Saltwater contamination in the lowlying coastland of the Venice Lagoon, Italy
Author(s)
Type
Conference paper
Language
English
Obiettivo Specifico
7A. Geofisica di esplorazione
Status
Published
Date Issued
June 6, 2014
Conference Location
Husum, Germany
Abstract
TIle southem portion ofthe Venice coastland includes a very precarious environment. Due to an elevation down to 4 m below msl, ilie Venice Lagoon atld Adriatic Sea proximity, and the encroachment of seawater from ilie mouth of the river network up to 20 km inland, salt contamination of land atld groundwater is a severe problem that is seriously affecting the farmland productivity. An interdisciplinary multi-scale research is ongoing with the aim of understanding ilie contamination process, quantifying the effect of ilie saltwater intrusion of the crop production, and proposing possible mitigation strategies. A 21-ha representative basin has been selected and deeply monitored from the hydrogeological atld agricultural points of view. It has been clearly outlined that in the upper 5 to 10 m mainly the lowpermeable soils are contaminated by salt. Conversely, fresh to brackish waters are located in
the sandy elongated paleo-channels. This is likely due to the origin of the area which was a salty marshlatld since one century ago. The freshwater supplied for almost 100 years by the rainfall and leakage from the river and chatlnel beds has been able to reduce ilie salt concentration only in the highly permeable deposits.
the sandy elongated paleo-channels. This is likely due to the origin of the area which was a salty marshlatld since one century ago. The freshwater supplied for almost 100 years by the rainfall and leakage from the river and chatlnel beds has been able to reduce ilie salt concentration only in the highly permeable deposits.
References
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Carbognin, 1., P. Teatini, A. Tomasin and 1. Tosi. 2010. Global change and relative sea level rise at Venice: what impact in tenn of flooding. Climate Dynamics 35 : 1039-1047.
Manoli, G., S. Bonetti, E. Scudiero, P. Teatini, P. J. Binning, F. Morari, M. Putti, and M. Marani. 2013. Monitoring and modeling fannland productivity along the Venice coastland, Italy. Procedia Environmental Sciences 19: 361-368.
Rizzetto, F., 1. Tosi, 1. Carbognin, M. Bonardi and P. Teatini. 2003. Geomorphological setting and related hydrogeological implications of the coastal plain south of the Venice Lagoon (Italy). In: Hydrology of tile Mediterranean and Semiarid Regions, ed E. Servat et aI., 463-470, IARS Publ. n.278.
Scudiero, E., Deiana, R., Teatini, P., Cassiani, G., Morari, F., 2011. Constrained optimization of spatial sampling in salt contaminated coastal fannland using EM! and continuous simulated annealing. Procedia Enviromnental Sciences 7: 234-239.
Scudiero, E., P. Teatini, D. 1. Corwin, A. Berti, and F. Morari. 2013. Delineation of site-specific management units in a saline region at the Venice Lagoon margin, Italy, using soil reflectance and apparent electrical conductivity. Computers and Electronics in Agriculture 99: 54-64.
Teatini, P., 1. Tos~ A, Viezzoli, 1. Baradello, M. Zecchin, and S. Silvestri. 2011. Understanding the hydrogeology ofthe Venice Lagoon subsurface with airborne electromagnetics. Jomnalof Hydrology 411: 342-354.
Tosi, 1., P. Teatini, 1. Carbognin, and G. Brancolini. 2009.Using high resolution data to reveal deptll-dependent mechanisms that drive land subsidence: The Venice coast, Italy. Tectonophysics 474: 271-284.
Viezzoli, A., A. V. Christiansen, E. Auken, and K. Smensen. 2008. Quasi-3D modeling of airborne TEM data by spatially constrained inversion. Geophysics 73: FI05- Fl13.
Carbognin, 1., P. Teatini, A. Tomasin and 1. Tosi. 2010. Global change and relative sea level rise at Venice: what impact in tenn of flooding. Climate Dynamics 35 : 1039-1047.
Manoli, G., S. Bonetti, E. Scudiero, P. Teatini, P. J. Binning, F. Morari, M. Putti, and M. Marani. 2013. Monitoring and modeling fannland productivity along the Venice coastland, Italy. Procedia Environmental Sciences 19: 361-368.
Rizzetto, F., 1. Tosi, 1. Carbognin, M. Bonardi and P. Teatini. 2003. Geomorphological setting and related hydrogeological implications of the coastal plain south of the Venice Lagoon (Italy). In: Hydrology of tile Mediterranean and Semiarid Regions, ed E. Servat et aI., 463-470, IARS Publ. n.278.
Scudiero, E., Deiana, R., Teatini, P., Cassiani, G., Morari, F., 2011. Constrained optimization of spatial sampling in salt contaminated coastal fannland using EM! and continuous simulated annealing. Procedia Enviromnental Sciences 7: 234-239.
Scudiero, E., P. Teatini, D. 1. Corwin, A. Berti, and F. Morari. 2013. Delineation of site-specific management units in a saline region at the Venice Lagoon margin, Italy, using soil reflectance and apparent electrical conductivity. Computers and Electronics in Agriculture 99: 54-64.
Teatini, P., 1. Tos~ A, Viezzoli, 1. Baradello, M. Zecchin, and S. Silvestri. 2011. Understanding the hydrogeology ofthe Venice Lagoon subsurface with airborne electromagnetics. Jomnalof Hydrology 411: 342-354.
Tosi, 1., P. Teatini, 1. Carbognin, and G. Brancolini. 2009.Using high resolution data to reveal deptll-dependent mechanisms that drive land subsidence: The Venice coast, Italy. Tectonophysics 474: 271-284.
Viezzoli, A., A. V. Christiansen, E. Auken, and K. Smensen. 2008. Quasi-3D modeling of airborne TEM data by spatially constrained inversion. Geophysics 73: FI05- Fl13.
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