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Radiocarbon Variability in Groundwater in an Extremely Arid Zone—The Arava Valley, Israel

Published online by Cambridge University Press:  09 February 2016

Avihu Burg ,
Michael Zilberbrand  and
Yoseph Yechieli
Avihu Burg*
Affiliation:
Geological Survey of Israel, 30 Malkhe Israel St., Jerusalem 95501, Israel
Michael Zilberbrand
Affiliation:
Israeli Water Administration, Hydrological Service, P.O. Box 36118, Jerusalem 91360, Israel
Yoseph Yechieli
Affiliation:
Geological Survey of Israel, 30 Malkhe Israel St., Jerusalem 95501, Israel
*
2Corresponding author. Email: [email protected].
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Abstract

Radiocarbon values of groundwater in main aquifers of the extremely arid Negev Desert and the Arava Valley, southern Israel, are used for studying the underground flow regime, particularly the complex connections between different aquifers and mixing of water bodies. The study shows that 14C can serve as a hydrological tracer in arid environments and that groundwater dating may be possible (although not very accurate) even in this extremely arid environment (precipitation, <50 mm/yr), where there is almost no vegetation. There are several aquifers in this region, some of which are deep (deeper than 500 m) and regional and contain mainly fossil water, while others are local and restricted to the Arava, much shallower (50–200 m) and are thought to contain historical to recent waters. Most of the current recharge to these shallow unconsolidated aquifers comes from flash floods that flow from the mountains rising on both sides of the valley. The groundwater in the deep aquifers has low 14C values (usually <5 pMC), implying old ages (preliminary ages >26,000 yr). Groundwater in the shallow aquifers characterized by higher 14C values (up to 60–70 pMC) imply younger ages and faster groundwater flow (recent recharge). This is also supported by the presence of tritium in some of the samples. A few exceptional values are explained by the unique mixing of water from different sources; another is due to a technical failure in the well.

Type
Articles
Information
Radiocarbon , Volume 55 , Issue 2: Proceedings of the 21st International Radiocarbon Conference (Part 1 of 2) , 2013 , pp. 963 - 978
Copyright
Copyright © 2013 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

Abed el Rahman, H. 2001. Evaluation of groundwater resources in Lower Cretaceous aquifer system in Sinai. Water Resources Management 15:187–202.Google Scholar
Abed el Sarnie, SG, Sadek, MA. 2001. Groundwater recharge and flow in the Lower Cretaceous Nubian Sandstone aquifer in the Sinai Peninsula, using isotopic techniques and hydrochemistry. Hydrogeolgy Journal 9:378–89.Google Scholar
Adar, EM, Rosenthal, E, Issar, AS, Batelaan, O. 1992. Quantitative assessment of the flow pattern in the southern Arava Valley (Israel) by environmental tracers and a mixing cell model. Journal of Hydrology 136:333–52.CrossRefGoogle Scholar
Anker, Y. 2003. The evolution of the carbonate system in hyper-arid environments (Central Arava area, Israel), and its implication for 14C groundwater dating. Israel Geological Survey, Report GSI/19/03. 107 p. In Hebrew with English abstract.Google Scholar
Arad, A, Kafri, U. 1980. Hydrogeological inter-relationship between the Judea Group and the Nubian sandstone aquifers in Sinai and in the Negev. Israel Journal of Earth Sciences 29:67–72.Google Scholar
Bein, A, Yechieli, Y, Halicz, L. 1995. Geochemistry of groundwater in the southern Arava valley. Israel Geological Survey, Report GSI/43/95. 28 p In Hebrew.Google Scholar
Ben Zvi, A, Shentsis, I. 2001. Assessment of runoff as a component of water resources in the Negev and Arava. Israel Journal of Earth Sciences 50:61–70.CrossRefGoogle Scholar
Carmi, I. 1987. Rehovot radiocarbon measurements III. Radiocarbon 29(1):100–14.CrossRefGoogle Scholar
Carmi, I, Noter, Y, Schlesinger, R. 1971. Rehovot radiocarbon measurements I. Radiocarbon 13(2):412–9.CrossRefGoogle Scholar
Clark, ID, Fritz, P. 1997. Correction for carbonate dissolution. In: Environmental Isotopes in Hydrogeology. New York: Lewis Publishers. p 206–13.Google Scholar
Dahan, O, Shani, Y, Enzel, Y, Yechieli, Y, Yakirevich, A. 2007. Direct measurements of floodwater infiltration into shallow alluvial aquifers. Journal of Hydrology 344:157–70.CrossRefGoogle Scholar
Edmunds, WM, Wright, EP. 1979. Groundwater recharge and palaeoclimate in the Sirte and Kufra basins, Libya. Journal of Hydrology 40:215–41.CrossRefGoogle Scholar
Fontes, JC. 1983. Dating of groundwater. In: Guidebook of Nuclear Techniques in Hydrology. Technical Report No. 91. Vienna: IAEA. p 285–317.Google Scholar
Fridman, V, Mazor, E, Becker, A, Avraham, D, Adar, E. 1995. Stagnant aquifer concept Part 3. Stagnant mini-aquifers in the stage of formation, Makhtesh Ramon, Israel. Journal of Hydrology 173:263–82.CrossRefGoogle Scholar
Gat, JR, Mazor, E, Tzur, Y. 1969. The stable isotope composition of mineral waters in the Jordan Rift Valley, Israel. Journal of Hydrology 7:334–52.CrossRefGoogle Scholar
Gat, JR, Issar, A. 1974. Desert isotope hydrology: water sources of the Sinai Desert. Geochimica et Cosmochimica Acta 38:1171–31.CrossRefGoogle Scholar
Gat, JR, Galai, A. 1982. Groundwaters of the 'Arava Valley: an isotopic study of their origin and interrelationships. Israel Journal of Earth Sciences 31:25–38.Google Scholar
Greenbaum, N, Enzel, Y, Schick, AP. 2001. Magnitude and frequency of paleofloods and historical floods in the Arava basin, Negev Desert, Israel. Israel Journal of Earth Sciences 50:159–86.CrossRefGoogle Scholar
Guttman, Y, Burg, A, Lifshitz, A, Lumelsky, S, Zukerman, H. 1999. Hydrological model for estimation of water potential in the Arava aquifers – final report. Tahal Company, Report 6127–d99.201. 52 p In Hebrew.Google Scholar
Himida, IH. 1970. The Nubian Artesian Basin, its regional hydrogeological aspects and palaeohydrogeological reconstruction. Journal of Hydrology 9:89–116.Google Scholar
Issar, AS. 1982. A composite cumulative chemical and isotope data diagram as a tool in hydrochemical investigation. In: Proceedings, 3rd Seminar on Hydrogeology. Lisbon. p 190–200.Google Scholar
Issar, AS. 1985. Fossil water under the Sinai-Negev Peninsula. Scientific American 253(1):82–8.CrossRefGoogle Scholar
Issar, A, Bein, A, Michaeli, A. 1972. On the ancient water of the Upper Nubian sandstone aquifer in central Sinai and southern Israel. Journal of Hydrology 17:353–74.CrossRefGoogle Scholar
Issar, A, Gat, J. 1981. Environmental isotopes as a tool in hydrogeological research in an arid basin. Ground Water 19(5):490–4.Google Scholar
Knetsch, G, Shata, A, Munnich, KO, Vogel, JC, Shazly, MM. 1962. Untersuchungen an groundwasser der Ost-Sahara. Geologische Rundschau 52:587–610.Google Scholar
Kroitoru, L. 1980. The hydrogeology of the Nubian sandstone in southern Israel (lower Cretaceous) , Tel-Aviv University. In Hebrew with English abstract.Google Scholar
Kroitoru, L, Kronfeld, J, Ginzburg, A. 1981. The geohydrology of the Gerofit-Ya'alon area. Israel Journal of Earth Sciences 30:24–30.Google Scholar
Kroitoru, L, Carmi, I, Mazor, E. 1989. Groundwater 14C activity as affected by initial water-rock interactions in the Judean Mountains, Israel. Chemical Geology 79:259–74.Google Scholar
Kronfeld, J, Weinberger, G, Yaniv, A, Zafrir, H, Vulcan, U, Agami, M, Rosenthal, E. 1992. Uranium isotope disequilibrium studies and the geohydrology of the Arava Rift Valley, Israel. Nuclear Geophysics 6(4):535–45.Google Scholar
Levin, M, Gat, JR, Issar, A. 1980. Precipitation, flood- and groundwaters of the Negev highlands: an isotopic study of desert hydrology. Arid-Zone Hydrology: Investigation with Isotope Techniques. IAEA-AG-158/1. Vienna: IAEA. p 3–22.Google Scholar
Mazor, E. 1985. Mixing in natural and modified groundwater systems: detection and implications on quality and management. In: Scientific Basis for Water Resources Management. Proceedings of the Jerusalem Symposium, International Association of Hydrological Sciences Publication 153. p 193–251.Google Scholar
Mazor, E, Gilad, D, Fridman, V. 1995. Stagnant aquifer concept, Part 2. Small scale artesian systems – Hazeva, Dead Sea Rift Valley, Israel. Journal of Hydrology 173:241–61.CrossRefGoogle Scholar
Mook, WG. 1980. Carbon-14 in hydrogeological studies. In: Fritz, P, Fontes, JC, editors. Handbook Of Environmental Isotope Geochemistry 1: the Terrestrial Environment. New York: Elsevier. p 49–74.Google Scholar
Munnich, KO, Vogel, JC. 1962. Untersuchungen an pluvialen wassern der Ost-Sahara. Geologische Rundschau 52:611–24.Google Scholar
Naor, H, Granit, Y, Zurieli, A, Burg, A. 2004. Southern Arava – updating of the hydrological and geochemical state of the aquifers and boreholes for the year 2003, operational forecast for 2007 and recommendations for new boreholes. Tahal Company, Report 15046-d04.173. 62 p In Hebrew.Google Scholar
Oren, O, Yechieli, Y, Bohlke, JK, Dody, A. 2004. Contamination of groundwater under cultivated fields in an arid environment, central Arava Valley, Israel. Journal of Hydrology 290:312–28.CrossRefGoogle Scholar
Plummer, LN, Prestemon, EC, Parkhurst, DL. 1991. An interactive code (NETPATH) for modeling NET geochemical reactions along a flow PATH. US Geological Survey, Water-Resources Investigations, Report 91–4078. 227 p.Google Scholar
Plummer, LN, Sprinkle, CL. 2001. Radiocarbon dating of dissolved inorganic carbon in groundwater from confined parts of the Upper Floridan aquifer, Florida, USA. Hydrogeology Journal 9:127–50.CrossRefGoogle Scholar
Rosenthal, E, Adar, E, Issar, AS, Batelaan, O. 1990. Definition of groundwater flow patterns by environmental tracers in the multiple aquifer system of southern Arava Valley, Israel. Journal of Hydrology 117:339–68.CrossRefGoogle Scholar
Rosenthal, E, Weinberger, G, Berkowitz, B, Flexer, A, Kronfeld, J. 1992. The Nubian sandstone aquifer in central and northern Negev, Israel: delineation of hydrogeological model under conditions of scarce data. Journal of Hydrology 132:107–35.CrossRefGoogle Scholar
Rosenthal, E, Jones, BF, Weinberger, G. 1998. The chemical evolution of Kurnub Group paleowater in the Sinai-Negev province – a mass balance approach. Applied Geochemistry 13:553–69.CrossRefGoogle Scholar
Rosenthal, E, Bein, A. 2001. The Arava Rift Valley (Dead Sea Transform) – an interdisciplinary approach to assess available water resources of an arid basin. Israel Journal of Earth Sciences 50:49–52.CrossRefGoogle Scholar
Rosenthal, E, Zilberbrand, M, Livshitz, Y. 2007. The hydrochemical evolution of brackish groundwater in central and northern Sinai (Egypt) and in the western Negev (Israel). Journal of Hydrology 337:294–314.CrossRefGoogle Scholar
Schneider-Mor, A, Alsenz, H, Ashckenazi-Polivoda, S, Illner, P, Abramovich, S, Feinstein, S, Almogi-Labin, A, Berner, Z, Puttmann, W. 2012. Paleoceanographic reconstruction of the late Cretaceous oil shale of the Negev, Israel: integration of geochemical, and stable isotope records of the organic matter. Palaeogeography, Palaeoclimatology, Palaeoecology 319–320:46–57.CrossRefGoogle Scholar
Shalev, N, Gavrieli, I, Lazar, B, Burg, A. 2012. Groundwater contamination by agriculture activities in arid environment: evidence from nitrogen and oxygen isotopic composition, Arava Valley, Israel. In: Hydrogeology of Arid Environments, Proceedings. Poster abstract. Stuttgart. p 271.Google Scholar
Shiftan, ZL. 1961. New data on the artesian aquifers of the southern Dead Sea Basin and their geological evolution. Bulletin of the Research Council of Israel 10G(1–2):267–91.Google Scholar
Sonntag, C, Klitzsch, E, Lohnert, EP, El-Shazly, EM, Munnich, KO, Junghans, C, Thorweihe, U, Weistroffer, K, Swailem, FM. 1979. Palaeoclimatic information from deuterium and oxygen-18 in carbon-14–dated North Saharian groundwaters; groundwater formation in the past. In: Proceedings of the International Symposium on Isotope Hydrology, Neuherberg, I978. Volume 2. Vienna: IAEA. p 569–81.Google Scholar
Stuiver, M, Polach, HA. 1977. Discussion: reporting of 14C data. Radiocarbon 19(3):355–63.CrossRefGoogle Scholar
Sturchio, NC, Du, X, Purtschert, R, Lehmann, BE, Sultan, M, Patterson, LJ, Lu, ZT, Muller, P, Bigler, T, Bailey, K, O'Connor, TP, Young, L, Lorenzo, R, Becker, R, El Alfy, Z, El Kaliouby, B, Dawood, Y, Abdallah, AMA. 2004. One million year old groundwater in the Sahara revealed by krypton-81 and chlorine-36. Geophysical Research Letters 31:L05503, doi:10.1029/2003GL019234.CrossRefGoogle Scholar
Vengosh, A, Hening, S, Ganor, J, Bernhard, M, Weyhenmeyer, CE, Bullen, TD, Paytan, A. 2007. New isotopic evidence for the origin of groundwater from the Nubian Sandstone aquifer in the Negev, Israel. Applied Geochemistry 22:1052–73.CrossRefGoogle Scholar
Vogel, JC. 1970. 14C dating of groundwater. In: Isotope Hydrology. Vienna: IAEA. p 225–34.Google Scholar
Yechieli, Y. 1987. The geology of the northern Arava Valley and Mahmal anticline, Hazeva region , The Hebrew University. Israel Geological Survey, Report GSI/30/87, 94 p. In Hebrew with English abstract.Google Scholar
Yechieli, Y, Starinsky, A, Rosenthal, E. 1992. Evolution of brackish groundwater in a typical arid region: northern Arava Rift Valley, southern Israel. Applied Geochemistry 7(4):361–74.CrossRefGoogle Scholar
Yechieli, Y, Bein, A, Halicz, L. 1997. Geochemistry of groundwater in the central Arava Valley. Israel Geological Survey, Report GSI/30/96. 10 p In Hebrew.Google Scholar
Yechieli, Y, Bein, A, Burg, A, Yarom, I. 2001. The impact of flash flood interception on the Arava shallow groundwater: characterization of the interrelationships in the natural and disturbed systems. Israel Geological Survey, Report TR-GSI/11/2001. 15 p In Hebrew.Google Scholar