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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10274
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dc.contributor.authorallZuffianò, L. E.en
dc.contributor.authorallBasso, A.en
dc.contributor.authorallCasarano, D.en
dc.contributor.authorallDragone, V.en
dc.contributor.authorallLimoni, P. P.en
dc.contributor.authorallRomanazzi, A.en
dc.contributor.authorallSantaloia, F.en
dc.contributor.authorallPolemio, M.en
dc.date.accessioned2016-03-07T15:44:20Zen
dc.date.available2016-03-07T15:44:20Zen
dc.date.issued2015-07-24en
dc.identifier.urihttp://hdl.handle.net/2122/10274en
dc.description.abstractThe 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 sediments 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 2,000 wells, located in the study area (1,600 km2). The conceptualisation of the hydrogeological basin, which is 978 km2 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 106.93 106 m3. The numerical modelling permitted an assessment of the mean monthly yield of each spring outflow (surveyed or not), travel time, and main path flow.en
dc.language.isoEnglishen
dc.publisher.nameSpringer Berlin Heidelbergen
dc.relation.ispartofEnvironmental Science and Pollution Researchen
dc.subjectCoastal water qualityen
dc.subjectKarstic coastal aquiferen
dc.subjectSpring yielden
dc.subjectGroundwater modellingen
dc.subjectMediterranean Seaen
dc.subjectItalyen
dc.subjectSubaerial and submarine springsen
dc.subjectApuliaen
dc.titleCoastal hydrogeological system of Mar Piccolo (Taranto, Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV03. Hydrosphere::03.03. Physical::03.03.01. Air/water/earth interactionsen
dc.identifier.doi10.1007/s11356-015-4932-6en
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PCBs) in sediments from the Mar Piccolo in Taranto (Ionian Sea. Southern Italy). Marine Pollution Bulletin 55: 451–458 Castany G (1982) Principes et méthodes de l'hydrogéologie. Dunod, Paris Cerruti A (1938) Le sorgenti sottomarine (Citri) del Mar Grande e Mar Piccolo di Taranto. Annali Istituto Superiore Navale Di Napoli, Napoli 7 Ciaranfi N, Pieri P, Ricchetti G (1988) Note alla carta geologica delle Murge e del Salento (Puglia centromeridionale). Mem. Soc. Geol. It. 41: 449-460 Civita M (2005) Idrogeologia applicata ed ambientale. Casa Editrice Ambrosiana, Milan CNR (1987) Neotectonic Map of ltaly. Quaderni della ricerca scientifica, Firenze, 114, 4 COST (2005) Cost Action 621 Groundwater management of coastal karst aquifers. European Commission, Directorate-General for Research. Report EUR 21366 Cotecchia V, Grassi D, Polemio M (2005) Carbonate aquifers in Apulia and seawater intrusion. Giornale di Geologia Applicata 1: 219-231 Cotecchia V, Lollino G, Pagliarulo R, Stefanon A, Tadolini T, Trizzino R (1989) Studi e controlli in situ per la captazione della sorgente sottomarina Galeso. Mar Piccolo di Taranto. Conv. Int. Geoing. Suolosottosuolo. Torino. 27-30 Settembre 1989. 475-484 Doherty J (2002) PEST Model-independent parameter estimation. Watermark Numerical Computing Fetter CW (2001) Applied Hydrogeology. 4th Edition. New Jersey. Prentice Hall. Hanshaw BB, Back W, Deike RG (1971) A geochemical hypothesis for dolomitization by groundwater. Economic Geology 66: 710 – 724 Langevin CD (2003) Simulation of Submarine Ground Water Discharge to a Marine Estuary: Biscayne Bay: Florida. Ground Water 41(6): 758-771 McDonald MG, Harbaugh AW (1988) A modular three-dimensional finite-difference ground-water flow model. Techniques of Water-Resources Investigations of the United States Geological Survey. 6 Panetta P, Dell’Angelo B (1975) I citri del Mar Piccolo di Taranto. Conchiglie. 11 3-4: 65-86 Pearson F.J (1965) Use of C-13/C-12 ratios to correct radiocarbon ages of material initially diluted by limestone. Proceedings of the 6th International Conference on Radiocarbon and Tritium Dating: 357 366 Polemio M (1998) Le calamità idrogeologiche dell'inverno 1995-96 nel territorio tarantino. In: Luino F (ed) International Conference "Prevention of hydrogeological Hazards: the role of scientific research". Alba. CNR IRPI. 2: 63-73 Polemio M, Romanazzi L (1999) Numerical simulation of ground water protection works for industrial waste dump. Bulletin of Engineering Geology and the Environment 57: 253-261. doi: 10.1007/s100640050042 Polemio M, Limoni PP (2001) L'evoluzione dell'inquinamento salino delle acque sotterranee della Murgia e del Salento: Memorie della Società Geologica Italiana 56: 327-331 Polemio M, Limoni PP (2006) Groundwater pollution and risks for the coastal environment (southeastern Italy). In Predictions in Ungauged Basins: Promise and Progress (ed) Sivapalan M, Wagener T, Uhlenbrook S, Zehe E, Lakshmi V, Liang X, Tachikawa Y, and Kumar P. IAHS Publications 303: 477-486 Polemio M, Casarano D (2008) Climate change, drought and groundwater availability in southern Italy: Geological Society Special Publication 288: 39-51 Polemio M, Dragone V, Limoni PP (2008) Salt contamination of Apulian aquifers: spatial and time trend. 19th SWIM & 3rd SWICA jointed meeting: Cagliari. 115-121 Polemio M, Dragone V, Limoni PP (2009) Monitoring and methods to analyse the groundwater quality degradation risk in coastal karstic aquifers (Apulia. Southern Italy): Environmental Earth Sciences (formerly Environmental Geology) 58: 299-312. doi: 10.1007/s00254-008-1582-8 Pollock DW (1989) Documentation of computer programs to compute and display pathlines using results from the U.S. Geological Survey modular three-dimensional finite-difference ground-water flow model. Open File Report. 89-381 Romanazzi A, Polemio M (2013) Modelling of coastal karst aquifers for management support: A case study of Salento (Apulia. Italy). Source of the Document Italian Journal of Engineering Geology and Environment 1: 65-83 Sanford W, Langevin C, Polemio M, Povinec P (2007) Preface. In A new focus on groundwater-seawater interactions. IAHS Publications (ed)Sanford W, Langevin C, Polemio M, Povinec P. IAHS Press 312: V-VI. Scanlon BR, Mace RE, Barrett ME, Smith B (2003) Can we simulate regional groundwater flow in a karst system using equivalent porous media models? Case study. Barton Springs Edwards aquifer. USA. Journal of Hydrology 276 (1-4): 137-158. Servizio Idrografico (1953) Le Sorgenti Italiane (Italian Springs. in Italian). Elenco e descrizione. Regione Pugliese. Pubbl. n.14 del Servizio Idrografico. l. Roma Stefanon A, Cotecchia F, (1969) Prime notizie sulle caratteristiche di efflusso e sulle modalità di investigazione delle sorgenti subacquee ai fini·di una loro captazione. La Ricerca Scientifica 58: 165-195 Tamers MA (1975) Validity of radiocarbon dates on ground water. Geophysical Surveys 2: 217-239 Todd DK, Mays LW, (2005) Groundwater Hydrology. John Wiley & Son inc, New York Uil H, Van Geer FC, Gehrels JC, Kloosterman FH (1999) State of the art on monitoring and assessment of groundwaters. UN/ECE Task Force on Monitoring & Assessment. Working Programme 1996/1999. Vol. 4. ISBN 9036952778 Delft, The Netherlands UNESCO (2004) Submarine groundwater discharge. IHP Groundwater series n. 5 Wigley TML (1973) The incongruent dissolution of dolomite. Geochimica et Cosmochimica Acta 37: 1397-1402 WMO (1994) Guide to hydrological practices. Fifth edition. WMO No.168en
dc.description.obiettivoSpecifico3A. Ambiente Marinoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextembargoed_20160725en
dc.contributor.authorZuffianò, L. E.en
dc.contributor.authorBasso, A.en
dc.contributor.authorCasarano, D.en
dc.contributor.authorDragone, V.en
dc.contributor.authorLimoni, P. P.en
dc.contributor.authorRomanazzi, A.en
dc.contributor.authorSantaloia, F.en
dc.contributor.authorPolemio, M.en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptCNR-IRPI-
crisitem.author.deptCNR-IRPI, Bari-
crisitem.author.deptCNR-IRPI-
crisitem.author.deptCNR-IRPI, Italy-
crisitem.author.deptCNR-IRPI, Italy-
crisitem.author.deptCNR-IRPI-
crisitem.classification.parent03. Hydrosphere-
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