“…The possibility of quantifying both the origin and the secondary processes affecting N concentrations by means of a single tracer appears more limited however. Nitrogen cannot be considered conservative because it is biologically modified through nitrification and denitrification reactions, both during infiltration of the water and in the groundwater body, causing isotopic fractionation that modifies the б 15 N signatures of the dissolved N species (VOGEL et al, 1981;MARIOTTI et al, 1988;Böttcher et al, 1990;Smith et al, 1991;FEATS et al, 1998;ARAVENA AND ROBERTSON, 1998;PAUWELS et al, 2000, TORRENTÓ et al, 2010ZHANG et al, 2010). In some cases, the interference between the isotopic fractionation (linked to denitrification) and the mixing processes (from the combination of multiple nitrate sources) might hamper the identification of nitrate sources, since the associated fractionation processes can alter the isotope composition of dissolved nitrate.…”