| Project/Area Number |
14550477
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (C)
|
| Allocation Type | Single-year Grants |
|---|
| Section | 一般 |
|---|
| Research Field |
構造工学・地震工学
|
|---|
| Research Institution | Shinshu University |
|---|
Principal Investigator |
IZUTANI Yasuo Shinshu University, Faculty of Engineering, Professor, 工学部, 教授 (60092863)
|
|---|
| Project Period (FY) |
2002 – 2004
|
| Project Status |
Completed (Fiscal Year 2004)
|
| Budget Amount *help |
¥2,900,000 (Direct Cost: ¥2,900,000)
Fiscal Year 2004: ¥1,000,000 (Direct Cost: ¥1,000,000)
Fiscal Year 2003: ¥700,000 (Direct Cost: ¥700,000)
Fiscal Year 2002: ¥1,200,000 (Direct Cost: ¥1,200,000)
|
|---|
| Keywords | Source spectrum / Radiated energy / Seismic moment / Corner frequency / Similarity / Strong ground motion / K-NET / KiK-net / 強振動 / 鳥取県西部地震 |
|---|
| Research Abstract |
Strong motion records at K-NET and KiK-net stations are analyzed to examine relationship between short-period source spectral amplitude and seismic moment. Earthquakes dealt with in this study are those occurred in Northwestern Kagoshima region, Western Tottori region, Northern Miyagi region, and Niigata Chuetsu region. Moment magnitude of these events are from 3.3 to 6.6. Epicentral distance to the stations is less than 60 km.
Spectral ratio between transverse component aaelerograms of the largest event and each of the other event in each group are calculated at each station in order to remove the effects of wave propagation path to the stations. Then the spectral ratios at all stations are averaged to remove the effect of difference in focal mechanism. Thus, the spectral ratio of the records represents the source spectral ratio.
The similarity of earthquake expects that the short-period spectral ratio is proportional to the cubic root of the ratio of the seismic moment. However, the observed short-period spectral ratio is generally larger than the expectation from the similarity. Larger earthquakes radiate short-period seismic energy more effectively than smaller ones.
Appropriate correction for the deviation from the similarity of earthquake should be made when we aim at simulation of strong ground motion for future large earthquakes by the empirical Green's function method. If we assume the similarity of earthquake, the resultant short period seismic wave for large earthquakes would be underestimated. A correction factor is proposed in terms of the difference in seismic moment between a target large earthquake and a small earthquake whose records are adopted as empirical Green's functions.
|
