H13J-1722
Aquifer recharge from infiltration basins in a highly urbanized area: the river Po Plain (Italy)

Monday, 14 December 2015
Poster Hall (Moscone South)
Marco Masetti1, Son V Nghiem2, Alessandro Sorichetta3, Stefania Stevenazzi1, Emanuele Santi Santi4, Simone Pettinato4, Marianna Bonfanti1 and Daniele Pedretti5, (1)Università degli Studi di Milano, Dipartimento di Scienze della Terra “Ardito Desio”, Milan, Italy, (2)Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United States, (3)University of Southampton, Southampton, United Kingdom, (4)CNR Institute of Applied Physics, Sesto Fiorentino, Italy, (5)University of British Columbia, Vancouver, BC, Canada
Abstract:
Due to the extensive urbanization in the Po Plain in northern Italy, rivers need to be managed to alleviate flooding problems while maintaining an appropriate aquifer recharge under an increasing percentage of impermeable surfaces.
During the PO PLain Experiment field campaign in July 2015 (POPLEX 2015), both active and under-construction infiltration basins have been surveyed and analyzed to identify appropriate satellite observations that can be integrated to ground based monitoring techniques. A key strategy is to have continuous data time series on water presence and level within the basin, for which ground based monitoring can be costly and difficult to be obtained consistently.
One of the major and old infiltration basin in the central Po Plain has been considered as pilot area. The basin is active from 2003 with ground based monitoring available since 2009 and supporting the development of a calibrated unsaturated-saturated two-dimensional numerical model simulating the infiltration dynamics through the basin.
A procedure to use satellite data to detect surface water change is under development based on satellite radar backscatter data with an appropriate incidence angle and polarization combination. An advantage of satellite radar is that it can observe surface water regardless of cloud cover, which can be persistent during rainy seasons. Then, the surface water change is correlated to the reservoir water stage to determine water storage in the basin together with integrated ground data and to give quantitative estimates of variations in the local water cycle.
We evaluated the evolution of the infiltration rate, to obtain useful insights about the general recharge behavior of basins that can be used for informed design and maintenance. Results clearly show when the basin becomes progressively clogged by biofilms that can reduce the infiltration capacity of the basin by as much as 50 times compared to when it properly works under clean conditions.