prikaz prve stranice dokumenta Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia
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Scientific paper - Original scientific paper
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 | Appendix
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Krajcar Bronić, I., Barešić, J., Sironić, A., Lovrenčić Mikelić, I., Borković, D., Horvatinčić, N. & 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, no. 9, 2020. https://doi.org/10.3390/w12092414

Krajcar Bronić, Ines, Jadranka Barešić, Andreja Sironić, Ivanka Lovrenčić Mikelić, Damir Borković, Nada Horvatinčić and Zoran Kovač. "Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia." Water 12, no. 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, and sur.. Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia. Water [Internet]. 2020 August 28 [cited 2024 October 01];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, no. 9, August 2020. [Online]. Available at: https://urn.nsk.hr/urn:nbn:hr:169:980763. [Accessed: 01 October 2024]

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Metadata
Title (english)Isotope composition of precipitation, groundwater, and surface and lake waters from the Plitvice Lakes, Croatia
AuthorInes Krajcar Bronić
AuthorJadranka Barešić
AuthorAndreja Sironić
AuthorIvanka Lovrenčić Mikelić
AuthorDamir Borković
AuthorNada Horvatinčić
AuthorZoran Kovač
Author's institutionRuđer Bošković Institute
Author's institutionUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Physics
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Chemistry
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Interdisciplinary Natural Sciences
Abstract (english)
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.
Keywords (english)
Languageenglish
Publication typeScientific paper - Original scientific paper
Publication statusPublished
Peer reviewPeer review - international
Publication versionPublished version
Journal titleWater
Numberingvol. 12, no. 9, 2414
e-ISSN2073-4441
DOIhttps://doi.org/10.3390/w12092414
URN:NBNurn:nbn:hr:169:980763
Publication2020-08-28
Document URLhttps://www.mdpi.com/2073-4441/12/9/2414
Type of resourceText
Access conditionsOpen access
Terms of useLicence Attribution 4.0 International (CC BY 4.0) icon
Created on2021-01-29 10:18:15