2012
DOI: 10.1002/eqe.1188
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The effect of near‐fault directivity on building seismic collapse risk

Abstract: SUMMARY Forward directivity may cause large velocity pulses in ground motion time histories that are damaging to buildings at sites close to faults, potentially increasing seismic collapse risk. This study quantifies the effects of forward directivity on collapse risk through incremental dynamic analysis of building simulation models that are capable of capturing the key aspects of strength and stiffness degradation associated with structural collapse. The paper also describes a method for incorporating the ef… Show more

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Cited by 181 publications
(143 citation statements)
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“…For this reason, a second set of far-field records is needed for the determination of collapse probability for sites that are not influenced by forward directivity 305 effects. Similarly to [11], the set of far-field ground motions used in this study is based on the FEMA P695 [41] far-field ground motion set, which includes 22 record pairs, each with two horizontal components for a total of 44 ground motions. Those ground motions are recorded at sites located greater than or equal to 10 km from fault rupture; event magnitudes range from M 6.5 to M 7.6 with an average magnitude of M 7.0.…”
Section: Ground Motions Consideredmentioning
confidence: 99%
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“…For this reason, a second set of far-field records is needed for the determination of collapse probability for sites that are not influenced by forward directivity 305 effects. Similarly to [11], the set of far-field ground motions used in this study is based on the FEMA P695 [41] far-field ground motion set, which includes 22 record pairs, each with two horizontal components for a total of 44 ground motions. Those ground motions are recorded at sites located greater than or equal to 10 km from fault rupture; event magnitudes range from M 6.5 to M 7.6 with an average magnitude of M 7.0.…”
Section: Ground Motions Consideredmentioning
confidence: 99%
“…According to the NEHRP Site Class, 16 sites are classified as Site Class D (stiff soil sites) and the remaining are classified as Site Class C (very stiff soil sites). The wavelet classification algorithm developed by Baker [40] indicates that nine of these ground motion records have pulses in the velocity history [11]; these pulse-like record were then removed from the far-field database. It is worth noting that the ground motion records were selected without consideration of spectral shape.…”
Section: Ground Motions Consideredmentioning
confidence: 99%
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