Improving the management of nitrate pollution in water by the use of isotope monitoring: the δ15N, δ18O and δ11B triptych.

In spite of increasing efforts to reduce nitrogen inputs into ground water from intensive agriculture, nitrate (NO(3)) remains one of the major pollutants of drinking-water resources worldwide, with NO(3) levels approaching the defined limit of 50 mg l(-1) in an increasing number of water bodies. Determining the source(s) of contamination in water is an important first step for improving its quality by emission control. The Life ISONITRATE project aimed at showing the benefit of a multi-isotope approach (δ(15)N and δ(18)O of NO(3), and δ(11)B), in addition to conventional hydrogeological analysis, to track the origin of NO(3) contamination in water. Based on land use and local knowledge, four distinct cases were studied: (1) natural soil NO(3), (2) natural denitrification, (3) single source of NO(3) pollution and (4) multiple sources of NO(3) pollution. Our results show the added value of combining isotope information, compared to knowledge based on local authorities' experience, land use and the 'classical' chemical approach, by efficiently identifying the number and type of NO(3) source(s) for each watershed studied.