Micro-seismic monitoring after the shipwreck of the Costa Concordia at Giglio Island (Italy)

• Autorzy: Fiaschi A. , Matassoni L. , Lotti A. , Saccorotti G.

Identyfikatory

DOI

10.1007/s11600-017-0077-y

• Języki publikacji: EN

Abstrakty

EN

A microseismic network was used for monitoring the wreck of the Costa Concordia cruise ship, wrecked and run agrounded along the Giglio Island coasts during the night of 13 January 2012, until its removal. The seismic traces were processed by means of real-time and “a posteriori” procedures to detect transients that could be ascribed to wreck movements on the sea bed to integrate this information in an early warning system for assessing the wreck stability. After a first discrimination of the transients using amplitude criteria we proceeded to the localization of the detected signals to focus the attention only on the transients originated in the shipwreck resting area. The results showed that most of the events localized on the wreck were likely related to human work activities or sudden internal brittle failure but not to displacements on the sea-floor. Instead, the displacements are associated to the impact on the vessel of great sea storms which approach were well correlated with the increasing seismic noise at low frequency. The carried out procedures based on this unique dataset represent an opportunity to test seismic monitoring techniques also in not usual engineering context to support emergency management activities.

Słowa kluczowe

EN

seismic monitoring; Costa Concordia; Giglio Island; seismic noise; wreak displacement

PL

monitoring sejsmiczny; Costa Concordia; Wyspa Giglio; szum sejsmiczny

• Wydawca: Instytut Geofizyki PAN ; Springer
• Czasopismo: Acta Geophysica
• Rocznik: 2017
• Tom: Vol. 65, no. 5
• Strony: 1019--1027
• Opis fizyczny: Bibliogr. 27 poz.

Twórcy

autor

Fiaschi A.

• Fondazione Parsec, Prato, Italy

autor

Matassoni L.

• Fondazione Parsec, Prato, Italy

autor

Lotti A.

• Dipartimento di Scienze della Terra, Università di Firenze, Florence, Italy

autor

Saccorotti G.

• Istituto Nazionale di Geofisica e Vulcanologia-Sezione di Pisa, Pisa, Italy

Bibliografia

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018)