prikaz prve stranice dokumenta Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia
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Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia
Water, 12 (2020), 9; 2414. https://doi.org/10.3390/w12092414
Krajcar Bronić, Ines; Barešić, Jadranka; Sironić, Andreja; Lovrenčić Mikelić, Ivanka; Borković, Damir; Horvatinčić, Nada; Kovač, Zoran

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Isotope composition of precipitation, groundwater, surface and lake waters from Plitvice Lakes, Croatia : supplementary material | Prilog
Citirajte ovaj rad

Krajcar Bronić, I., Barešić, J., Sironić, A., Lovrenčić Mikelić, I., Borković, D., Horvatinčić, N. i Kovač, Z. (2020). Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia. Water, 12. (9). doi: 10.3390/w12092414

Krajcar Bronić, Ines, et al. "Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia." Water, vol. 12, br. 9, 2020. https://doi.org/10.3390/w12092414

Krajcar Bronić, Ines, Jadranka Barešić, Andreja Sironić, Ivanka Lovrenčić Mikelić, Damir Borković, Nada Horvatinčić i Zoran Kovač. "Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia." Water 12, br. 9 (2020). https://doi.org/10.3390/w12092414

Krajcar Bronić, I., et al. (2020) 'Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia', Water, 12(9). doi: 10.3390/w12092414

Krajcar Bronić I, Barešić J, Sironić A, Lovrenčić Mikelić I, Borković D, Horvatinčić N, i sur.. Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia. Water [Internet]. 28.08.2020. [pristupljeno 01.10.2024.];12(9). doi: 10.3390/w12092414

I. Krajcar Bronić, et al., "Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia", Water, vol. 12, br. 9, Kolovoz 2020. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:980763. [Citirano: 01.10.2024.]

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Podaci o radu
Naslov (engleski)Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia
AutorInes Krajcar Bronić
AutorJadranka Barešić
AutorAndreja Sironić
AutorIvanka Lovrenčić Mikelić
AutorDamir Borković
AutorNada Horvatinčić
AutorZoran Kovač
Autorova ustanovaInstitut Ruđer Bošković
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Fizika
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Kemija
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Interdisciplinarne prirodne znanosti
Sažetak (engleski)
The application of tritium, 2H, and 18O in the characterization of the precipitation, groundwater, and surface and lake water of the Plitvice Lakes (PL), Croatia, over the 1979–2019 period is presented. An increase in the mean annual air temperature of 0.06 °C/year and in the annual precipitation amount of 10 mm/year is observed. The good correlation of the tritium activity concentration in the PL and Zagreb precipitation implies that the tritium data for Zagreb are applicable for the study of the PL area. The best local meteoric water line at PL was obtained by the reduced major axis regression (RMA) and precipitation-weighted ordinary least squares regression (PWLSR) approaches: δ2HPWLSR = (7.97 ± 0.12) δ18O + (13.8 ± 1.3). The higher deuterium excess at PL (14.0 ± 2.2 ‰) than that at Zagreb reflects the higher altitude and influence of the Mediterranean precipitation. The δ2H in precipitation ranges from −132.4‰ to −22.3‰ and δ18O from −18.3 ‰ to −4.1‰. The much narrower ranges in the groundwater (<1‰ in δ18O, <10‰ in δ2H) indicate the good mixing of waters in aquifers and short mean residence times. The higher average δ2H in all three karst springs observed after 2003 can be attributed to the increase in the mean air temperature. The mean δ2H and δ18O values in the surface and lake water increase downstream due to the evaporation of surface waters. There is no significant difference between the surface water line and the lake water line (2011–2014). The stable isotope composition of the surface and lake waters reacts to extreme hydrological conditions.
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaWater
Brojčani podacivol. 12, br. 9, 2414
e-ISSN2073-4441
DOIhttps://doi.org/10.3390/w12092414
URN:NBNurn:nbn:hr:169:980763
Datum objave publikacije2020-08-28
URL dokumentahttps://www.mdpi.com/2073-4441/12/9/2414
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje 4.0 međunarodna (CC BY 4.0)
Datum i vrijeme pohrane2021-01-29 10:18:15