We use environmental isotope and chemical tracer tools to understand complex groundwater flow and evolution processes including nitrate contamination. Examples where these environmental tracers, in addition to conventional hydrologic investigations, have significantly improved the understanding of groundwater processes include:
This summary aims to show where the combination of the age tracers, water and nitrate stable isotopes, gas tracers, nutrients and major ions enabled us to understand recharge source and rate, interaction between surface and groundwater, lag times, discharge pathways, and denitrification processes, in order to enable better management of groundwater problems and resources.