2018
DOI: 10.1002/eqe.3026
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Earthquake soil‐structure interaction of nuclear power plants, differences in response to 3‐D, 3 × 1‐D, and 1‐D excitations

Abstract: Summary In soil‐structure interaction modeling of systems subjected to earthquake motions, it is classically assumed that the incoming wave field, produced by an earthquake, is unidimensional and vertically propagating. This work explores the validity of this assumption by performing earthquake soil‐structure interaction modeling, including explicit modeling of sources, seismic wave propagation, site, and structure. The domain reduction method is used to couple seismic (near‐field) simulations with local soil‐… Show more

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Cited by 39 publications
(26 citation statements)
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“…For this reason, the direct approach with three-dimensional high-fidelity models has not been often used. With the advancement of computers, the works applying larger three-dimensional models have been increasing; see [25][26][27][28]. The characteristic of such works is that they applied the solid element models with non-linear property only to the soil domain, not to the structure domain.…”
Section: Direct Methods For Evaluating Ssimentioning
confidence: 99%
“…For this reason, the direct approach with three-dimensional high-fidelity models has not been often used. With the advancement of computers, the works applying larger three-dimensional models have been increasing; see [25][26][27][28]. The characteristic of such works is that they applied the solid element models with non-linear property only to the soil domain, not to the structure domain.…”
Section: Direct Methods For Evaluating Ssimentioning
confidence: 99%
“…The two plate elements were interposed inside each of approximately 9,000 concrete blocks. We used the same material values, including Rayleigh damping, listed by Abell et al 6 The element number, node number, and DOFs were 334,260, 349,793, and 1,004379, respectively. The 1940 El Centro ground motion was applied for a duration of 53.78 s in increments of 0.02 s. The analysis was performed using server was equipped with an Intel Xeon E5-2670 CPU (2.6 GHz, 8 cores per node).…”
Section: Implementation and Scalabilitymentioning
confidence: 99%
“…an inevitable increase of potentially dangerous places [1]. Therefore, scientists and regulators are progressively taking advantage of the ever-increasing computational power available, to embrace a holistic modeling strategy that couples the large scale seismological models for the region of interest (including the fault mechanism and the geological properties of the Earth's crust), with local engineering models for geotechnical, site-effect and structural analyses (see, for instance, the well established engineering method called Domain Reduction Method (DRM) [2,3], the Micro-Macro Analysis Method (MMAM) [4,5,6]). To this purpose, one major challenge to be faced resides into the need to enlarge the accuracy of the numerical prediction at higher frequency, so to render a synthetic broad-band On the other hand, seismological studies are struggling with the poor characterization of continental discontinuities and geological interfaces in the Earth's crust, which adds to the huge computational burden required to perform wave propagation/inversion studies in complex and large 3-D domains.…”
Section: Synthetic Simulation Of 3-d Earthquake Ground Motion From Thmentioning
confidence: 99%