TY - CHAP AU - Körösparti, János Tamás AU - Kajári, Balázs AU - Kerezsi, György AU - Túri, Norbert AU - Szőcs, Teodóra AU - Kun, Éva AU - Bozán, Csaba ED - Somlyódy, Balázs ED - Váradi, József TI - A felszín alatti vizek kitermelésének hatása a belvíz-veszélyeztetettségre T2 - Magyar Hidrológiai Társaság XL. Országos Vándorgyűlése PB - Magyar Hidrológiai Társaság (MHT) CY - Budapest SN - 9789638172457 PY - 2023 PG - 13 UR - https://m2.mtmt.hu/api/publication/34350976 ID - 34350976 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Flores Carpio, Yetzabbel Gerarda AU - Hemida, Mohamed Hamdy Eid AU - Szűcs, Péter AU - Szőcs, Teodóra AU - Fancsik, Tamás AU - Szanyi, János AU - Kovács, Balázs AU - Markos, Gábor AU - Péter, Újlaki AU - Péter, Tóth AU - McIntosh, Richard William AU - Püspöki, Zoltán TI - Integration of Geological, Geochemical Modelling and Hydrodynamic Condition for Understanding the Geometry and Flow Pattern of the Aquifer System, Southern Nyírség–Hajdúság, Hungary JF - WATER J2 - WATER-SUI VL - 15 PY - 2023 IS - 16 PG - 26 SN - 2073-4441 DO - 10.3390/w15162888 UR - https://m2.mtmt.hu/api/publication/34109504 ID - 34109504 AB - Geological heterogeneity impacts groundwater flow patterns, necessitating a detailed hydrogeological framework for conceptualization process of aquifer systems. This research developed a new conceptual model of detailed geologic geometry by integrating 133 well-logs, 366 hydrodynamic data and 118 water samples. As new results, systematic 3D log correlation detected four distinct hydrostratigraphic units in the Southern Nyírség–Hajdúság Groundwater Body (East Hungary). The primary aquifer was identified as an incised valley 10–13 km wide and a NE–SW strike. Logan’s approach estimated the average hydraulic conductivity of the Incised Valley Unit (IVU) at 11 m/d, higher than the other three aquifers (3.2 m/d to 4.6 m/d). The average specific capacity of wells screening the IVU is 315.6 m3/d/m, in contrast with the remaining aquifers ranging from 31.6 m3/d/m to 92 m3/d/m. Pressure–depth profiles, dynamic pressure increment and hydraulic head maps revealed recharge–discharge zones and hydraulic windows between hydrostratigraphic units. The elongated pattern on the hydraulic head map at the depth of the IVU showed the existence of a preferential path along its axis within the mapped borders of the IVU. Hydrochemical analysis revealed Ca-Mg-HCO3 water type within the primary aquifer and Na-HCO3 water type in the laterally connected aquifer. The saturation index values indicated a transition from undersaturated to supersaturated state inside the main aquifer for calcite and dolomite minerals. The correlation matrix and PCA results demonstrated that the carbonate weathering process is the main factor controlling the groundwater chemistry. This integrated approach holds significance for future applications of the regional conceptual model in water management planning, sustainable aquifer development and contaminant transport modelling. It provides essential contributions to informed decision-making and the formulation of effective strategies, ensuring the long-term availability and utilization of groundwater resources. LA - English DB - MTMT ER - TY - JOUR AU - Giménez-Forcada, Elena AU - Luque-Espinar, Juan Antonio AU - López-Bahut, María Teresa AU - Grima-Olmedo, Juan AU - Jiménez-Sánchez, Jorge AU - Ontiveros-Beltranena, Carlos AU - Díaz-Muñoz, José Ángel AU - Elster, Daniel AU - Skopljak, Ferid AU - Voutchkova, Denitza AU - Hansen, Birgitte AU - Hinsby, Klaus AU - Schullehner, Jörg AU - Malcuit, Eline AU - Gourcy, Laurence AU - Szőcs, Teodóra AU - Gál, Nóra Edit AU - Þorbjörnsson, Daði AU - Tedd, Katie AU - Borozdins, Dāvis AU - Debattista, Henry AU - Felter, Agnieszka AU - Cabalska, Jolanta AU - Mikołajczyk, Anna AU - Pereira, Ana AU - Sampaio, Jose AU - Perşa, Diana AU - Petrović Pantic, Tanja AU - Rman, Nina AU - Arnó, Georgina AU - Herms, Ignasi AU - Rosenqvist, Lars TI - Analysis of the geological control on the spatial distribution of potentially toxic concentrations of As and F- in groundwater on a Pan-European scale JF - ECOTOXICOLOGY AND ENVIRONMENTAL SAFETY J2 - ECOTOX ENVIRON SAFE VL - 247 PY - 2022 SN - 0147-6513 DO - 10.1016/j.ecoenv.2022.114161 UR - https://m2.mtmt.hu/api/publication/33215552 ID - 33215552 LA - English DB - MTMT ER - TY - JOUR AU - Rman, Nina AU - Szőcs, Teodóra AU - Palcsu, László AU - Lapanje, Andrej TI - Chemical and isotopic composition of CO2-rich magnesium-sodium-bicarbonate-sulphate-type mineral waters from volcanoclastic aquifer in Rogaska Slatina, Slovenia JF - ENVIRONMENTAL GEOCHEMISTRY AND HEALTH J2 - ENVIRON GEOCHEM HLTH VL - 44 PY - 2022 SP - 2187 EP - 2214 PG - 28 SN - 0269-4042 DO - 10.1007/s10653-021-01062-2 UR - https://m2.mtmt.hu/api/publication/32272943 ID - 32272943 N1 - Geological Survey of Slovenia (GeoZS), Dimičeva ulica 14, Ljubljana, 1000, Slovenia Mining and Geological Survey of Hungary (MBFSZ), Columbus u. 17-23, Budapest, 1145, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Bem tér 18/c, Debrecen, 4026, Hungary Export Date: 4 January 2023 Correspondence Address: Rman, N.; Geological Survey of Slovenia (GeoZS), Dimičeva ulica 14, Slovenia; email: nina.rman@geo-zs.si AB - Bottled natural mineral waters from an andesitic aquifer in Slovenia are enriched in magnesium (1.1 g/l), sulphate (2.2 g/l) and dissolved inorganic carbon (204 g/l). We analysed major ions, trace elements, tritium activity, C-14, delta O-18(H2O), delta H-2(H2O,)delta C-13(DIC), gas composition and noble gases in six wells. In addition, Sr-87/Sr-/86, delta S-34(SO4) and delta B-11 were analysed here for the first time. Stable isotopes with delta O-18 = -11.97 to -10.30 parts per thousand and delta H-2 = -77.3 to -63.8 confirm meteoric origin. CO2 degassing is evident at three wells, causing the oxygen shift of about -1.3 parts per thousand. Tritium activity was detectable only in the shallowest well, where the freshwater component was dated to the 1960s. delta C-13(DIC) in five waters is -1.78 to + 1.33 parts per thousand, typical of carbonate dissolution. Radiocarbon is low, 1.03-5.16 pMC. Chemical correction with bicarbonate concentration and delta C-13 correction methods gave best mean residence times, slightly longer than previously published. Sulphate has delta S-34 26.6-28.9 parts per thousand and delta O-18 8.9-11.1 parts per thousand due to dissolution of evaporites in carbonate rocks. Boron at concentrations of 1.2-6.1 mg/l has two origins: delta B-11 = 11.3-16.4 parts per thousand from hydrothermal alteration and delta B-11 = 26.6-31.7 parts per thousand from carbonate dissolution. Strontium at concentrations of 0.5-22.0 mg/l has Sr-87/Sr-/86, indicating three sources: 0.7106 for Miocene clastic rocks, 0.7082 for Triassic carbonates and 0.7070 for Lower Oligocene andesitic rocks. CO2 represents the majority of the dissolved (> 98.84 vol%) and separated gas (> 95.23 vol%). Methane is only found in two wells with a max. of 0.30 vol%. All waters show excess helium and 16-97% of mantle-derived helium. Since all show subsurface degassing, the paleo-infiltration temperature could not be calculated. LA - English DB - MTMT ER - TY - JOUR AU - Püspöki, Zoltán AU - Gibbard, PL AU - Nádor, A AU - Thamóné Bozsó, Edit AU - Sümegi, Pál AU - Fogarassy-Pummer, Tímea AU - McIntosh, Richard William AU - Lantos, M AU - Tóth‐Makk, Á AU - Stercel, F AU - Krassay, Z AU - Kovács, Péter Gábor AU - Szőcs, Teodóra AU - Fancsik, Tamás TI - Fluvial magnetic susceptibility as a proxy for long‐term variations of mountain permafrost development in the Alp‐Carpathian region JF - BOREAS J2 - BOREAS VL - 50 PY - 2021 IS - 3 SP - 806 EP - 825 PG - 20 SN - 0300-9483 DO - 10.1111/bor.12520 UR - https://m2.mtmt.hu/api/publication/31950068 ID - 31950068 LA - English DB - MTMT ER - TY - JOUR AU - Püspöki, Zoltán AU - Fogarassy-Pummer, Tímea AU - Thamóné Bozsó, Edit AU - Falus, György AU - Cserkész-Nagy, Ágnes AU - Szappanos, B AU - Márton Péterné Szalay, Emőke AU - Lantos, Zoltán AU - Szabó, Szilárd AU - Stercel, F AU - Tóth‐Makk, Á AU - McIntosh, Richard William AU - Szőcs, Teodóra AU - Pálóczy, P AU - Fancsik, Tamás TI - High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data JF - BOREAS J2 - BOREAS VL - 50 PY - 2021 IS - 1 SP - 205 EP - 223 PG - 19 SN - 0300-9483 DO - 10.1111/bor.12471 UR - https://m2.mtmt.hu/api/publication/31621407 ID - 31621407 N1 - Mining and Geological Survey of Hungary, Stefánia út 14, Budapest, H-1143,, Hungary Hungarian Malacological Society, Stefánia út 14, Budapest, H-1143,, Hungary Department of Mineralogy and Geology, University of Debrecen, Egyetem tér 1, Debrecen, H-4032, Hungary Department of Physical Geography and Geoinformatics, University of Debrecen, Egyetem tér 1, Debrecen, H-4032, Hungary Cited By :1 Export Date: 26 August 2022 Correspondence Address: Püspöki, Z.; Mining and Geological Survey of Hungary, Stefánia út 14, Hungary; email: puspoki.zoltan@mbfsz.gov.hu LA - English DB - MTMT ER - TY - GEN ED - Püspöki, Zoltán AU - Fogarassy-Pummer, Tímea AU - Cserkész-Nagy, Ágnes AU - Thamóné Bozsó, Edit AU - Kónya, Péter AU - Markos, Gábor AU - Demény, K. AU - Pálfi, É AU - Tihanyiné, Szép E. AU - Angyal, J. AU - Szőcs, Teodóra AU - Báthori, I.-né TI - HGFO–9 Paleoklíma változások kimutatás ásványtan-geokémiai módszerekkel PY - 2020 SP - 1 EP - 72 PG - 73 UR - https://m2.mtmt.hu/api/publication/31991821 ID - 31991821 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Püspöki, Zoltán AU - Fogarassy-Pummer, Tímea AU - Thamóné Bozsó, Edit AU - Berényi, Bernadett AU - Cserkész-Nagy, Ágnes AU - Szappanos, B AU - Márton Péterné Szalay, Emőke AU - Lantos, Zoltán AU - Nádor, Annamária AU - Fancsik, Tamás AU - Stercel, F AU - Tóth‐Makk, Á AU - McIntosh, Richard William AU - Szőcs, Teodóra AU - Faragó, Enikő TI - High‐resolution stratigraphy of a Quaternary fluvial deposit based on magnetic susceptibility variations (Jászság Basin, Hungary). JF - BOREAS J2 - BOREAS VL - 49 PY - 2020 IS - 1 SP - 181 EP - 199 PG - 19 SN - 0300-9483 DO - 10.1111/bor.12412 UR - https://m2.mtmt.hu/api/publication/30829948 ID - 30829948 N1 - Mining and Geological Survey of Hungary, Stefánia út 14, Budapest, H-1143, Hungary Research Centre for Natural Sciences, Hungarian Academy of Sciences, Magyar tudósok körútja 2, Budapest, H-1117, Hungary Hungarian Malacological Society, Stefánia út 14, Budapest, H-1143, Hungary Department of Mineralogy and Geology, University of Debrecen, Egyetem tér 1, Debrecen, H-4032, Hungary Export Date: 27 November 2019 Correspondence Address: Püspöki, Z.; Mining and Geological Survey of Hungary, Stefánia út 14, Hungary; email: puspoki.zoltan@mbfsz.gov.hu AB - Quaternary fluvial succession of the Jaszsag Basin (Hungary) was investigated, challenging the stratigraphical potential of 'early postglacial fluvial magnetic susceptibility episodes' recognized earlier in the Koros Basin. Low field magnetic susceptibility (MS) was measured in four boreholes from the basin centre and margins, representing channel and flood-plain environments. Statistical distributions of MS data contain significant sets of outliers, regardless of facies conditions. The downhole distribution of these outliers produces magnetic susceptibility cycles. Supported by magnetic susceptibility cycles, high-resolution facies correlations were performed reflecting a steady palaeohydrographical situation in the area, with a trunk river to the southeast and tributaries to the northwest. SEM-EDX data revealed that ferromagnetic grains are responsible for the outlying MS values. The heterogeneous association of magnetite indicates a catchment area with volcanic and metamorphic rocks, while the group of small (<5 mu m) magnetite octahedrons originated from nearby rhyolitic tuff formations. Magnetic grains were transported along channel belts, while small (<2 mu m) magnetic particles were floated onto flood-plains attached to clays. Climatic control is indicated by peaks at similar to 100 ka frequency in spectra of MS records and was also detected in palaeosol development and in flood frequency using the spectra of measured colour (similar to 100 ka) and logged resistivity (similar to 100 ka, similar to 41 ka), respectively. The climate-dependent MS signal traceable far into the basin in both channel and flood-plain environments can be summoned when the Quaternary fluvial succession of the Pannonian Basin is investigated, assuming some sources of magnetite in the catchment areas. According to the concept of 'fluvial magnetic susceptibility episodes', the early postglacial escape and spreading of the magnetite fraction control the MS signal that can support mapping of the unconformable Quaternary base and building of high-resolution models of aquifers. LA - English DB - MTMT ER - TY - CHAP AU - Šram, D. AU - Vengust, A. AU - Rman, N. AU - Lapanje, A. AU - Marković, T. AU - Šolaja, D. AU - Larva, O. AU - Avanić, R. AU - Ádám, L. AU - Gál, Nóra Edit AU - Mérész, E. AU - Szőcs, Teodóra AU - Rotárné Szalkai, Ágnes ED - Nádor, Annamária TI - The Slovenian–Hungarian–Croatian pilot area. T2 - Cascades and Calories PB - EU Interreg Danube Transnational Programme CY - Belgrade SN - 9788673523552 PY - 2019 SP - 99 EP - 114 PG - 15 UR - https://m2.mtmt.hu/api/publication/31345852 ID - 31345852 LA - English DB - MTMT ER - TY - CHAP AU - Rman, N. AU - Lapanje, A. AU - Gál, Nóra Edit AU - Marković, T. AU - Samardžić, N. AU - Jolović, B. AU - Vranješ, A. AU - Vîjdea, A.-M. AU - Rotárné Szalkai, Ágnes AU - Szőcs, Teodóra AU - Mérész, E. AU - Szanyi, J. AU - Šolaja, D. AU - Lenuta-Bǎlan, L. AU - Olah, S. AU - Krunić, O. AU - Bobovećki, I. AU - Pavić, S. ED - Nádor, Annamária TI - Thermal water utilisation practice. T2 - Cascades and Calories PB - EU Interreg Danube Transnational Programme CY - Belgrade SN - 9788673523552 PY - 2019 SP - 51 EP - 58 PG - 8 UR - https://m2.mtmt.hu/api/publication/31345837 ID - 31345837 LA - English DB - MTMT ER -