Hydrogeological Survey, Radiometric Analysis and Field Parametric Measurements: A Combined Tool for the Study of Porous Aquifers

The use of isotopic geochemistry for hydrogeological studies is growing internationally. methodologies on survey data, integrated with the natural tracers, helpful when defining model aquifer. In particular, radioisotope concentration measurements as tracers and detection temperature, redox potential dissolved oxygen in groundwater field provide information underground water circulation, which useful identifying recharge areas drainage. Variations these parameters aquifer allow about its hydrodynamics to be obtained. application this method a sample area showed how uranium radon concentrations, vary different sectors aquifer, depending mobility. This information, results static levels, distinguished drainage preferential directions terms flow allowed mobility various presented paper was tested larger study southern sector shallow S. Eufemia Lamezia plain (Calabria, Italy).