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001-es BibID:	BIBFORM074801
035-os BibID:	(Cikkazonosító)12813 (WOS)000442608400001 (Scopus)85052329220
Első szerző:	Palcsu László (fizikus)
Cím:	Modulation of Cosmogenic Tritium in Meteoric Precipitation by the 11-year Cycle of Solar Magnetic Field Activity / László Palcsu, Uwe Morgenstern, Jürgen Sültenfuss, Gabriella Koltai, Elemér László, Marjan Temovski, Zoltán Major, Judit T. Nagy, László Papp, Carmen Varlam, Ionut Faurescu, Marianna Túri, László Rinyu, György Czuppon, Emese Bottyán, A. J. Timothy Jull
Dátum:	2018
ISSN:	2045-2322
Megjegyzések:	The relationship between the atmospheric concentration of cosmogenic isotopes, the change of solar activity and hence secondary neutron flux has already been proven. The temporal atmospheric variation of the most studied cosmogenic isotopes shows a significant anti-correlation with solar cycles. However, since artificial tritium input to the atmosphere due to nuclear-weapon tests masked the expected variations of tritium production rate by three orders of magnitude, the natural variation of tritium in meteoric precipitation has not previously been detected. For the first time, we provide clear evidence of the positive correlation between the tritium concentration of meteoric precipitation andneutron flux modulated by solar magnetic activity. We found trends in tritium time series for numerouslocations worldwide which are similar to the variation of secondary neutron flux and sun spot numbers.This variability appears to have similar periodicities to that of solar cycle. Frequency analysis, crosscorrelation analysis, continuous and cross wavelet analysis provide mathematical evidence that thecorrelation between solar cycle and meteoric tritium does exist. Our results demonstrate that theresponse of tritium variation in precipitation to the solar cycle can be used to help us understand its rolein the water cycle.
Tárgyszavak:	Természettudományok Földtudományok idegen nyelvű folyóiratközlemény külföldi lapban folyóiratcikk tritium, solar cycle
Megjelenés:	Scientific Reports. - 8 : 1 (2018), p. 1-9. -
További szerzők:	Morgenstern, Uwe Sültenfuss, Jürgen Koltai Gabriella László Elemér (1987-) (meteorológus előrejelző szakiránnyal) Temovski, Marjan Major Zoltán Nagy Judit, T. (1976-) (matematika tanár, közgazdász) Papp László Varlam, Carmen Faurescu, Ionut Túri Marianna (1988-) (geográfus-geoinformatikus) Rinyu László (fizikus) Czuppon György Bottyán Emese Jull, A. J. Timothy (1951-) (radiocarbon scientist)
Pályázati támogatás:	GINOP-2.3.2.-15-2016-00009 'ICER' GINOP
Internet cím:	Szerző által megadott URL DOI Intézményi repozitóriumban (DEA) tárolt változat
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001-es BibID:	BIBFORM103310
035-os BibID:	(WOS)000805561200044 (Scopus)85131125056 (cikkazonosító)9202
Első szerző:	Temovski, Marjan
Cím:	Combined use of conventional and clumped carbonate stable isotopes to identify hydrothermal isotopic alteration in cave walls / Marjan Temovski, László Rinyu, István Futó, Kata Molnár, Marianna Túri, Attila Demény, Bojan Otoničar, Yuri Dublyansky, Philippe Audra, Victor Polyak, Yemane Asmerom, László Palcsu
Dátum:	2022
ISSN:	2045-2322
Megjegyzések:	Alteration of conventional carbonate stable isotopes (delta O-18, delta C-13) in cave walls has been shown to be a useful tool to identify cave formation driven by deep-seated processes, i.e., hypogene karstification. If combined with a prior information on the paleowater stable isotope composition, further insights can be obtained on the temperature and the source of the paleowater. Clumped isotope composition (Delta(47)) of carbonates is an independent measurement of temperature, and if combined with the conventional stable isotopes, can provide information on the paleowater stable isotope composition. On the example of Provalata Cave (N. Macedonia), we apply for the first time, both conventional and clumped stable isotope analysis, and identify two different isotope alteration trends, reflecting two distinct hydrothermal events: an older, hotter one, where isotope alteration was likely related to isotope diffusion, lowering the delta O-18 values of the carbonate; and a younger one, related to the cave formation by low-temperature CO2-rich thermal waters, with dissolution-reprecipitation as the alteration mechanism, causing decrease in delta O-18 values, and unexpected increase in delta C-13 values. The findings are further corroborated by additional insight from optical petrography and cathodoluminescence microscopy, as well as fluid inclusion analysis of secondary calcite crystals related to the cave forming phase.
Tárgyszavak:	Természettudományok Fizikai tudományok idegen nyelvű folyóiratközlemény külföldi lapban folyóiratcikk
Megjelenés:	Scientific Reports. - 12 : 1 (2022), p. 1-17. -
További szerzők:	Rinyu László (fizikus) Futó István (fizikus) Molnár Kata Túri Marianna (1988-) (geográfus-geoinformatikus) Demény Attila Otoničar, Bojan Dublyansky, Yuri Audra, Philippe Polyak, Victor Asmerom, Yemane Palcsu László (1975-) (fizikus)
Pályázati támogatás:	GINOP-2.3.2-15-2016-00009 GINOP
Internet cím:	Szerző által megadott URL DOI Intézményi repozitóriumban (DEA) tárolt változat
Borító:
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