Uranium isotopes in groundwater from the continental intercalaire aquifer in Algerian Tunisian Sahara (Northern Africa)

Chkir, N; Guendouz, A; Zouari, K; Hadj Ammar, F; Moulla, AS

HERO ID

555769

Reference Type

Journal Article

Year

2009

Language

English

PMID

19559509

HERO ID 555769
In Press No
Year 2009
Title Uranium isotopes in groundwater from the continental intercalaire aquifer in Algerian Tunisian Sahara (Northern Africa)
Authors Chkir, N; Guendouz, A; Zouari, K; Hadj Ammar, F; Moulla, AS
Journal Journal of Environmental Radioactivity
Volume 100
Issue 8
Page Numbers 649-656
Abstract The disequilibrium between 234U and 238U is commonly used as a tracer of groundwater flow. This paper aims to identify uranium contents and uranium isotopic disequilibria variation in groundwater sampled from deep Continental Intercalaire aquifer (southern Algeria and Tunisia). Large variations in both U contents (0.006-3.39 ppb) and 234U/238U activity ratios (0.4-15.38) are observed. We conduct a first assessment in order to verify whether the results of our investigation support and complete previous hydrogeological and isotopic studies. The dissolved U content and 234U/238U activity ratio data were plotted on a two-dimensional diagram that was successfully utilized on sharing the CI aquifer into different compartments submitted to different oxidising/reducing conditions and leads also to distinguished two preferential flow paths in the Nefzaoua/Chott Fejej discharge area. Uranium isotopes disequilibrium indicate that ranium chemistry is mainly controlled by water-rock interaction enhanced by long residence time recognised for this aquifer.
Doi 10.1016/j.jenvrad.2009.05.009
Pmid 19559509
Is Certified Translation No
Dupe Override No
Is Public Yes
Language Text English
Keyword Uranium; Disequilibrium; Activity ratio; 234U/238U; Solubility; Mobility
Is Qa No