This paper reports the results of a long-term monitoring of the slow movements of two deep earthflows in tectonized clay shales of southern Apennines. The cumulated movements have caused over the years severe damage to buildings and infrastructure, with important social and economic costs. Deep and superficial displacements, along with pore water pressures, are being monitored since 2005; in some areas of the slope, displacement monitoring by inclinometers started about 30 years ago. The kinematics of the landslides has been clarified sufficiently on the basis of ground-based measurements. On the other hand, the mostly N-S orientation of displacements, and the rather limited urbanization, make it rather challenging to monitor the area by satellite interferometry methodology. To minimize such problem, satellite data relative to areas where the displacements and their directions are clearly determined by inclinometers and GPS were analysed at the most detailed scale of analysis. The data validation allowed to confidently exploit remote sensing results in a wider area. Thus, images acquired by the COSMO-SkyMed satellite system, supplemented by ERS and Envisat data (available since 1993), allowed the reconstruction of the kinematic history of the urbanized area even where inclinometer displacement series were available only over short periods. Indications about the effectiveness of the remedial measures constructed in the area under study could also be obtained. ? 2021 Patron Editore S.r.l.. All rights reserved., funding_text?1=The Authors would like to thank the Italian Space Agency (ASI) for providing the Cosmo-SkyMed data set through the ASI Open Call for Science Project ID-763. This research has been supported by MI-UR PON R&I 2014-2020 Program (project MITIGO, ARS01_00964).
In situ and satellite long-term monitoring of two earthflows of the Italian southern Apennines and of the structures built on them [Monitoraggio di lungo periodo in situ e satellitare di due colate di terreni argillosi dell'Appennino meridionale e delle strutture su di esse costruite]
Reale D;Verde S;Fornaro;
2021
Abstract
This paper reports the results of a long-term monitoring of the slow movements of two deep earthflows in tectonized clay shales of southern Apennines. The cumulated movements have caused over the years severe damage to buildings and infrastructure, with important social and economic costs. Deep and superficial displacements, along with pore water pressures, are being monitored since 2005; in some areas of the slope, displacement monitoring by inclinometers started about 30 years ago. The kinematics of the landslides has been clarified sufficiently on the basis of ground-based measurements. On the other hand, the mostly N-S orientation of displacements, and the rather limited urbanization, make it rather challenging to monitor the area by satellite interferometry methodology. To minimize such problem, satellite data relative to areas where the displacements and their directions are clearly determined by inclinometers and GPS were analysed at the most detailed scale of analysis. The data validation allowed to confidently exploit remote sensing results in a wider area. Thus, images acquired by the COSMO-SkyMed satellite system, supplemented by ERS and Envisat data (available since 1993), allowed the reconstruction of the kinematic history of the urbanized area even where inclinometer displacement series were available only over short periods. Indications about the effectiveness of the remedial measures constructed in the area under study could also be obtained. ? 2021 Patron Editore S.r.l.. All rights reserved., funding_text?1=The Authors would like to thank the Italian Space Agency (ASI) for providing the Cosmo-SkyMed data set through the ASI Open Call for Science Project ID-763. This research has been supported by MI-UR PON R&I 2014-2020 Program (project MITIGO, ARS01_00964).I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
