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DatoValore
TitleUnderstanding the subsidence process of a quaternary plain by combining geological and hydrogeological modelling with satellite InSAR data: The Acque Albule Plain case study
AbstractThis paper focuses on a multidisciplinary study carried out in an urban area affected by subsidence and related structural damages. The study area is located about 20 km east of Rome (Italy) and is characterised by relevant groundwater exploitation for various purposes as well as by the presence of compressible soils immediately below the ground level. Extensive processing at different scales of SAR satellite images (ERS and ENVISAT provided by ESA in the frame of a CAT-1 project) by means of A-DInSAR technique was performed. The time histories of ground displacements, have been analysed in combination with a detailed geological setting of the study area and with the hydrogeological changes occurred in the last decades (as the response to the anthropic stress) based on a large piezometric dataset. This comprehensive dataset allowed us to describe the space and time distributions of the subsidence process. The spatial pattern and deformation rate change is attributed to the following causes: i) the changes in the groundwater levels due to the intensification of mine exploitation (requiring dewatering operations) and ii) the distribution and thickness of recent compressible deposits. Specifically, it is derived that the groundwater level variations drive the timing of subsidence triggering over the area, whereas the local geological conditions control the magnitude of the deformation process. (C) 2015 Elsevier Inc. All rights reserved.
SourceRemote sensing of environment 168, pp. 219–238
KeywordsSynthetic Aperture Radar InterferometrySubsidenceHydrogeological modellingMiningDewateringCompressible soil
JournalRemote sensing of environment
EditorAmerican Elsevier Pub. Co.,, New York,, Stati Uniti d'America
Year2015
TypeArticolo in rivista
DOI10.1016/j.rse.2015.07.010
AuthorsBozzano, Francesca; Esposito, Carlo; Franchi, Stefania; Mazzanti, Paolo; Perissin, Daniele; Rocca, Alfredo; Romano, Emanuele
Text336498 2015 10.1016/j.rse.2015.07.010 ISI Web of Science WOS 000361405500018 Scopus 2 s2.0 84937861906 Synthetic Aperture Radar Interferometry Subsidence Hydrogeological modelling Mining Dewatering Compressible soil Understanding the subsidence process of a quaternary plain by combining geological and hydrogeological modelling with satellite InSAR data The Acque Albule Plain case study Bozzano, Francesca; Esposito, Carlo; Franchi, Stefania; Mazzanti, Paolo; Perissin, Daniele; Rocca, Alfredo; Romano, Emanuele Dipartimento di Scienze della Terra, Universita La Sapienza ; Dipartimento di Scienze della Terra, Universita La Sapienza ; Dipartimento di Scienze della Terra, Universita La Sapienza ; NHAZCA S.r.l. Spin off dell Universita La Sapienza ; Lyle School of Civil Engineering, Purdue University, 550 Stadium Mall Drive West Lafayette, IN 47907, United States; Dipartimento di Scienze della Terra, Universita La Sapienza ; Istituto di Ricerca sulle Acque, Consiglio Nazionale delle Ricerche This paper focuses on a multidisciplinary study carried out in an urban area affected by subsidence and related structural damages. The study area is located about 20 km east of Rome Italy and is characterised by relevant groundwater exploitation for various purposes as well as by the presence of compressible soils immediately below the ground level. Extensive processing at different scales of SAR satellite images ERS and ENVISAT provided by ESA in the frame of a CAT 1 project by means of A DInSAR technique was performed. The time histories of ground displacements, have been analysed in combination with a detailed geological setting of the study area and with the hydrogeological changes occurred in the last decades as the response to the anthropic stress based on a large piezometric dataset. This comprehensive dataset allowed us to describe the space and time distributions of the subsidence process. The spatial pattern and deformation rate change is attributed to the following causes i the changes in the groundwater levels due to the intensification of mine exploitation requiring dewatering operations and ii the distribution and thickness of recent compressible deposits. Specifically, it is derived that the groundwater level variations drive the timing of subsidence triggering over the area, whereas the local geological conditions control the magnitude of the deformation process. C 2015 Elsevier Inc. All rights reserved. 168 Published version Understanding the subsidence process of a quaternary plain by combining geological and hydrogeological modelling with satellite InSAR data 2015_Bozzano_et_al_Understanding_the_subsidence_process_of_a_quaternary_plain_by_combining_geological_and_hydrogeological_modelling_with_satellite_InSAR_data.pdf Articolo in rivista American Elsevier Pub. Co., 0034 4257 Remote sensing of environment Remote sensing of environment Remote sens. environ. Remote sensing of environment. emanuele.romano ROMANO EMANUELE