Giuseppina Tusa

Dr. Giuseppina Tusa

Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Catania, Sicilia, Italy
orcid

Research Focus & Metrics

Academic Career Length

25Years (2002-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 October 2002 in Journal of Seismology
Verified
Journal Article
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EGE. Giampiccolo
E. Giampiccolo
GTGiuseppina Tusa
Giuseppina Tusa
HLH. Langer
H. Langer
SGS. Gresta
S. Gresta

1 December 2008 in Bulletin of the Seismological Society of America
Verified
Journal Article
Closed access
GTGiuseppina Tusa
Giuseppina Tusa
SGS. Gresta
S. Gresta

2 August 2015 in Journal of Seismology
Verified
Journal Article
Closed access
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GTGiuseppina Tusa
Giuseppina Tusa
HLHorst Langer
Horst Langer

27 May 2022 in Remote Sensing
Verified
Journal Article
Open access
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DPDomenico Patanè
Domenico Patanè
GTGiuseppina Tusa
Giuseppina Tusa
WYWilliam Yang
William Yang
AAAntonio Astuti
Antonio Astuti
ACAntonio Colino
Antonio Colino
OTOrazio Torrisi
Orazio Torrisi
We describe the first dense real-time urban seismic–accelerometric network in Italy, named OSU-CT, located in the historic center of Catania. The city lies in the region with the greatest danger, vulnerability, and earthquake exposure in the entire Italian territory. OSU-CT was planned and realized within the project called EWAS “an Early WArning System for cultural heritage”, aimed at the rapid assessment of earthquake-induced damage and the testing of an on-site earthquake early warning system. OSU-CT is mainly based on low-cost instrumentation realized ad hoc by using cutting-edge technologies and digital MEMS (micro-electro-mechanical systems) triaxial accelerometers with excellent resolution and low noise. Twenty of the forty scheduled stations have already been set up on the ground floor of significant historic public buildings. In order to assess the performance of an earthquake early warning (EEW) on-site system, we also installed wide-band velocimeters (ETL3D/5s) in three edifices chosen as test sites, which will be instrumented for a structural health monitoring (SHM). In addition to several laboratory and field validation tests on the developed instruments, an effective operational test of OSU-CT was the Mw 4.3 earthquake occurring on 23 December 2021, 16 km west, south-west of Catania. Peak ground accelerations (4.956 gal to 39.360 gal) recorded by the network allowed obtaining a first urban shakemap and determining a reliable distribution of ground motion in the historical center of the city, useful for the vulnerability studies of the historical edifices.

7 October 2015 in Bulletin of Earthquake Engineering
Verified
Journal Article
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HLHorst Langer
Horst Langer
GTGiuseppina Tusa
Giuseppina Tusa
LSLuciano Scarfì
Luciano Scarfì
Raffaele AzzaroRaffaele Azzaro
Raffaele Azzaro

8 February 2025 in Sensors
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Journal Article
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GOGiuseppe Occhipinti
Giuseppe Occhipinti
Francesco Lo IaconoFrancesco Lo Iacono
Francesco Lo Iacono
GTGiuseppina Tusa
Giuseppina Tusa
ACAntonio Costanza
Antonio Costanza
GFGioacchino Fertitta
Gioacchino Fertitta
DPDomenico Patanè
Domenico Patanè
This study presents the results of an experimental investigation conducted on a 2:3 scale model of a two-story stone masonry building. We tested the model on the UniKORE L.E.D.A. lab shake table, simulating the Mw 6.3 earthquake ground motion that struck L’Aquila, Italy, on 6 April 2009, with progressively increasing peak acceleration levels. We installed a network of accelerometric sensors on the model to capture its structural behaviour under seismic excitation. Medium-to lower-cost MEMS accelerometers (classes A and B) were compared with traditional piezoelectric sensors commonly used in Structural Health Monitoring (SHM). The experiment assessed the structural performance and damage progression of masonry buildings subjected to realistic earthquake inputs. Additionally, the collected data provided valuable insights into the effectiveness of different sensor types and configurations in detecting key vibrational and failure patterns. All the sensors were able to accurately measure the dynamic response during seismic excitation. However, not all of them were suitable for Operational Modal Analysis (OMA) in noisy environments, where their self-noise represents a crucial factor. This suggests that the self-noise of MEMS accelerometers must be less than 1 µg/√Hz, or preferably below 0.5 µg/√Hz, to obtain good results from the OMA. Therefore, we recommend ultra-low-noise sensors for detecting differences in the structural behaviour before and after seismic events. Our findings provide valuable insights into the seismic vulnerability of masonry structures and the effectiveness of sensors in detecting damage. The management of buildings in earthquake-prone areas can benefit from these specifications.