Author/Authors :
Saccon، نويسنده , , P. and Leis، نويسنده , , A. and Marca، نويسنده , , A. and Kaiser، نويسنده , , J. and Campisi، نويسنده , , L. and Bِttcher، نويسنده , , M.E. and Savarino، نويسنده , , J. and Escher، نويسنده , , Matty P. and Eisenhauer، نويسنده , , A. and Erbland، نويسنده , , J.، نويسنده ,
Abstract :
A multi-isotope approach has been used in the Marano lagoon (NE Italy) and parts of its catchment area to identify causes of increased NO 3 - pollution. The hydrogeochemical features of different water types and potential sources of NO 3 - were characterized using the isotopic composition of NO 3 - (δ15N, δ18O, and Δ17O) and other source-related species such as B (δ11B), water (δ2H and δ18O) and SO 4 2 - (δ34S and δ18O). Water samples from the lagoon, its tributary rivers, the groundwater up-welling line, groundwater, sewer pipes, and open sea water have been collected at quarterly intervals in the years 2009–2010. The results indicate that the NO 3 - load in the lagoon was not only derived from agricultural activities but also from other sources such as urban waste water, in situ nitrification and atmospheric deposition. The δ34S signature in the lagoon clearly denotes the largely prevailing origin of aqueous SO 4 2 - from seawater, and practically points to the absence of any appreciable redox process involving S species in the lagoon. It also supports the existence of a connection between the lagoon and the nearby Tagliamento river.