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Ines Krajcar-Bronić

Biographic Data

ID5598014
NAMEInes Krajcar-Bronić
GIVEN NAMESInes
FAMILY NAMEKrajcar-Bronić
SIGNATUREKRAJCAR-BRONIĆ I
VERIFIEDNo
TOTAL WORKS5
TOTAL CITATIONS38
AUTHOR COUNT5
EDITOR COUNT0
FIRST PUBLICATION YEAR1986
LATEST PUBLICATION YEAR1997
H-INDEX4
  • Two Decades of Environmental Isotope Records in Croatia

    Open Access•Ines Krajcar-Bronić, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1997•Cited by: 3•References: 21

    A two-decade-long record of environmental isotopes ( 2 H, 3 H, 14 C, 18 O) in Croatia is presented and the data are statistically analyzed. The atmospheric 14 C activity for the period before the actual measurements started is reconstructed by measuring tree rings from the clean-air sites, and the past tritium activity in precipitation is estimated by the correlation of our data with the Vienna station record. The long-term 3 H record helped to d…

  • Radiocarbon Dating of Lake Sediment from Two Karst Lakes in Yugoslavia

    Open Access•Dušan Srdoč, Bogomil Obelić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 2

    Samples of sediment cores from two lakes in the karst area of northwest Yugoslavia were analyzed. Both Lakes Kozjak and Prošće are in the Plitvice National Park, Central Croatia. 14 C dating, sedimentologic, seismic, and isotopic studies, and distribution of diatoms are presented. 14 C dating of lake marl revealed a uniforn sedimentation rate in Lake Prošće as opposed to Lake Kozjak. Both lake sediments belong to the Holocene period. 14 C dating …

  • Increase of 14 C Activity of Dissolved Inorganic Carbon Along a River Course

    Open Access•Dušan Srdoč, Ines Krajcar-Bronić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 5

    Results of measurements for 3 years (1981–1983) of 14 C activity of dissolved inorganic carbon (DIG) in water samples from the Korana River, as well as that of recent tufa and aquatic plants, showed that 14 C concentration increases from karst spring to the estuary. A model describing the increase of 14 C activity was developed assuming that the increase is due to the exchange of the dissolved CO 2 in stream water with atmospheric CO 2 and to dis…

  • The Effects of Contamination of Calcareous Sediments on their Radiocarbon Ages

    Open Access•Dušan Srdoč, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1986•Cited by: 5•References: 5

    Two principal reasons for the inherent uncertainty in 14 C dating of calcareous sediments such as tufa or those of lacustrine origin are the unknown initial 14 C activity (A o ) of the sediment, mainly affecting younger (Holocene) samples, and contamination of older sediments with recent carbonate, causing 14 C ages to be excessively young. To assess the contamination effect, samples of old tufa from the Riss/Würm interglacial were examined. Thes…

  • On the Initial 14 C Activity of Karst Aquifers with Short Mean Residence Time

    Open Access•Ines Krajcar-Bronić, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 2

    The 14 C activity of total dissolved inorganic carbon (DIC) as well as tritium activity and stable isotope content ( 13 C, 2 H, 18 O) of spring water were measured for 3 consecutive years at 3 karst springs that feed Plitvice Lakes, NW Yugoslavia. The constant chemical and stable isotope composition and temperature indicated well mixed aquifers. A very short mean residence time of underground water (2–5 yr) was determined by tritium activity meas…

  • Radiocarbon Dating of Lake Sediment from Two Karst Lakes in Yugoslavia

    Open Access•Dušan Srdoč, Bogomil Obelić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 2

    Samples of sediment cores from two lakes in the karst area of northwest Yugoslavia were analyzed. Both Lakes Kozjak and Prošće are in the Plitvice National Park, Central Croatia. 14 C dating, sedimentologic, seismic, and isotopic studies, and distribution of diatoms are presented. 14 C dating of lake marl revealed a uniforn sedimentation rate in Lake Prošće as opposed to Lake Kozjak. Both lake sediments belong to the Holocene period. 14 C dating …

  • Increase of 14 C Activity of Dissolved Inorganic Carbon Along a River Course

    Open Access•Dušan Srdoč, Ines Krajcar-Bronić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 5

    Results of measurements for 3 years (1981–1983) of 14 C activity of dissolved inorganic carbon (DIG) in water samples from the Korana River, as well as that of recent tufa and aquatic plants, showed that 14 C concentration increases from karst spring to the estuary. A model describing the increase of 14 C activity was developed assuming that the increase is due to the exchange of the dissolved CO 2 in stream water with atmospheric CO 2 and to dis…

  • On the Initial 14 C Activity of Karst Aquifers with Short Mean Residence Time

    Open Access•Ines Krajcar-Bronić, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 2

    The 14 C activity of total dissolved inorganic carbon (DIC) as well as tritium activity and stable isotope content ( 13 C, 2 H, 18 O) of spring water were measured for 3 consecutive years at 3 karst springs that feed Plitvice Lakes, NW Yugoslavia. The constant chemical and stable isotope composition and temperature indicated well mixed aquifers. A very short mean residence time of underground water (2–5 yr) was determined by tritium activity meas…

  • The Effects of Contamination of Calcareous Sediments on their Radiocarbon Ages

    Open Access•Dušan Srdoč, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1986•Cited by: 5•References: 5

    Two principal reasons for the inherent uncertainty in 14 C dating of calcareous sediments such as tufa or those of lacustrine origin are the unknown initial 14 C activity (A o ) of the sediment, mainly affecting younger (Holocene) samples, and contamination of older sediments with recent carbonate, causing 14 C ages to be excessively young. To assess the contamination effect, samples of old tufa from the Riss/Würm interglacial were examined. Thes…

  • Two Decades of Environmental Isotope Records in Croatia

    Open Access•Ines Krajcar-Bronić, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1997•Cited by: 3•References: 21

    A two-decade-long record of environmental isotopes ( 2 H, 3 H, 14 C, 18 O) in Croatia is presented and the data are statistically analyzed. The atmospheric 14 C activity for the period before the actual measurements started is reconstructed by measuring tree rings from the clean-air sites, and the past tritium activity in precipitation is estimated by the correlation of our data with the Vienna station record. The long-term 3 H record helped to d…

  • Radiocarbon Dating of Lake Sediment from Two Karst Lakes in Yugoslavia

    Open Access•Dušan Srdoč, Bogomil Obelić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 2

    Samples of sediment cores from two lakes in the karst area of northwest Yugoslavia were analyzed. Both Lakes Kozjak and Prošće are in the Plitvice National Park, Central Croatia. 14 C dating, sedimentologic, seismic, and isotopic studies, and distribution of diatoms are presented. 14 C dating of lake marl revealed a uniforn sedimentation rate in Lake Prošće as opposed to Lake Kozjak. Both lake sediments belong to the Holocene period. 14 C dating …

  • Increase of 14 C Activity of Dissolved Inorganic Carbon Along a River Course

    Open Access•Dušan Srdoč, Ines Krajcar-Bronić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 5

    Results of measurements for 3 years (1981–1983) of 14 C activity of dissolved inorganic carbon (DIG) in water samples from the Korana River, as well as that of recent tufa and aquatic plants, showed that 14 C concentration increases from karst spring to the estuary. A model describing the increase of 14 C activity was developed assuming that the increase is due to the exchange of the dissolved CO 2 in stream water with atmospheric CO 2 and to dis…

  • The Effects of Contamination of Calcareous Sediments on their Radiocarbon Ages

    Open Access•Dušan Srdoč, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1986•Cited by: 5•References: 5

    Two principal reasons for the inherent uncertainty in 14 C dating of calcareous sediments such as tufa or those of lacustrine origin are the unknown initial 14 C activity (A o ) of the sediment, mainly affecting younger (Holocene) samples, and contamination of older sediments with recent carbonate, causing 14 C ages to be excessively young. To assess the contamination effect, samples of old tufa from the Riss/Würm interglacial were examined. Thes…

  • On the Initial 14 C Activity of Karst Aquifers with Short Mean Residence Time

    Open Access•Ines Krajcar-Bronić, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1986•Cited by: 10•References: 2

    The 14 C activity of total dissolved inorganic carbon (DIC) as well as tritium activity and stable isotope content ( 13 C, 2 H, 18 O) of spring water were measured for 3 consecutive years at 3 karst springs that feed Plitvice Lakes, NW Yugoslavia. The constant chemical and stable isotope composition and temperature indicated well mixed aquifers. A very short mean residence time of underground water (2–5 yr) was determined by tritium activity meas…

  • Two Decades of Environmental Isotope Records in Croatia

    Open Access•Ines Krajcar-Bronić, Nada Horvatinčić et al.•ARTICLE•Radiocarbon•1997•Cited by: 3•References: 21

    A two-decade-long record of environmental isotopes ( 2 H, 3 H, 14 C, 18 O) in Croatia is presented and the data are statistically analyzed. The atmospheric 14 C activity for the period before the actual measurements started is reconstructed by measuring tree rings from the clean-air sites, and the past tritium activity in precipitation is estimated by the correlation of our data with the Vienna station record. The long-term 3 H record helped to d…

Geology (5 works) · Radiocarbon dating (4 works) · Chemistry (3 works) · Geology and Paleoclimatology Research (3 works) · Isotope Analysis in Ecology (3 works) · Karst (3 works) · Absolute dating (2 works) · Archaeology and ancient environmental studies (2 works) · Carbonate (2 works) · Ecology (2 works)

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