Radiocarbon in Seawater Intruding into the Israeli Mediterranean Coastal Aquifer
Issue Date
2001-01-01Keywords
water resourceswater rock interaction
salinization
salt water intrusion
hydrogen
tritium
residence time
hydrochemistry
tracers
Israel
coastal environment
sea water
ground water
aquifers
pollution
Middle East
isotope ratios
Mediterranean region
Asia
C 14
carbon
isotopes
radioactive isotopes
C 13 C 12
stable isotopes
geochemistry
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Yechieli, Y., Sivan, O., Lazar, B., Vengosh, A., Ronen, D., & Herut, B. (2001). Radiocarbon in seawater intruding into the Israeli Mediterranean coastal aquifer. Radiocarbon, 43(2B), 773-781.Journal
RadiocarbonDescription
From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.Additional Links
http://radiocarbon.webhost.uits.arizona.edu/Abstract
Saline groundwaters from the Israeli coastal aquifer were analyzed for their radiocarbon and tritium content to assess the rate of seawater penetration. The low 14C values (28-88 pMC versus 100-117 pMC in seawater) imply an apparent non-recent seawater source, or water-rock interactions along the penetration route. The latter process is supported by measurable tritium values at some locations, which imply a relatively rapid rate of seawater intrusion. In other locations, low tritium values (<2 T.U.) indicate that recent seawater (<50 yr) did not penetrate inland. The low delta-13C values in saline groundwater (average of -5.3 per mil versus 0 per mil in seawater) indicate that the dissolved carbon pool is comprised of a significant fraction of organic carbon. A linear negative correlation between delta-13C and 14C implies that this organic source is old (low 14C values).Type
Proceedingstext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200041448
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