TY - CONF AU - Vancsik, Anna AU - Szabó, Lili AU - Bauer, László AU - Király, Csilla AU - Pirger, Zsolt AU - Kondor, Attila Csaba AU - Jakab, Gergely Imre AU - Szalai, Zoltán TI - The impact of land use on the adsorption of fluoroquinolone antibiotics: a study on bulk soils and organic matter pools T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 DO - 10.5194/egusphere-egu24-8888 UR - https://m2.mtmt.hu/api/publication/34821394 ID - 34821394 N1 - poszter LA - English DB - MTMT ER - TY - CONF AU - Cseresznyés, Dóra AU - Preto, N AU - Báldi, Katalin AU - Kónya, Péter AU - Király, Csilla AU - Gelencsér, Orsolya AU - Szamosfalvi, Ágnes AU - Szabó, Csaba AU - Czuppon, György AU - Falus, György TI - Limestone reservoirs: are they good for CO2 geological storage? T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 DO - 10.5194/egusphere-egu24-12575 UR - https://m2.mtmt.hu/api/publication/34821362 ID - 34821362 N1 - poszter LA - English DB - MTMT ER - TY - CONF AU - Király, Csilla AU - Keya, Mondal J AU - Jakab, Gergely Imre AU - Karlik, Máté AU - Falus, György AU - Cseresznyés, Dóra AU - Kónya, Péter AU - Viczián, István AU - Szeberényi, József AU - Szalai, Zoltán TI - Varying weathering degree indicators within three paleosol layers T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 DO - 10.5194/egusphere-egu24-11217 UR - https://m2.mtmt.hu/api/publication/34821344 ID - 34821344 N1 - poszter LA - English DB - MTMT ER - TY - CONF AU - Jakab, Gergely Imre AU - Filep, Tibor AU - Chevallier, T AU - Szalai, Zoltán AU - Zacháry, Dóra TI - The role of (in)organic carbon removal as a pretreatment in the 13C isotope composition of various soils T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 DO - 10.5194/egusphere-egu24-9123 UR - https://m2.mtmt.hu/api/publication/34821328 ID - 34821328 N1 - poszter LA - English DB - MTMT ER - TY - CONF AU - Szabó, Lili AU - Vancsik, Anna AU - Bauer, László AU - Kondor, Attila Csaba AU - Jakab, Gergely Imre AU - Szalai, Zoltán TI - Effects of root-derived organic acids on sorption of pharmaceuticals in cultivated sandy soil T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 DO - 10.5194/egusphere-egu24-8943 UR - https://m2.mtmt.hu/api/publication/34821302 ID - 34821302 N1 - poszter LA - English DB - MTMT ER - TY - CONF AU - Bauer, László AU - Szabó, Lili AU - Vancsik, Anna AU - Kondor, Attila Csaba AU - Jakab, Gergely Imre AU - Szalai, Zoltán TI - Fixed-bed thermodynamical analysis of the sorption mechanisms of Pharmaceutically Active Compounds (PhACs) in sandy soil T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 PG - 2 DO - 10.5194/egusphere-egu24-9323 UR - https://m2.mtmt.hu/api/publication/34821260 ID - 34821260 LA - English DB - MTMT ER - TY - CONF AU - Zacháry, Dóra AU - Zatykó, Ch AU - Mihucz, Viktor Gábor AU - Filep, Tibor AU - Jakab, Gergely Imre AU - Ringer, Marianna AU - Szalai, Zoltán TI - Crystalline, poorly-crystalline and organic matter-complexed Fe and Al phases in acid and calcareous temperate forest topsoils and subsoils T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 PG - 2 DO - 10.5194/egusphere-egu24-11914 UR - https://m2.mtmt.hu/api/publication/34821205 ID - 34821205 N1 - poszter LA - English DB - MTMT ER - TY - CONF AU - Filep, Tibor AU - Zacháry, Dóra AU - Tőke, Orsolya AU - Domján, Attila AU - Szalai, Zoltán TI - Chemical differences in the non-protected carbon pool of four Hungarian soils with different vegetation types T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 DO - 10.5194/egusphere-egu24-8025 UR - https://m2.mtmt.hu/api/publication/34821191 ID - 34821191 N1 - poszter LA - English DB - MTMT ER - TY - CONF AU - Ruszkiczay-Rüdiger, Zsófia AU - Kern, Zoltán AU - Madarász, Balázs AU - Urdea, P AU - Braucher, R AU - Molnár, Mihály AU - Buró, Botond ED - Team, A / Collaborative Organization TI - New surface exposure age data using cosmogenic radionuclides 10Be and 14C to constrain the age of the last deglaciation in the Retezat Mts, Southern Carpathians, Romania T2 - EGU General Assembly 2024 : abstracts PB - European Geosciences Union (EGU) C1 - Wien PY - 2024 DO - 10.5194/egusphere-egu24-12758 UR - https://m2.mtmt.hu/api/publication/34805880 ID - 34805880 N1 - poszter LA - English DB - MTMT ER - TY - JOUR AU - Gyollai, Ildikó AU - Biri, Sándor AU - Juhász, Zoltán AU - Király, Csilla AU - Rácz, Richárd Péter AU - Rezes, Dániel AU - Sulik, Béla AU - Szabó, Máté Zoltán AU - Szalai, Zoltán AU - Szávai, P AU - Szklenár, Tamás AU - Kereszturi, Ákos TI - Raman–Infrared Spectral Correlation of an Artificially Space-Weathered Carbonaceous Chondrite Meteorite JF - MINERALS J2 - MINERALS-BASEL VL - 14 PY - 2024 IS - 3 SN - 2075-163X DO - 10.3390/min14030288 UR - https://m2.mtmt.hu/api/publication/34762210 ID - 34762210 AB - Raman and infrared measurements of the same locations were conducted on a northwest African (NWA) 10580 CO3 meteorite sample, before and after three proton irradiations (1 keV ion energy using 1011, 1014, and 1017 ion/cm2 fluent values), to simulate space weathering effects. In the case of Raman spectroscopy, both FWHM and peak positions of the major olivine and pyroxene bands changed after the irradiation, and the minor bands disappeared. In the FTIR spectra, the minor bands of olivine and pyroxene also disappeared; meanwhile, major IR bands of pyroxene remained visible, demonstrating both positive and negative peak shifts, and the olivines were characterised only by negative peak shifts. The olivines were characterised by negative FWHM changes for major bands, but positive FWHM changes for minor bands. The pyroxenes were characterised by elevated FWHM changes for minor bands after the irradiation. The disappearance of minor bands both of IR and Raman spectra indicates the amorphization of minerals. The negative peak shift in IR spectra indicates Mg loss for olivine and pyroxene, in agreement with the literature. The Raman spectra are characterised by positive peak shift and positive FWHM changes; the IR spectra are characterised by a negative peak shift. The Mg loss, which was detected by negative peak shifts of FTIR bands, may be caused by distortion of the crystal structure, which could be detected by a positive peak shift in Raman spectra. This joint observation and interpretation has not been formulated in the literature, but indicates further possibilities in the confirmation of mineral changes by different instruments. Shock alteration-based observations by other researchers could be used as a reference for irradiation experiments as irradiation makes a similar structural alteration, like a low-grade shock metamorphism. LA - English DB - MTMT ER -