| Project/Area Number |
07555140
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| Research Category |
Grant-in-Aid for Scientific Research (A)
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| Allocation Type | Single-year Grants |
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| Section | 展開研究 |
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| Research Field |
構造工学・地震工学
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| Research Institution | TOKYO INSTITUTE OF TECHNOLOGY |
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Principal Investigator |
OHMACHI Tatsuo TOKYO INSTITUTE OF TECHNOLOGY, 大学院・総合理工学研究科, 教授 (90126269)
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| Co-Investigator(Kenkyū-buntansha) |
TOSHINAWA Takumi TOKYO INSTITUTE OF TECHNOLOGY, 大学院・総合理工学研究科, 助教授 (00188749)
NAKAMURA Yutaka TOKYO INSTITUTE OF TECHNOLOGY, 研究職
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| Project Period (FY) |
1995 – 1997
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| Project Status |
Completed (Fiscal Year 1997)
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| Budget Amount *help |
¥7,200,000 (Direct Cost: ¥7,200,000)
Fiscal Year 1997: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1996: ¥600,000 (Direct Cost: ¥600,000)
Fiscal Year 1995: ¥6,100,000 (Direct Cost: ¥6,100,000)
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| Keywords | Ground-motion characteristics / Seismic hazard prediction / Site amplification / Microtremors / Strong motions / データベース / コヒーレンス |
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| Research Abstract |
Strong-motion and microtremor observations are carried out in Kamakura and Kitahassaku area, Yokohama, in order to evaluate ground-motion characteristics in the areas. In Kamakura, four accelerographs are installed on soft rocks and Holocene lowland. The observed records contain siteamplification characteristics at each site although the records are contaminated by building vibrations. It is shown that the site-amplification characteristics can be detected by H/V spectral ratios of microtremors. The H/V spectral method is modified by introducing coherence between horizontal and vertical motions. The new method is applied to site-amplification evaluation in Kamakura. The results are consistent with the damage distribution in Kamakura area during the 1923 Kanto earthquake. In Kitahassaku area, three accelerographs are installed on loam plateau and Holocene lowland. Strong-motion observation shows that a plateau site has larger site-amplification characteristics in comparison to lowland sites by a factor of about 1.5 in peak horizontal ground velocity and about 2 in spectral peak amplitudes of Fourier amplitude-spectra. The amplification is due to subsurface soils which are accumulated on soft rocks. The site-amplification characteristics at the strong-motion sites can be detected by H/V spectral ratios of microtremors. Spot microtremor observations conducted in the area demonstrate that resonance periods on plateaus are related to elevation ; high site amplification areas distribute along rivers in the lowlands and the Shimosueyoshi plateau. The comparisons of spectral characteristics of strong motions and microtremors show the applicability of microtremors to evaluation of ground-motion characteristics for seismic hazard prediction.
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