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Bulletin of Engineering Geology and the Environment

Erschienen in:

01.08.2003

High-resolution geoelectrical tomographies in the study of Giarrossa landslide (southern Italy)

verfasst von: Vincenzo Lapenna, Pietro Lorenzo, Angela Perrone, Sabatino Piscitelli, Francesco Sdao, Enzo Rizzo

Erschienen in: Bulletin of Engineering Geology and the Environment | Ausgabe 3/2003

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Abstract.

New geoelectrical techniques have been applied to the study of the Giarrossa landslide in the Lucano Appennines of southern Italy. Dipole–dipole electrical resistivity tomographies (ERT) and self-potential (SP) surveys were carried out using innovative techniques for data acquisition and inversion. The ERT showed the presence of a conductive zone at a depth of about 25–35 m associated with the landslide body and some shallow high-resistivity nuclei associated with intercalations (calcilutitic, calcarenitic blocks, etc.) in the disturbed material. Two SP areal surveys, undertaken after the winter and summer seasons, highlighted equipotential contours following the landslide boundary and an electrical field predominantly negative in the source zone and positive in the accumulation zone.

Vorheriger Artikel Batch adsorption tests of phenol in soils

Nächster Artikel Impacts de recouvrements de résidus organiques sur des résidus miniers réactifs

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Titel: High-resolution geoelectrical tomographies in the study of Giarrossa landslide (southern Italy)
verfasst von: Vincenzo Lapenna
Pietro Lorenzo
Angela Perrone
Sabatino Piscitelli
Francesco Sdao
Enzo Rizzo
Publikationsdatum: 01.08.2003
Verlag: Springer Berlin Heidelberg
Erschienen in: Bulletin of Engineering Geology and the Environment / Ausgabe 3/2003
Print ISSN: 1435-9529
Elektronische ISSN: 1435-9537
DOI: https://doi.org/10.1007/s10064-002-0184-z

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