2003 Seattle Annual Meeting (November 2–5, 2003)

Paper No. 7
Presentation Time: 3:00 PM


STURCHIO, N.C.1, LU, Z.-T.2, PURTSCHERT, R.3, LEHMANN, B.E.4, SULTAN, M.5, DU, X.2, MUELLER, P.2, LORENZO, R.3, EL ALFY, Z.6 and EL KALIOUBY, B.7, (1)Earth and Environmental Sciences, Univ of Illinois at Chicago, 845 West Taylor St., MC-186, Chicago, IL 60607, (2)Physics Division, Argonne National Lab, 9700 South Cass Ave., PHY-203, Argonne, IL 60439, (3)Physics Institute, Univ of Bern, Sidlerstrasse 5, Bern, 3012, Switzerland, (4)Physics Institute, Univ of Bern, Sidlerstrasse 5, Bern, 3012, (5)Geology Department, Univ at Buffalo, 876 NSC, Buffalo, NY 14260, (6)Remote Sensing Laboratory, Egyptian Geol Survey and Mining Authority, Abbassia, Egypt, (7)Geology Department, Ain Shams Univ, Cairo, Egypt, sturchio@uic.edu

Beneath a 2 ´ 106 km2 area of the hyperarid Western Desert of Egypt and adjacent portions of eastern Libya, northeastern Chad, and northwestern Sudan lies an immense reservoir of fresh water in the Nubian Aquifer system.  This is a fossil groundwater reservoir with recharge that is minor compared to natural discharge and pumping for agricultural and industrial use.  Its water volume (~5 ´ 104 km3) is equivalent to about 500 years of Nile River discharge.  Although there have been a large number of radiocarbon analyses of Nubian aquifer water, indicating that some samples have ages (mean residence times) ≥ 5´104 years, and hydrologic models indicate ages up to 106 a, there has not yet been a definitive measurement of the age of the Nubian aquifer water and its variation along flowpath.   An outstanding question is whether recharge has been restricted mainly to the highlands in the southwest, or has been distributed regionally, during humid climate periods during the Quaternary; each of these recharge modes results in a different distribution of natural radioactive tracers within the aquifer.  We address this question using measurements of 81Kr, a new tool for groundwater dating.  81Kr has been recognized as an ideal tracer for groundwater dating in the 50,000–1,000,000-year range, but its low abundance (~103 atoms/L H2O) has made routine measurement nearly intractable.  We have applied a new analytical method, atom-trap trace analysis (ATTA) (Chen et al., 1999, Science), to measure the 81Kr abundance in samples of Nubian aquifer groundwater.  Six groundwater samples were taken from wells screened in the deeper portion of the aquifer (600–1200 m) in major oasis areas of the Western Desert (Baris, Kharga, Dakhla, Farafra, Bahariya).  Dissolved gas was bulk-stripped from water in the field.  The Kr was separated from the bulk gas and analyzed by low-level counting (LLC) for 85Kr at Bern.  It was then spiked with 85Kr, analyzed again by LLC, and shipped to Argonne for analysis of 81Kr/85Kr by ATTA.  81Kr ages of the water samples, obtained by comparing their 81Kr/Kr ratios with that of modern air, range from ~200 to ~1,000 ka.  Ages increase with distance along the flowpath and correlate well with 36Cl/Cl ratios.