CONICET | Buscador de Institutos y Recursos Humanos

The hydrological events that occur in floodplains are largely defined by precipitation and runoff inputs interacting with their geomorphological characteristics. In the middle Paraná River, hydrological events have traditionally been studied using water level time series and topographic charts or satellite images of certain floodplain sectors, using the same scale throughout the studyarea. Different zones of the floodplain were integrated using fractal dimension to better understandhydrological processes. Fractal dimension is a useful tool used to characterize the geomorphological complexity of river networks in watersheds. The box-counting method was applied in the middle Paraná River floodplain. The result showed that as water levels increase, fractal dimension decreases, thereby indicating the direct relation with the hydrological attributes of the floodplain (e.g., duration, magnitude, recurrence of the flood event and connectivity). This relation constitutes the basis of a new approach analysis of hydrological events and their effect on the middle Paraná River floodplain. This research provides fundamental information obtained from two hydrological stages and different spatial scales which may complement the method designed to accurately understand the hydrogeomorphological processes that operate e in the Paraná River floodplain. Indeed, it provides a simple parameter that can be used to evaluate the role that each floodplain section plays in attenuating the hydrograph recorded at each gauge analyzed along the river. This information will be useful in the implementation of management policies directed to the mitigation of future hydrological threats generated by alterations in the hydrological regime due to hydroclimatic variations or watershed alterations. The results further strengthen the basis for an integral sustainable planning of the main channel of the Paraná River, its floodplain, and the resources provided by this ecosystem.

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