Groundwater responses to recharge in the Gacka Area, Croatia, as revealed by stable isotopes, tritium, CFCs and noble gases

Author:

Han Liang-Feng1,Roller-Lutz Zvjezdana2,Hunjak Tamara2,Lutz Hans O.23,Matsumoto Takuya1,Aggarwal Pradeep1

Affiliation:

1. Isotope Hydrology Section, Division of Physical and Chemical Sciences, Department of Nuclear Sciences and Applications, International Atomic Energy Agency

2. Stable Isotope Laboratory, Medical Faculty, Rijeka University

3. Faculty of Physics, Bielefeld University

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Reference40 articles.

1. Aeschbach-Hertig, W., Peeters, F., Beyerle, U. and Kipfer, R. (2000) Palaeotemperature reconstruction from noble gases in ground water taking into account equilibration with entrapped air. Nature 405, 1040–1044.

2. Becker, K. H., Ionescu, A. and Ionescu, M. (1978) Ground level measurements of atmospheric concentrations of CCl2F2 and CCl3F in the Wuppertal-Duesseldorf region. Pure Appl. Geophys. 116, 567–574.

3. Bonacci, O. (2012) Karst Hydrology: With Special Reference to the Dinaric Karst. Springer, Berlin.

4. Bonacci, O. and Andrić, I. (2008) Sinking karst rivers hydrology: The case of Lika and Gacka (Croatia). Acta Carsologica 37(2–3), 185–196.

5. Burgman, J. O., Calles, B. and Westman, F. (1987) Conclusions from a ten year study of oxygen-18 in precipitation and runoff in Sweden. Isotope Techniques in Water Resources Development.

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