Deep geoelectrical investigation to bound a coastal thermal outflow area

The coastal carbonate Apulian aquifers, located in southern Italy, feed several coastal fresh springs and constitute the main local source of high quality water. The Santa Cesarea Terme cave system is almost unique case of hypogenic coastal spring caves, located along the Adriatic Sea coastline and...

Full description

Bibliographic Details
Main Authors:	Rizzo Enzo, Zuffianò L.E., Santaloia F., Polemio M.
Format:	Article
Language:	English
Published:	EDP Sciences 2018-01-01
Series:	E3S Web of Conferences
Online Access:	https://doi.org/10.1051/e3sconf/20185400028

id	doaj-ee813d95cde34441b578eb4410d7714c
record_format	Article
spelling	doaj-ee813d95cde34441b578eb4410d7714c2021-04-02T11:27:51ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01540002810.1051/e3sconf/20185400028e3sconf_swim2018_00028Deep geoelectrical investigation to bound a coastal thermal outflow areaRizzo Enzo0Zuffianò L.E.1Santaloia F.2Polemio M.3CNR-IMAA, National Research Council – Institute of Methodology for Environmental Analysis, C.da S. LojaCNR-IRPI, National Research Council – Research Institute for Hydrogeological Protection Via Amendola 122 ICNR-IRPI, National Research Council – Research Institute for Hydrogeological Protection Via Amendola 122 ICNR-IRPI, National Research Council – Research Institute for Hydrogeological Protection Via Amendola 122 IThe coastal carbonate Apulian aquifers, located in southern Italy, feed several coastal fresh springs and constitute the main local source of high quality water. The Santa Cesarea Terme cave system is almost unique case of hypogenic coastal spring caves, located along the Adriatic Sea coastline and hosting spring coastal outflow of mixed groundwater (from 22°C to 33°C) mainly of thermal groundwater due to infiltration offshore, in the sea bottom, and pure fresh groundwater due rainfall infiltration. Thermal springs and the outflow system are strictly controlled by both the discontinuity network and the karst processes involving the foreland environment. Detailed geoelectrical prospecting were carried out to bound the upflow continental area of this system, considering the geoelectrical effects of deep water mixing with different salinity and temperature close the Adriatic coast.https://doi.org/10.1051/e3sconf/20185400028
collection	DOAJ
language	English
format	Article
sources	DOAJ
author	Rizzo Enzo Zuffianò L.E. Santaloia F. Polemio M.
spellingShingle	Rizzo Enzo Zuffianò L.E. Santaloia F. Polemio M. Deep geoelectrical investigation to bound a coastal thermal outflow area E3S Web of Conferences
author_facet	Rizzo Enzo Zuffianò L.E. Santaloia F. Polemio M.
author_sort	Rizzo Enzo
title	Deep geoelectrical investigation to bound a coastal thermal outflow area
title_short	Deep geoelectrical investigation to bound a coastal thermal outflow area
title_full	Deep geoelectrical investigation to bound a coastal thermal outflow area
title_fullStr	Deep geoelectrical investigation to bound a coastal thermal outflow area
title_full_unstemmed	Deep geoelectrical investigation to bound a coastal thermal outflow area
title_sort	deep geoelectrical investigation to bound a coastal thermal outflow area
publisher	EDP Sciences
series	E3S Web of Conferences
issn	2267-1242
publishDate	2018-01-01
description	The coastal carbonate Apulian aquifers, located in southern Italy, feed several coastal fresh springs and constitute the main local source of high quality water. The Santa Cesarea Terme cave system is almost unique case of hypogenic coastal spring caves, located along the Adriatic Sea coastline and hosting spring coastal outflow of mixed groundwater (from 22°C to 33°C) mainly of thermal groundwater due to infiltration offshore, in the sea bottom, and pure fresh groundwater due rainfall infiltration. Thermal springs and the outflow system are strictly controlled by both the discontinuity network and the karst processes involving the foreland environment. Detailed geoelectrical prospecting were carried out to bound the upflow continental area of this system, considering the geoelectrical effects of deep water mixing with different salinity and temperature close the Adriatic coast.
url	https://doi.org/10.1051/e3sconf/20185400028
work_keys_str_mv	AT rizzoenzo deepgeoelectricalinvestigationtoboundacoastalthermaloutflowarea AT zuffianole deepgeoelectricalinvestigationtoboundacoastalthermaloutflowarea AT santaloiaf deepgeoelectricalinvestigationtoboundacoastalthermaloutflowarea AT polemiom deepgeoelectricalinvestigationtoboundacoastalthermaloutflowarea
_version_	1724164755747241984

Deep geoelectrical investigation to bound a coastal thermal outflow area

Similar Items