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Kohei Fujita

Researcher at University of Tokyo

Publications -  156
Citations -  1600

Kohei Fujita is an academic researcher from University of Tokyo. The author has contributed to research in topics: Damper & Computer science. The author has an hindex of 18, co-authored 136 publications receiving 1293 citations. Previous affiliations of Kohei Fujita include Kyoto University & Japan Society for the Promotion of Science.

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The 2011 off the Pacific coast of Tohoku earthquake and response of high-rise buildings under long-period ground motions

TL;DR: In this article, the effectiveness of visco-elastic dampers like high-hardness rubber dampers in the reduction of responses of super high-rise buildings subjected to such long-period ground motions is investigated.
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Optimal placement of viscoelastic dampers and supporting members under variable critical excitations

TL;DR: In this article, a new strategy based on the concept of active and passive structural control has been introduced rather recently in order to provide structural designers with powerful tools for performance-based design.
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Innovative base-isolated building with large mass-ratio TMD at basement for greater earthquake resilience

TL;DR: In this article, an innovative and resilient base-isolated building with a large mass-ratio tuned mass dampers (TMD) is introduced for earthquake loading in which the large massratio TMD is located at basement.
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An efficient methodology for robustness evaluation by advanced interval analysis using updated second-order Taylor series expansion

TL;DR: In this article, an enhanced and efficient methodology for interval analysis is proposed to evaluate the robustness of an uncertain structure by taking into account the possibility of occurrence of the extreme value of the objective function in an inner domain of interval parameters.
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Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake.

TL;DR: The results suggest that a rapid mantle flow takes place in the asthenosphere with temporarily decreased viscosity in response to large coseismic stress, presumably due to the activation of power-law creep during the post-earthquake period.