flows turn upward causing a decrease in solubility. Based on this concept and the flow pattern of regional scale topography-driven groundwater flow systems, the present study built a simplistic 2D model in MS Excel including a methane solubility database with 32000 data. The model can calculate the required flow pathway length to saturate groundwater with methane, the amount of free gas that can be released in a potential accumulation zone, and the necessary time interval for the whole process. Application of the model was demonstrated based on the geological and hydrogeological conditions of a study area in the Central Pannonian Basin (Hungary) focusing on the Hajdúszoboszló gas field. In light of the upscaled results of the 2D model, the known microbial gas accumulations of the study area could be charged according to the model. In addition, parameter sensitivity analysis also provided valuable insights into the complex mechanisms of microbial gas migration.},
	year = {2024},
	eissn = {2041-4927},
	orcid-numbers = {Czauner, Brigitta/0000-0001-6591-8611}
}

@article{MTMT:34874660,
	title = {How to consider groundwater flow systems in the Earth's Critical Zone? – Demonstration in the Central Pannonian Basin, Hungary},
	url = {https://m2.mtmt.hu/api/publication/34874660},
	author = {Czauner, Brigitta and Simon, Szilvia and Mádlné Szőnyi, Judit},
	doi = {10.1016/j.ejrh.2024.101833},
	journal-iso = {J HYDROL-REG STUD},
	journal = {JOURNAL OF HYDROLOGY: REGIONAL STUDIES},
	volume = {53},
	unique-id = {34874660},
	abstract = {Study region Central Pannonian Basin, Hungary. Study focus Critical Zone (CZ) Science generally focuses on the soil and weathered bedrock in a few or tens of meters depth, thus influence of deeper groundwater on the CZ is understudied. Here we aim to introduce a hydrogeological methodology that can separate normal and abnormal pressure regimes and determine the groundwater flow pattern to characterize the connection of different groundwater flow systems to the CZ. Basin-scale evaluation of about 5500 measured hydraulic data were carried out by p(z) and h(z) profiles, tomographic maps and hydraulic cross sections. New hydrological insights for the Region Three flow domains were separated and characterized. Namely, i) the uppermost topography-driven flow systems, which penetrate only a few hundred meters, ii) a deep overpressured regime below 1600–2100 m depth, which drives fluids upward; and iii) a newly identified transition zone between the former two, which gains its energy from overpressure dissipation and contains non-renewable water resources. Topography-driven flow systems and discharge areas of the transition zone, where its upwelling saline water contributes to surface salinization, are parts of the CZ. Discharge areas of the transition zone cover about 50% of the Great Hungarian Plain. The overpressured system can only influence the CZ through the transition zone. The approach and methodology can be used in any terrestrial sedimentary basin where a deep overpressured regime exists.},
	keywords = {climate change; Critical Zone; Overpressure; groundwater flow systems; Topography-driven; Surface salinization},
	year = {2024},
	eissn = {2214-5818},
	orcid-numbers = {Czauner, Brigitta/0000-0001-6591-8611; Simon, Szilvia/0000-0002-3811-9141; Mádlné Szőnyi, Judit/0000-0002-5628-4386}
}

@CONFERENCE{MTMT:35076255,
	title = {Flow, transport and karstification model of the Buda Thermal Karst, Hungary - theoretical and practical consequences},
	url = {https://m2.mtmt.hu/api/publication/35076255},
	author = {Mádlné Szőnyi, Judit and Czauner, Brigitta and Erőss, Anita and Szijártó, Márk and Tóth, Ádám and Trásy-Havril, Tímea and Galsa, Attila and Kovácsné Bodor, Petra},
	booktitle = {Eurokarst Abstract book},
	unique-id = {35076255},
	year = {2024},
	pages = {1},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Czauner, Brigitta/0000-0001-6591-8611; Erőss, Anita/0000-0002-2395-3934; Szijártó, Márk/0000-0001-5408-4092; Tóth, Ádám/0000-0002-7300-6687; Trásy-Havril, Tímea/0000-0003-3478-2787; Galsa, Attila/0000-0002-7198-4524}
}

@misc{MTMT:35533037,
	title = {Climate change adaptation through groundwater flow understanding - How do we find nature-based MAR solutions?},
	url = {https://m2.mtmt.hu/api/publication/35533037},
	author = {Mádlné Szőnyi, Judit and Czauner, Brigitta and Trásy-Havril, Tímea and Szabó, Zsóka and Tóth, Ádám and Szijártó, Márk and Oláh, Soma and Simon, Szilvia},
	unique-id = {35533037},
	year = {2024},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Czauner, Brigitta/0000-0001-6591-8611; Trásy-Havril, Tímea/0000-0003-3478-2787; Tóth, Ádám/0000-0002-7300-6687; Szijártó, Márk/0000-0001-5408-4092; Simon, Szilvia/0000-0002-3811-9141}
}

@misc{MTMT:35605568,
	title = {Súlyosbodó aszály, csökkenő vízszintek, kényszerű alkalmazkodás - avagy lehet-e újat mondani a hidrogeológus szemszögéből?},
	url = {https://m2.mtmt.hu/api/publication/35605568},
	author = {Mádlné Szőnyi, Judit and Czauner, Brigitta and Szabó, Zsóka and Simon, Szilvia and Szijártó, Márk and Oláh, Soma and Trásy-Havril, Tímea and Vincze, Miklós},
	unique-id = {35605568},
	year = {2024},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Czauner, Brigitta/0000-0001-6591-8611; Simon, Szilvia/0000-0002-3811-9141; Szijártó, Márk/0000-0001-5408-4092; Trásy-Havril, Tímea/0000-0003-3478-2787; Vincze, Miklós/0000-0003-3220-7535}
}

@CONFERENCE{MTMT:35308801,
	title = {Thermal processes and groundwater ageing in the Buda Thermal Karst, Hungary},
	url = {https://m2.mtmt.hu/api/publication/35308801},
	author = {Szijártó, Márk and Galsa, Attila and Czauner, Brigitta and Tóth, Ádám and Mádlné Szőnyi, Judit},
	booktitle = {IAH2024 Davos Book of Abstracts},
	unique-id = {35308801},
	year = {2024},
	pages = {106958},
	orcid-numbers = {Szijártó, Márk/0000-0001-5408-4092; Galsa, Attila/0000-0002-7198-4524; Czauner, Brigitta/0000-0001-6591-8611; Tóth, Ádám/0000-0002-7300-6687; Mádlné Szőnyi, Judit/0000-0002-5628-4386}
}

@misc{MTMT:35605546,
	title = {Természetalapú célzott felszínalatti vízutánpótlás},
	url = {https://m2.mtmt.hu/api/publication/35605546},
	author = {Oláh, Soma and Koszta, Imola and Czauner, Brigitta and Szabó, Zsóka and Simon, Szilvia and Szijártó, Márk and Tóth, Ádám and Erhardt, Ildikó and Mádlné Szőnyi, Judit},
	unique-id = {35605546},
	year = {2024},
	orcid-numbers = {Czauner, Brigitta/0000-0001-6591-8611; Simon, Szilvia/0000-0002-3811-9141; Szijártó, Márk/0000-0001-5408-4092; Tóth, Ádám/0000-0002-7300-6687; Mádlné Szőnyi, Judit/0000-0002-5628-4386}
}

@misc{MTMT:34174184,
	title = {Topography induced shallow terrestrial water cycle: environmental and geological consequences},
	url = {https://m2.mtmt.hu/api/publication/34174184},
	author = {Czauner, Brigitta and Mádlné Szőnyi, Judit},
	unique-id = {34174184},
	year = {2023},
	orcid-numbers = {Czauner, Brigitta/0000-0001-6591-8611; Mádlné Szőnyi, Judit/0000-0002-5628-4386}
}

@misc{MTMT:34172655,
	title = {The influence of deep groundwater flow systems on the Earth’s critical zone},
	url = {https://m2.mtmt.hu/api/publication/34172655},
	author = {Czauner, Brigitta and Simon, Szilvia and Mádlné Szőnyi, Judit},
	publisher = {EGU},
	unique-id = {34172655},
	year = {2023},
	orcid-numbers = {Czauner, Brigitta/0000-0001-6591-8611; Simon, Szilvia/0000-0002-3811-9141; Mádlné Szőnyi, Judit/0000-0002-5628-4386}
}