Abstract
Piana di Palermo is characterized by the presence of two different aquifers: one shallow, constituted by calcarenites and the other deep in fractured carbonates. The calcarenitic aquifer presents a low potential compared to the carbonatic aquifer. The chemistry of the water in both aquifers reflects water-rock interaction, seawater intrusion, ionic exchange etc. The application of SINTACS method showed that about 80% of the study area can be classified as of high to very high vulnerability.
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Cusimano, G., De Maio, M., Gatto, L., Hauser, S., & Pisciotta, A. (2004). Application of SINTACS method to the aquifers of Piana di Palermo, Sicily, Italy. Geofisica Internacional, 43(4), 661–670. https://doi.org/10.22201/igeof.00167169p.2004.43.4.850
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