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Anticipate Construction of Single Pylon Cable-Stayed Kretek II Bridge in Near-Fault Zone

 Anticipate Construction of Single Pylon Cable-Stayed Kretek II Bridge in Near-Fault Zone
Autor(en): , ,
Beitrag für IABSE Congress: The Evolving Metropolis, New York, NY, USA, 4-6 September 2019, veröffentlicht in , S. 158-164
DOI: 10.2749/newyork.2019.0158
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The earthquake event occurred with a magnitude of 7.4 which caused a tsunami and liquefaction was the cause the Ponulele bridge collapse, which precisely cut the location of the fault. Such events ...
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Bibliografische Angaben

Autor(en): (PT. Pratama Daya Cahya Manunggal)
(PT. Pratama Daya Cahya Manunggal)
(PT. Pratama Daya Cahya Manunggal)
Medium: Tagungsbeitrag
Sprache(n): Englisch
Tagung: IABSE Congress: The Evolving Metropolis, New York, NY, USA, 4-6 September 2019
Veröffentlicht in:
Seite(n): 158-164 Anzahl der Seiten (im PDF): 7
Seite(n): 158-164
Anzahl der Seiten (im PDF): 7
DOI: 10.2749/newyork.2019.0158
Abstrakt:

The earthquake event occurred with a magnitude of 7.4 which caused a tsunami and liquefaction was the cause the Ponulele bridge collapse, which precisely cut the location of the fault. Such events are expected not to occur in other locations. The characteristics of Kretek II cable-stayed bridge location is relatively identical to the location of the Ponulele Bridge. The distance of Opak fault from the location of the planned Kretek II Bridge is approximately 20 m with a slip-rate of 2.4 mm/year. This situation is also exacerbated by local soil conditions that have the potential for liquefaction.

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