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<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences Discussions</journal_title>
		<journal_url>www.hydrol-earth-syst-sci-discuss.net</journal_url>
		<issn>1812-2108</issn>
		<eissn>1812-2116</eissn>
		<volume_number>5</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/hessd-5-2859-2008</doi>
	<article_url>http://www.hydrol-earth-syst-sci-discuss.net/5/2859/2008/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci-discuss.net/5/2859/2008/hessd-5-2859-2008.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci-discuss.net/5/2859/2008/hessd-5-2859-2008.pdf</fulltext_pdf>
	<start_page>2859</start_page>
	<end_page>2898</end_page>
	<publication_date>2008-10-21</publication_date>
	<article_title content_type="html">The role of integrated high resolution stratigraphic and geophysic surveys for groundwater modelling</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Margiotta</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Mazzone</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>S. Negri</name>
			<email>sergio.negri@unile.it</email>
		</author>
		<author numeration="4" affiliations="1">
			<name>M. Calora</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratorio di modellistica idrogeofisica e stratigrafica per i rischi naturali, Dipartimento di Scienza dei Materiali, Università del Salento, via per Monteroni, Lecce 73100, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">This work sets out a methodology of integrated geological, hydrogeological
and geophysical surveys for the characterization of contaminated sites. The
flow model of the shallow aquifer in the Brindisi area (recognized to be at
significant environmental risk by the Italian government) and the impact of
an antrophic structure on the groundwater flow have been evaluated. The
stratigraphic and hydrogeological targets used for the calibration phase of
the flow model provide a means of assessing calibration quality. The good
calibration of the model point out the key role of a detailed knowledge of
the physical-stratigraphycal attributes of the area to be studied and field
data collection. Geoelectrical tomography focus the attention on an area
resulted of particular interest by the flow model obtained. This method
permit to reconstruct in detail the lateral and vertical lithological
variations in the geological formations improving the spatial resolution of
the data and consequently the scale of observation. Besides, anomaly
resistivity values have been correlated with pollution. Chemical analysis
have confirmed this correlation.</abstract>
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</article>
