GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 3.2 GNGTS 2024 approach to monitor the salt wedge phenomenon during the warmer periods with increased drought but also on a daily basis due to the infuence of tdes. Fig.1: The map shows the pathway of the acquisitons. The acquisitons carried out in two diferent tmes of the day along part of Po di Goro (15 Km). During the morning (8.00 AM) when there was low tde and during the afernoon (13.00 PM) when there was a peak of maximum tde. The two paths have an overlap of about 1.5 Km. The diferent EMs were performed using diferent frequency of Profler. It was located on a infatable boat pulled by a kayak. References [1] Crestani E., Camporese M., Belluco E., Bouchedda A., Gloaguen E., Salandin P.; 2022: Large- Scale Physical Modeling of Salt-Water Intrusion. Water. htps://doi.org/10.3390/w14081183 [2] Umberto S. Corbau C.; 2009: A review of the Delta Po evoluton (Italy) related to climatc change s and human impac t s . Geomo r pho l ogy. htp : / /dx . do i . o rg / 10 . 1016/ j.geomorph.2008.11.004 [3] Boldrin P., Bondesan A., Droghet F, Ferrari E., Fornasari G., Neri F., Rizzo E.; 2023: DC and FDEM monitoring of the salt wedge on the Po di Goro river (Italy). At del 41° Convegno Nazionale del GNGTS. Corresponding author: bldpla4@unife.it , enzo.rizzo@unife.it