Application of multi-isotope data (O, D, C and S) to quantify redox processes in urban groundwater

The different recharge sources and their mixing ratios were investigated in water samples from an urban aquifer. Two distinct zones from Barcelona city were compared: (1) Poble Sec and (2) Besos River Delta, which are located in a densely populated area with a strong industrial impact. In this study 106 water samples were collected from July 2007 to May 2010 for hydrochemical and isotopic characterisation. The application of environmental isotopes coupled with hydrochemistry provided the necessary information to isotopically quantify groundwater recharge sources and evaluate the occurrence of redox processes. In the Besos River Delta, a decrease in dissolved SO42- concentration and an increase in delta S-34(SO4) and delta O-18(SO4) values were observed in groundwater samples, both indicating SO42- reduction. Moreover, other chemical indicators supported a reducing environment, such as low or null levels of dissolved O-2 and NO3-, the presence of NH4+ and an increase in dissolved Fe and As. The reducing conditions were probably induced by the organic C dissolved in water infiltrating from the River Besos. In Poble Sec, the relationship between delta S-34(SO4) and delta O-18(SO4) showed a strong influence of sewage water infiltration into the aquifer. However, the aquifer is oxic and there is no influence of SO42- reduction. (c) 2013 Elsevier Ltd. All rights reserved.