Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/8925
DC Field | Value | Language |
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dc.contributor.authorall | Polemio, M.; CNR-IRPI, Bari | en |
dc.contributor.authorall | Limoni, P.P.; CNR-IRPI, Bari | en |
dc.contributor.authorall | Mitolo, D.; CNR-IRPI, Bari | en |
dc.contributor.authorall | Santaloia, F. | en |
dc.contributor.editorall | Bocanegra, E. M. | en |
dc.contributor.editorall | Martinez, D. | en |
dc.contributor.editorall | Massone, H. E. | en |
dc.date.accessioned | 2014-02-11T20:29:01Z | en |
dc.date.available | 2014-02-11T20:29:01Z | en |
dc.date.issued | 2002-10-21 | en |
dc.identifier.uri | http://hdl.handle.net/2122/8925 | en |
dc.description.abstract | This paper deals with a Southern Italy area, 40 km by 10 km wide, located where four river valleys anastomose themselves in the coastal plain. The geological and hydrogeological features of the study area and the chemical-physical groundwater characterisation have been inferred from the data analysis of 1130 boreholes. Some aquifers, connected among them, constituted by soils of different geological origin -marine terraces deposits, river valley alluvial deposits and alluvial and coastal deposits - have been considered. The coastal plain aquifer is the most interesting for practical utilisation. Groundwater flow is mainly unconfined in the marine terraces and in the river valleys while it becomes mostly confined in the coastal plain aquifer. An upper clayey layer overlies the sandy coastal aquifer characterised by a mean hydraulic conductivity value equal to 2.3 10-4 m/s. The bottom is a silty-clayey bed which lies under the sea level. Being the direct natural recharge extremely low, the recharge of this coastal aquifer is mainly guaranteed by the discharge from upward aquifers and from the river leakage. The new acquired knowledge permits to delineate scenarios useful for an optimization of the groundwater resources tapping and for pursuing the safeguard of them. | en |
dc.language.iso | English | en |
dc.relation.ispartof | Groundwater and human development | en |
dc.subject | coastal aquifer | en |
dc.subject | hydrogeological parameters | en |
dc.subject | Basilicata | en |
dc.subject | Italy | en |
dc.title | Characterisation of the Ionian-Lucanian coastal plain aquifer | en |
dc.type | Conference paper | en |
dc.description.status | Published | en |
dc.subject.INGV | 05. General::05.08. Risk::05.08.02. Hydrogeological risk | en |
dc.description.ConferenceLocation | Mar del Plata, Argentina | en |
dc.relation.references | Brückner H. 1980. Marine Terrassen in Süditalien, Eine quartärmorphologishe Studie über das Küstentiefland von Metapont. Düsseldorfer Geographische Schriften, 14, 1-235. Ciaranfi N., Maggiore M, Pieri P., Rapisardi L., Ricchetti G., and Walsh N. 1979. Considerazioni sulla neotettonica della Fossa bradanica (Considerations about the neotectonic of Bradanic trough). Progetto Finalizzato Geodinamica del CNR, 251, 73-95. Cocco E., Cravero E., Di Geronimo S., Mezzadri G., Parea G. C., Pescatore T., Valloni R., and Vinci A. 1975. Lineamenti geomorfologici e sedimentologici del litorale alto ionico (Golfo di Taranto) (Geomorphological and sedimentological features of the Ionian littoral, Taranto Gulf). Bollettino Società Geologica Italiana, 94, 993-1051. Cotecchia V. and Magri G. 1966. Idrogeologia del Gargano (Hydrogeology of the Gragano). Geologia Applicata e Idrogeologia, 1, 1-86. Cotecchia V., Dai Pra G. and Magri G. 1971. Morfogenesi litorale olocenica tra Capo Spulico e Taranto nella prospettiva della protezione costiera (Holocenic morphological evolution of the littoral between Capo Spulico and Taranto with the aim of a coastal protection). Geologia Applicata e Idrogeologia, 6, 65-78. Doglioni C., Tropeano M., Mongelli F, and Pieri P. 1996. Middle-Late Pleistocene uplift of Puglia: an “anomaly” in the Apenninic foreland. Memorie Società Geologica Italiana, 52, 457-468. Parea G. C. 1986. I terrazzi marini tardo-pleistocenici del fronte della catena appenninica in relazione alla geologia dell’avanfossa adriatica (The Late Pleistocene marine terraces in front of the Apennines in relation to the geology of Adriatic Foredeep). Memorie Società Geologica Italiana, 35, 913-936. Pieri P., Sabato L. and Tropeano M. 1996. Significato geodinamico dei caratteri deposizionali e strutturali della Fossa Bradanica nel Pleistocene. Memorie Società Geologica Italiana, 51, 501-515. Polemio M. and Mitolo D. 1999. La vulnerabilità dell’acquifero della piana costiera di Metaponto (The aquifer vulnerability of the Metaponto coastal plain). Il rischio idrogeologico e la difesa del suolo, Accademia Nazionale dei Lincei, 423-428. Polemio M., Dragone V., Limoni P.P., Mitolo D. and Santaloia F. 2002a. Extended report of CNR-CERIST unit on deliverables: first year of activity. European research project “CRYSTECHSALIN”. Polemio M., Limoni P.P., Mitolo D. and Santaloia F. 2002b. Characterisation of ionian-lucanian coastal aquifer and seawater intrusion hazard. 17th SWIM Meeting, Deft, 6 to 10 May 2002, in press. Radina B. 1956. Alcune considerazioni geoidrologiche sulla fascia costiera jonica compresa fra i fiumi Bradano e Sinni (Some geo-hydrogeological considerations about the Ionian coastal plain between the Bradano and Sinni Rivers). Geotecnica, 1, 3-11. Sella M., Turci C., and Riva A. 1988. Sintesi geopetrolifera della Fossa Bradanica (avanfossa della catena appenninica meridionale) (Summary of the oil explorations carried out in the Bradanic trough – foredeep of the Southern Italy Apennines). Memorie Società Geologica Italiana, 41, 87-107. Tropeano M., Sabato L, and Pieri P. 2001. The Quaternary “Post-turbidite” sedimentation in the South-Apennines Foredeep (Bradanic Trough-Southern Italy). Bollettino Società Geologica Italiana, in press. | en |
dc.description.obiettivoSpecifico | 6A. Monitoraggio ambientale, sicurezza e territorio | en |
dc.description.fulltext | open | en |
dc.contributor.author | Polemio, M. | en |
dc.contributor.author | Limoni, P.P. | en |
dc.contributor.author | Mitolo, D. | en |
dc.contributor.author | Santaloia, F. | en |
dc.contributor.department | CNR-IRPI, Bari | en |
dc.contributor.department | CNR-IRPI, Bari | en |
dc.contributor.department | CNR-IRPI, Bari | en |
dc.contributor.editor | Bocanegra, E. M. | en |
dc.contributor.editor | Martinez, D. | en |
dc.contributor.editor | Massone, H. E. | en |
item.openairetype | Conference paper | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | CNR-IRPI | - |
crisitem.author.dept | CNR-IRPI | - |
crisitem.author.dept | CNR-IRPI | - |
crisitem.author.dept | CNR-IRPI, Italy | - |
crisitem.classification.parent | 05. General | - |
Appears in Collections: | Conference materials |
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