InSAR Monitoring Using Persistent Scatterer Interferometry (PSI) and Small Baseline Subset (SBAS) Techniques for Ground Deformation Measurement in Metropolitan Area of Concepción, Chile

Author:

Giorgini Eugenia12ORCID,Orellana Felipe3,Arratia Camila4,Tavasci Luca1ORCID,Montalva Gonzalo3ORCID,Moreno Marcos5ORCID,Gandolfi Stefano1ORCID

Affiliation:

1. Department of Civil, Chemical, Environmental, and Materials Engineering—DICAM, University of Bologna, 40136 Bologna, Italy

2. National PhD in Earth Observation, Sapienza University of Rome, 00185 Rome, Italy

3. Department of Civil Engineering—DIC, University of Concepcion, Concepcion 4070371, Chile

4. Department of Geophysics—DGEO, University of Concepcion, Concepcion 4070386, Chile

5. Department of Structural and Geotechnical Engineering—DIEG, Pontifical Catholic University of Chile, Santiago 7820436, Chile

Abstract

InSAR capabilities allow us to understand ground deformations in large metropolitan areas, this is key to assessing site conditions in areas in an inherently expanding context. The multi-temporal interferometry of SAR data records ground surface displacement velocities over large metropolitan areas, identifying anomalous and potential geological hazards. The metropolitan city of Concepción, Chile, is an alluvial basin in one of the world’s most seismically active subduction zones, where many subduction earthquakes have occurred throughout history. In this study, we monitored the deformations of the ground surface in the metropolitan area of Concepción using two interferometric techniques, the first being Persistent Scatterer Interferometry (PSI) and the second, the Small Baseline Subset (SBAS) technique. To do this, we have used the same Sentinel-1 dataset, obtaining ground movement rates between 2019 and 2021. The velocities were aligned with the GNSS station available in the area. Ground deformation patterns show local deformations depending on factors such as soil type and heterogeneity, and regional deformations due to geographical location in the subduction area. Our results highlight the similarity of the deformation rates obtained with different processing techniques and have also allowed us to identify areas of deformation and compare them to site conditions. These results are essential to evaluate ground conditions and contribute to urban planning and risk management in highly seismic areas.

Funder

Chilean National Research and Development Agency

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

Reference66 articles.

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3. Leyton, F., Montalva, G., and Ramírez, P. (2011, January 23–26). Effects of surface geology on seismic motion. Proceedings of the 4th IASPEI/IAEEE International Symposium, Santa Barbara, CA, USA.

4. A new algorithm for surface deformation monitoring based on small baseline differential SAR interferograms;Berardino;IEEE Trans. Geosci. Remote Sens.,2002

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