Özet
Natural disasters from earthquakes can cause considerable damages, with potentially severe effects to urban environment. Last strong Vrancea earthquake on March 4, 1977 (Mw=7.4, depth=95km); tens of thousands of buildings damaged, many people injured and dead. Strong earthquakes in the Vrancea zone occur between 60-200 km depth within an almost vertical column. Bucharest Earthquake Early Warning (EEW) system detects earthquakes with a seismic network in the epicentral Vrancea region and issue a warning in Bucharest providing 20-25s warning time. In this study, we have investigated the relationships of the bracketed cumulative absolute velocity window (BCAV-W) approach versus epicentral distance and magnitude for Vrancea region. Firstly, a set of time histories contains 11 earthquakes, 111 strong ground motion records for intermediate depth earthquakes with different magnitudes (4.0≤Mw≤6.0) and epicentral distances (0-200 km) are analyzed to determine relations between the window size (W) and BCAV-W ratio. The BCAV-W computed for different windows time size 2s, 4s, 8s, 12s, 16s, 32s, 64s, 128s and 256s have the ratios 24%, 40%, 61%, 74%, 84%, 97%, 97%, 100% and 100% to the total BCAV respectively. The results show that there is no significant benefit to choose a window size more than 16s. Subsequently, rational threshold levels related to Mw=5.4+ earthquakes are determined as 0.28 m/s and 0.34 m/s related to 12-second and 16-second windows, respectively. The goal of the paper is to enhance EEW capability to decrease the effects of Vrancea earthquakes on urban and built environment.
Orijinal dil | İngilizce |
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Sayfa (başlangıç-bitiş) | 141-147 |
Sayfa sayısı | 7 |
Dergi | Environmental Engineering and Management Journal |
Hacim | 16 |
Basın numarası | 1 |
DOI'lar | |
Yayın durumu | Yayınlandı - Oca 2017 |
Harici olarak yayınlandı | Evet |
Bibliyografik not
Publisher Copyright:© 2017, Gheorghe Asachi Technical University of Iasi, Romania. All rights reserved.
Finansman
The authors appreciate two anonymous reviewers for their very constructive suggestions and critics, which helped in improving the manuscript. We also would like to thank to Prof. Dr. Gheorghe Marmureanu and to Dr. Y.M. Fahjan for their valuable suggestions and comments. This work was supported partially by a grant of the Romanian National Authority for Scientific Research, CNCS – UEFISCDI, project number PN-II-RU-TE-2012-3-0215 and by the Network of European Research Infrastructures for Earthquake Risk Assessment and Mitigation (NERA www.nera-eu.org) project, FP7, EC grant no. 262330.
Finansörler | Finansör numarası |
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Corporation for National and Community Service | |
European Commission | 262330 |
Consiliul National al Cercetarii Stiintifice | PN-II-RU-TE-2012-3-0215 |
Seventh Framework Programme | |
Autoritatea Natională pentru Cercetare Stiintifică | |
Unitatea Executiva pentru Finantarea Invatamantului Superior, a Cercetarii, Dezvoltarii si Inovarii |