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  5. Long-Term Displacement Monitoring of Slow Earthflows by Inclinometers and GPS, and Wide Area Surveillance by COSMO-SkyMed Data
 
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Long-Term Displacement Monitoring of Slow Earthflows by Inclinometers and GPS, and Wide Area Surveillance by COSMO-SkyMed Data

Author(s)
Vassallo, Roberto  
Scuola di Ingegneria, Università della Basilicata, Viale dell’Ateneo Lucano, 10, 85100 Potenza, Italy  
Calcaterra, Stefano  
Istituto Superiore per la Protezione e la Ricerca Ambientale (ISPRA), Servizio Geologico d’Italia, Via Brancati, 48, 00144 Roma, Italy  
D'Agostino, Nicola  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
De Rosa, Jacopo  
i Ingegneria, Università della Basilicata, Viale dell’Ateneo Lucano, 10, 85100 Potenza, Italy  
Di Maio, Caterina  
i Ingegneria, Università della Basilicata, Viale dell’Ateneo Lucano, 10, 85100 Potenza, Italy  
Gambino, Piera  
Istituto Superiore per la Protezione e la Ricerca Ambientale (ISPRA), Servizio Geologico d’Italia, Via Brancati, 48, 00144 Roma, Italy  
Language
English
Obiettivo Specifico
7A. Geofisica per il monitoraggio ambientale
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Geosciences  
Issue/vol(year)
5/10 (2020)
Publisher
mpdi
Pages (printed)
id 171
Date Issued
2020
DOI
10.3390/geosciences10050171
URI
https://www.earth-prints.org/handle/2122/13600
Abstract
With reference to two slow earthflows in structurally complex clayey formations of the Italian southern Apennines, this paper shows the results of a long-term displacement monitoring using integrated systems of inclinometers and GPS, and their comparison with PSInSAR data. A fixed-in-place and traversal inclinometer system, first installed in 2004, recorded both the shear displacements along the slip bands, and the internal deformations of the landslide masses. A GPS network of permanent stations and benchmarks, installed in 2006–2007 in 23 strategic points of the slope, allowed for the temporal continuity of displacement monitoring. The two long series of data allowed to evaluate the factor scaling of the PSInSAR COSMO-SkyMed data, although the component of the displacement vector along the line of sight (LOS) was small. PSInSAR data allowed for the monitoring extension to houses and rigid structures that acted as reflectors. The joint data analysis allowed for the comprehension of the main features of the landslides’ kinematics.
Type
article
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vassalo_etal_geosciences2020.pdf

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