Articles | Volume 20, issue 10
Hydrol. Earth Syst. Sci., 20, 4209–4221, 2016
Hydrol. Earth Syst. Sci., 20, 4209–4221, 2016

Research article 18 Oct 2016

Research article | 18 Oct 2016

Tracer test modeling for characterizing heterogeneity and local-scale residence time distribution in an artificial recharge site

Cristina Valhondo1,2,3, Lurdes Martínez-Landa2,3, Jesús Carrera1,3, Juan J. Hidalgo1,3, Isabel Tubau1,3, Katrien De Pourcq1,3, Alba Grau-Martínez4,5, and Carlos Ayora1,3 Cristina Valhondo et al.
  • 1Institute of Environmental Assessment and Water Research (IDAEA), CSIC, C/Jordi Girona 18, 08034 Barcelona, Spain
  • 2Department of Civil and Environmental Engineering, Universitat Politècnica de Catalunya (UPC), Jordi Girona 1-3, 08034 Barcelona, Spain
  • 3Associated Unit: Hydrogeology Group (UPC-CSIC)
  • 4Grup de Mineralogia Aplicada i Geoquímica de Fluids, Departament de Cristal.lografia, Mineralogia i Dipòsits Minerals, SIMGEO UB-CSIC, Facultad de Geologia, Universitat de Barcelona (UB), C/ Martí i Franquès, s/n 08028 Barcelona, Spain
  • 5Comunitat d'usuaris d'Aigües del delta del Llobregat, Av. de la Verge de Montserrat 133, 08820 El Prat del Llobregat, Barcelona, Spain

Abstract. Artificial recharge of aquifers is a technique for improving water quality and increasing groundwater resources. Understanding the fate of a potential contaminant requires knowledge of the residence time distribution (RTD) of the recharged water in the aquifer beneath. A simple way to obtain the RTDs is to perform a tracer test. We performed a pulse injection tracer test in an artificial recharge system through an infiltration basin to obtain the breakthrough curves, which directly yield the RTDs. The RTDs turned out to be very broad and we used a numerical model to interpret them, to characterize heterogeneity, and to extend the model to other flow conditions. The model comprised nine layers at the site scaled to emulate the layering of aquifer deposits. Two types of hypotheses were considered: homogeneous (all flow and transport parameters identical for every layer) and heterogeneous (diverse parameters for each layer). The parameters were calibrated against the head and concentration data in both model types, which were validated quite satisfactorily against 1,1,2-Trichloroethane and electrical conductivity data collected over a long period of time with highly varying flow conditions. We found that the broad RTDs can be attributed to the complex flow structure generated under the basin due to three-dimensionality and time fluctuations (the homogeneous model produced broad RTDs) and the heterogeneity of the media (the heterogeneous model yielded much better fits). We conclude that heterogeneity must be acknowledged to properly assess mixing and broad RTDs, which are required to explain the water quality improvement of artificial recharge basins.

Short summary
We performed and evaluated a pulse injection tracer test in an artificial recharge system to understand the fate of potential contaminants. A 2-D multilayer model (under homogeneous and heterogeneous medium hypothesis) was used to evaluate the measured breakthrough curves at six points. Both homogeneous and heterogeneous models reproduce the long tails observed. This implies that the shapes of the breakthrough curves are caused not only by heterogeneity, but also by the mean flow structure.