Use of PSInSAR data to map highly compressible soil layers
A new approach to the use of Persistent Scatterers (PS) Interferometry data in the reconstruction of the extension of compressible geological bodies is presented. The methodology was applied in the test area of the Tiber River delta (Italy), characterized by the presence of two large marshy zones, k...
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Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB)
2015-11-01
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Series: | Geologica Acta |
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Online Access: | https://revistes.ub.edu/index.php/GEOACTA/article/view/10404 |
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author | C. DEL VENTISETTE L. SOLARI F. RASPINI A. CIAMPALINI F. DI TRAGLIA M. MOSCATELLI A. PAGLIAROLI S. MORETTI |
author_facet | C. DEL VENTISETTE L. SOLARI F. RASPINI A. CIAMPALINI F. DI TRAGLIA M. MOSCATELLI A. PAGLIAROLI S. MORETTI |
author_sort | C. DEL VENTISETTE |
collection | DOAJ |
description | A new approach to the use of Persistent Scatterers (PS) Interferometry data in the reconstruction of the extension of compressible geological bodies is presented. The methodology was applied in the test area of the Tiber River delta (Italy), characterized by the presence of two large marshy zones, known as the Maccarese and Ostia Antica ponds. PSInSAR™ data, derived from ERS1/2, ENVISAT and RADARSAT-1 images, and spanning a time interval between 1992 and 2006 were used to verify the possibility to reconstruct the spatial distribution of the peat levels inside the Maccarese and Ostia Antica ponds. Borehole information was analyzed to calibrate the InSAR data and the deformation rates were used to hypothesize the presence of a thick compressible layer where geological information is lacking. Variations in deformation rates registered by the single PS were assumed to be representative of a variation in the stratigraphic asset. The obtained results demonstrate that this approach could be satisfactorily used to investigate wide areas in a short time, reducing the number of boreholes to drill, and it could be a complementary technique to obtain information about the 2D geometry of specific geological levels. |
first_indexed | 2024-03-11T17:01:28Z |
format | Article |
id | doaj.art-9b2e69486786409c9a54ab660793f54d |
institution | Directory Open Access Journal |
issn | 1696-5728 |
language | English |
last_indexed | 2024-03-11T17:01:28Z |
publishDate | 2015-11-01 |
publisher | Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) |
record_format | Article |
series | Geologica Acta |
spelling | doaj.art-9b2e69486786409c9a54ab660793f54d2023-10-20T07:22:45ZengUniversitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB)Geologica Acta1696-57282015-11-01134Use of PSInSAR data to map highly compressible soil layersC. DEL VENTISETTE0L. SOLARI1F. RASPINI2A. CIAMPALINI3F. DI TRAGLIA4M. MOSCATELLI5A. PAGLIAROLI6S. MORETTI7Department of earth Sciences, University of Firenze. Via La Pira 4, 50121 Firenze, Italy.Department of earth Sciences, University of Firenze. Via La Pira 4, 50121 Firenze, Italy.Department of earth Sciences, University of Firenze. Via La Pira 4, 50121 Firenze, Italy.Department of earth Sciences, University of Firenze. Via La Pira 4, 50121 Firenze, Italy.Department of earth Sciences, University of Firenze. Via La Pira 4, 50121 Firenze, Italy.CNR–IGAG, Institute of environmental Geology and Geoengineering. Area della Ricerca di Roma 1. Montelibretti, via Salaria km 29,300, 00015 Monterotondo Stazione, Roma, Italy.CNR–IGAG, Institute of environmental Geology and Geoengineering. Area della Ricerca di Roma 1. Montelibretti, via Salaria km 29,300, 00015 Monterotondo Stazione, Roma, Italy.Department of earth Sciences, University of Firenze. Via La Pira 4, 50121 Firenze, Italy.A new approach to the use of Persistent Scatterers (PS) Interferometry data in the reconstruction of the extension of compressible geological bodies is presented. The methodology was applied in the test area of the Tiber River delta (Italy), characterized by the presence of two large marshy zones, known as the Maccarese and Ostia Antica ponds. PSInSAR™ data, derived from ERS1/2, ENVISAT and RADARSAT-1 images, and spanning a time interval between 1992 and 2006 were used to verify the possibility to reconstruct the spatial distribution of the peat levels inside the Maccarese and Ostia Antica ponds. Borehole information was analyzed to calibrate the InSAR data and the deformation rates were used to hypothesize the presence of a thick compressible layer where geological information is lacking. Variations in deformation rates registered by the single PS were assumed to be representative of a variation in the stratigraphic asset. The obtained results demonstrate that this approach could be satisfactorily used to investigate wide areas in a short time, reducing the number of boreholes to drill, and it could be a complementary technique to obtain information about the 2D geometry of specific geological levels.https://revistes.ub.edu/index.php/GEOACTA/article/view/10404InSARPS analysisSurface deformation analysis2D stratigraphic reconstructionTiber deltaPeat |
spellingShingle | C. DEL VENTISETTE L. SOLARI F. RASPINI A. CIAMPALINI F. DI TRAGLIA M. MOSCATELLI A. PAGLIAROLI S. MORETTI Use of PSInSAR data to map highly compressible soil layers Geologica Acta InSAR PS analysis Surface deformation analysis 2D stratigraphic reconstruction Tiber delta Peat |
title | Use of PSInSAR data to map highly compressible soil layers |
title_full | Use of PSInSAR data to map highly compressible soil layers |
title_fullStr | Use of PSInSAR data to map highly compressible soil layers |
title_full_unstemmed | Use of PSInSAR data to map highly compressible soil layers |
title_short | Use of PSInSAR data to map highly compressible soil layers |
title_sort | use of psinsar data to map highly compressible soil layers |
topic | InSAR PS analysis Surface deformation analysis 2D stratigraphic reconstruction Tiber delta Peat |
url | https://revistes.ub.edu/index.php/GEOACTA/article/view/10404 |
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