Coastal hydrogeological system of Mar Piccolo (Taranto, Italy)

• Published in: Environmental science and pollution research international 2016-07, Vol.23 (13), p.12502-12514
• Main Authors: Zuffianò, L. E., Basso, A., Casarano, D., Dragone, V., Limoni, P. P., Romanazzi, A., Santaloia, F., Polemio, M.
• Format: Article
• Language: English
• Subjects: Anthropogenic factors; Aquatic Pollution; Aquifers; Atmospheric Protection/Air Quality Control/Air Pollution; Coasts; Contaminated sediments; Earth and Environmental Science; Ecotoxicology; Environment; Environmental Chemistry; Environmental Health; Environmental Monitoring; Environmental science; Equilibrium; Geology; Groundwater - analysis; Groundwater discharge; Hydrogeology; Hydrology; Integrated environmental characterization of the contaminated marine coastal area of Taranto; Ionian Sea (southern Italy) - the RITMARE Project; Italy; Karstic environments; Models, Theoretical; Natural Springs - analysis; Permeability; Pollution; Pumping tests; Salinity; Seawater; Seawater - analysis; Sediment pollution; Sediments; Sewage disposal; Ships; Studies; Travel time; Waste Water Technology; Water inflow; Water Management; Water pollution; Water Pollution Control; Water quality; Water springs
• ISSN: 0944-1344; 1614-7499
• DOI: 10.1007/s11356-015-4932-6

The Mar Piccolo basin is an internal sea basin located along the Ionian coast (Southern Italy), and it is surrounded primarily by fractured carbonate karstic environment. Because of the karstic features, the main continental water inflow is from groundwater discharge. The Mar Piccolo basin represents a peculiar and sensitive environment and a social emergency because of sea water and sediment pollution. This pollution appears to be caused by the overlapping effects of dangerous anthropogenic activities, including heavy industries and commercial and navy dockyards. The paper aims to define the contribution of subaerial and submarine coastal springs to the hydrological dynamic equilibrium of this internal sea basin. A general approach was defined, including a hydrogeological basin border assessment to detect inflowing springs, detailed geological and hydrogeological conceptualisation, in situ submarine and subaerial spring measurements, and flow numerical modelling. Multiple sources of data were obtained to define a relevant geodatabase, and it contained information on approximately 2000 wells, located in the study area (1600 km 2 ). The conceptualisation of the hydrogeological basin, which is 978 km 2 wide, was supported by a 3D geological model that interpolated 716 stratigraphic logs. The variability in hydraulic conductivity was determined using hundreds of pumping tests. Five surveys were performed to acquire hydro-geochemical data and spring flow-yield measurements; the isotope groundwater age was assessed and used for model validation. The mean annual volume exchanged by the hydrogeological basin was assessed equal to 106.93 10 6  m 3 . The numerical modelling permitted an assessment of the mean monthly yield of each spring outflow (surveyed or not), travel time, and main path flow.