HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic Response

Many Italian rock slopes are characterized by unstable rock masses that cause constant rock falls and rockslides. To effectively mitigate their catastrophic consequence thorough studies are required. Four velocimeters have been placed in the Torgiovannetto quarry area for an extensive seismic noise...

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Main Authors: Alessia Lotti, Veronica Pazzi, Gilberto Saccorotti, Andrea Fiaschi, Luca Matassoni, Giovanni Gigli
Format: Article
Language:English
Published: Hindawi Limited 2018-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2018/9383189
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spelling doaj-28cf280316bc4a83af67d6983ec8d9092020-11-24T21:23:14ZengHindawi LimitedInternational Journal of Geophysics1687-885X1687-88682018-01-01201810.1155/2018/93831899383189HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic ResponseAlessia Lotti0Veronica Pazzi1Gilberto Saccorotti2Andrea Fiaschi3Luca Matassoni4Giovanni Gigli5Department of Earth Sciences, University of Firenze, Via G. La Pira 4, 50121 Firenze, ItalyDepartment of Earth Sciences, University of Firenze, Via G. La Pira 4, 50121 Firenze, ItalyNational Institute of Geophysics and Volcanology, Via della Faggiola 32, Pisa, ItalyFondazione Parsec, Via di Galceti 74, Prato, ItalyFondazione Parsec, Via di Galceti 74, Prato, ItalyDepartment of Earth Sciences, University of Firenze, Via G. La Pira 4, 50121 Firenze, ItalyMany Italian rock slopes are characterized by unstable rock masses that cause constant rock falls and rockslides. To effectively mitigate their catastrophic consequence thorough studies are required. Four velocimeters have been placed in the Torgiovannetto quarry area for an extensive seismic noise investigation. The study area (with an approximate surface of 200×100 m) is located near the town of Assisi (Italy) and is threatened by a rockslide. In this work, we present the results of the preliminary horizontal to vertical spectral ratio analysis of the acquired passive seismic data aimed at understanding the pattern of the seismic noise variation in case of stress state and/or weathering conditions (fluid content and microfracturing). The Torgiovannetto unstable slope has been monitored since 2003 by Alta Scuola of Perugia and the Department of Earth Sciences of the University of Firenze, after the observation of a first movement by the State Forestry Corps. The available data allowed an extensive comparison between seismic signals, displacement, and meteorological information. The measured displacements are well correlated with the precipitation trend, but unfortunately no resemblance with the seismic data was observed. However, a significant correlation between temperature data and the horizontal to vertical spectral ratio trend of the seismic noise could be identified. This can be related to the indirect effect of temperature on rock mass conditions and further extensive studies (also in the time frequency domain) are required to better comprehend this dependency. Finally, the continuous on-line data reveal interesting applications to provide near-real time warning systems for emerging potentially disastrous rockslides.http://dx.doi.org/10.1155/2018/9383189
collection DOAJ
language English
format Article
sources DOAJ
author Alessia Lotti
Veronica Pazzi
Gilberto Saccorotti
Andrea Fiaschi
Luca Matassoni
Giovanni Gigli
spellingShingle Alessia Lotti
Veronica Pazzi
Gilberto Saccorotti
Andrea Fiaschi
Luca Matassoni
Giovanni Gigli
HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic Response
International Journal of Geophysics
author_facet Alessia Lotti
Veronica Pazzi
Gilberto Saccorotti
Andrea Fiaschi
Luca Matassoni
Giovanni Gigli
author_sort Alessia Lotti
title HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic Response
title_short HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic Response
title_full HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic Response
title_fullStr HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic Response
title_full_unstemmed HVSR Analysis of Rockslide Seismic Signals to Assess the Subsoil Conditions and the Site Seismic Response
title_sort hvsr analysis of rockslide seismic signals to assess the subsoil conditions and the site seismic response
publisher Hindawi Limited
series International Journal of Geophysics
issn 1687-885X
1687-8868
publishDate 2018-01-01
description Many Italian rock slopes are characterized by unstable rock masses that cause constant rock falls and rockslides. To effectively mitigate their catastrophic consequence thorough studies are required. Four velocimeters have been placed in the Torgiovannetto quarry area for an extensive seismic noise investigation. The study area (with an approximate surface of 200×100 m) is located near the town of Assisi (Italy) and is threatened by a rockslide. In this work, we present the results of the preliminary horizontal to vertical spectral ratio analysis of the acquired passive seismic data aimed at understanding the pattern of the seismic noise variation in case of stress state and/or weathering conditions (fluid content and microfracturing). The Torgiovannetto unstable slope has been monitored since 2003 by Alta Scuola of Perugia and the Department of Earth Sciences of the University of Firenze, after the observation of a first movement by the State Forestry Corps. The available data allowed an extensive comparison between seismic signals, displacement, and meteorological information. The measured displacements are well correlated with the precipitation trend, but unfortunately no resemblance with the seismic data was observed. However, a significant correlation between temperature data and the horizontal to vertical spectral ratio trend of the seismic noise could be identified. This can be related to the indirect effect of temperature on rock mass conditions and further extensive studies (also in the time frequency domain) are required to better comprehend this dependency. Finally, the continuous on-line data reveal interesting applications to provide near-real time warning systems for emerging potentially disastrous rockslides.
url http://dx.doi.org/10.1155/2018/9383189
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