2009
DOI: 10.1016/j.crci.2008.11.004
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Sediment dating and groundwater residence time in the lower basin of the Var river by radiochemistry and γ-ray spectrometry methods

Abstract: A method for dating sediment core layers from the Var riverbed was developed. The signature of the Chernobyl event was detected in the layer sequence by g-ray spectrometry of 137 Cs and correlated to the flow amplitude from the historical records.The residence time of groundwater in the aquifer of the lower Var valley was determined by measuring activity ratios of radium isotopes in well water samples. To cite this article: V.

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