4.7 Article

Characterisation of the natural attenuation of chromium contamination in the presence of nitrate using isotopic methods. A case study from the Matanza-Riachuelo River basin, Argentina

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 699, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2019.134331

Keywords

Cr(VI) reduction; Denitrification; Isotopic fractionation; Groundwater; Matanza-Riachuelo basin

Funding

  1. project PACE-ISOTEC - Spanish Government [CGL2017-87216-C4-1-R]
  2. AEI/FEDER from the UE
  3. project MAG from the Catalan Government [2017 SGR 1733]
  4. Instituto de Hidrologia de Llanura Dr. Eduardo J. Usunoff (IHLLA)
  5. IDAEA-CSIC as part of the programme EMHE Enhancing Mobility between LatinAmerican and Caribbean countries and Europe

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The groundwater contamination by hexavalent chromium (Cr(VI)) in a site of the Matanza-Riachuelo River basin (MRB), Argentina, has been evaluated by determining the processes that control the natural mobility and attenuation of Cr(VI) in the presence of high nitrate (NO3) contents. The groundwater Cr(VI) concentrations ranged between 1.9E-5 mM and 0.04 mM, while the NO3 concentrations ranged between 0.5 mM and 3.9 mM. In order to evaluate the natural attenuation of Cr(VI) and NO3 in the MRB groundwater, Cr and N isotopes were measured in these contaminants. In addition, laboratory batch experiments were performed to determine the isotope fractionation (epsilon) during the reduction of Cr(VI) under denitrifying conditions. While the Cr(VI) reduction rate is not affected by the presence of NO3, the NO3 attenuation is slower in the presence of Cr(VI). Nevertheless, no significant differences on E values were observed when testing the absence or presence of each contaminant. The epsilon Cr-53 determined in the batch experiments describe a two- stage trend, in which Stage I is characterized by epsilon Cr-53 similar to-1.8 parts per thousand, and Stage II by epsilon Cr-53 similar to -0.9 parts per thousand. The respective epsilon N-15(NO3) obtained is -23.9 parts per thousand, whereas epsilon O-18(NO3) amount to -25.7 parts per thousand. Using these E values and a Rayleigh fractionation model we estimate that an average of 60% of the original Cr(VI) is removed from the groundwater of the contaminated site. Moreover, the average degree of NO3 attenuation by denitrification is found to be about 20%. This study provides valuable information about the dynamics of a complex system that can serve as a basis for efficient management of contaminated groundwater in the most populated and industrialized basin of Argentina. (C) 2019 Elsevier B.V. All rights reserved.

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