•Tracer-tests are performed in a karstic network and breakthrough curves are modelled.•Transient storage is a major process in flooded areas, but not in river stretches.•Apparition of retardation depends greatly on the system geometry.•OTIS can simulate transport in karstic network and help to understand hydrodynamic.
Journal of Hydrology – Elsevier
Published: Mar 1, 2016
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