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A Direct Estimate of the Initial Concentration of 14C in the Mountain Aquifer of Israel

Published online by Cambridge University Press:  18 July 2016

Israel Carmi*
Affiliation:
Department of Geophysics and Planetary Science, Tel Aviv University, Tel Aviv 69978, Israel
Joel Kronfeld
Affiliation:
Department of Geophysics and Planetary Science, Tel Aviv University, Tel Aviv 69978, Israel
Yoseph Yechieli
Affiliation:
Geological Survey of Israel, 30 Malkei Israel St, Jerusalem 95501, Israel
Elisabetta Boaretto
Affiliation:
Department of Environmental Sciences and Energy Research, Weizmann Institute of Science, Rehovot 76100, Israel
Miryam Bar-Matthews
Affiliation:
Geological Survey of Israel, 30 Malkei Israel St, Jerusalem 95501, Israel
Avner Ayalon
Affiliation:
Geological Survey of Israel, 30 Malkei Israel St, Jerusalem 95501, Israel
*
Corresponding author. Email: [email protected].
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Abstract

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Five radiocarbon analyses were performed on 5 different sources within Soreq Cave, which was used as a model for the Judea Group Aquifer of Israel (pMC q0 ). The transit time of rainwater through the roof of the cave to sources within it had been determined with tritium. From this information, the year of deposition of rain on the roof of the cave, which later appeared in one of the sources, was estimated and the atmospheric 14C concentration at that time was ascertained (pMC a0 ). The parameter Q = pMC q0 / pMC a0 was found to be Q = 0.60 ± 0.04. This makes it possible to calculate the age of water in any well in the Judea Group Aquifer of Israel by measuring its 14C concentration (pMC qt ) by use of the decay equation and applying Q.

Type
Part II
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

References

Bar-Matthews, M, Ayalon, A, Matthews, M, Sass, E, Halicz, L. 1996. Carbon and oxygen isotope study of the active water-carbonate system in a karstic Mediterranean cave: implications for paleoclimate research in semiarid regions. Geochimica et Cosmochimica Acta 60:337–47.Google Scholar
Bouhlassa, S, Aiachi, A. 2002. Groundwater dating with radiocarbon: application to an aquifer under semi-arid conditions in the south of Morocco (Guelmime). Applied Radiation and Isotopes 56:637–47.CrossRefGoogle Scholar
Buckau, G, Artinger, R, Geyer, S, Wolf, M, Fritz, P, Kim, JI. 2000. 14C dating of Gorleben groundwater. Applied Geochemistry 15:583–97.Google Scholar
Kaufman, A, Bar-Mathews, M, Ayalon, A, Carmi, I. 2003. The vadose flow above Soreq Cave, Israel: a tritium study of the cave waters. Journal of Hydrology 273: 155–63.CrossRefGoogle Scholar
Kroitoru, L. 1987. The characterization of flow systems in carbonate rocks defined by the groundwater parameters: Central Israel [PhD dissertation]. Feinberg Graduate School of the Weizmann Institute of Science, Rehovot, Israel.Google Scholar
Levin, I, Kromer, B, Schoch-Fischer, H, Bruns, M, Münnich, M, Berdau, D, Vogel, JC, Münnich, KO. 1985. 25 years of tropospheric 14C observations in Central Europe. Radiocarbon 27(1):119.Google Scholar
Levin, I, Kromer, B 1997. Twenty years of atmospheric 14CO2 observations at Schauinsland station, Germany. Radiocarbon 39(2):205–18.Google Scholar
Münnich, KO. 1957. Messungen des 14C-Gehaltes von hartem Grundwasser. Naturewissenschaften 44:32–3.CrossRefGoogle Scholar
Plummer, LN, Prestemon, EC, Parkhurst, DL. 1991. NET-PATH. US Geological Survey Water Resources Investigations Report 914078, Reston, Virginia, USA.Google Scholar
Wigley, TMI. 1975. 14C dating of groundwater from closed and open systems. Water Resources Research 11:324–8.CrossRefGoogle Scholar