A flow pattern deduced from uranium disequilibrium studies for the Cenomanian carbonate aquifer of the Beersheva region, Israel

J. Kronfeld; E. Gradsztajn; A. Yaniv

doi:10.1016/0022-1694(79)90137-9

A flow pattern deduced from uranium disequilibrium studies for the Cenomanian carbonate aquifer of the Beersheva region, Israel

J. Kronfeld^*, E. Gradsztajn, A. Yaniv

^*Corresponding author for this work

Department of Geophysics

Research output: Contribution to journal › Article › peer-review

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.

Original language	English
Pages (from-to)	305-310
Number of pages	6
Journal	Journal of Hydrology
Volume	44
Issue number	3-4
DOIs	https://doi.org/10.1016/0022-1694(79)90137-9
State	Published - Dec 1979

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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.",

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N2 - 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.

AB - 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.

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A flow pattern deduced from uranium disequilibrium studies for the Cenomanian carbonate aquifer of the Beersheva region, Israel

Abstract

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