Abstract. After the nuclear weapons testing in the 1950s and 1960s,
the atmospheric tritium levels have almost returned to natural levels
(pre-1950 levels), which means that tritium is becoming more effective in
determining transit times in hydrological systems. It has also been
demonstrated that tritium is a non-reactive noble gas and in water is not
subject to chemical reactions, absorption, or dissolution/precipitation
processes, so it is conservative of the geochemical fingerprint of the
source. In addition, it is used as an effective tracer of water
contamination by landfill leachate, allowing to detect mixing percentages of
the leachate up to levels not achievable with normal chemical analyses (less
than 1 %). The purpose of the present work is to deepen the knowledge of
the hydrogeochemical characteristics of the aquifers in the pedemontana area
of the Venetian plain, and to formulate a conceptual framework of
underground water circulation, aimed at understanding phenomena of
contamination by toxic metals, harmful to human health. Tritium
concentration analyses were performed on selected samples of groundwater
collected in different wells in the south part of Treviso city to correlate
the young age of the water recharge. The abundance of young waters, in fact,
indicates a vulnerability of the aquifer to climate change with respect to
possible contributions of surface waters, in particular to prolonged drought
periods which could induce salinization dynamics.