Abstract
Changes in the uranium isotopic activity ratio and uranium content are correlated to changes in the calcium and sulphate content in waters from wells in various locations in the Cenomanian aquifer in the Beersheva region. These changes are related to an isotopically non-selective leaching of uranium from the overlying uranium- and sulphate-enriched Senonian rocks as the waters flow. A flow pattern can therefore be produced by plotting these systematic changes on a regional map.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
