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MICROZONATION FOR SEISMIC GEOTECHNICAL HAZARDS AND ACTUAL DAMAGE DURING THE 2005 FUKUOKA-KEN SEIHO-OKI EARTHQUAKE

机译:2005年福冈县精冲冲地震的地质岩土危害微型化与实际破坏。

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References(14) Cited-By(1) The 2005 Fukuoka-ken Seiho-oki earthquake caused damage to structures due to liquefaction, slope failure and strong shaking in Fukuoka City. One of the authors had conducted microzonation for liquefaction, slope failure and strong shaking about 17 years before the earthquake. After the earthquake, the authors compared the zoning map with the actual damage. The results showed that liquefied sites coincided fairly well with predicted zones in the reclaimed lands. However, they were slightly different in a big sand spit named Uminonakamichi. Failure occurred at several slopes inside the predicted areas, while damage to buildings occurred due to strong shaking along the Kego Fault. The damaged area was slightly different from the predicted area. Furthermore, a liquefaction analysis was conducted and the results of this analysis were compared with the results of microzonation in 1988. In this paper, the authors discuss the validity of microzonation based on this comparison.
机译:参考文献(14)引用(1)2005年福冈县圣保冈地震导致福冈市的液化,边坡破坏和强烈震动造成结构破坏。其中一位作者在地震发生前约17年进行了液化,边坡破坏和强烈震动的微区划。地震后,作者将分区图与实际破坏进行了比较。结果表明,液化场地与开垦土地上的预测区域相当吻合。但是,它们在名为Uminonakamichi的大沙坑中略有不同。在预测区域内的几个斜坡上发生了破坏,而由于沿Kego断层的强烈震动而对建筑物造成了破坏。损坏区域与预测区域略有不同。此外,还进行了液化分析,并将其分析结果与1988年的微区化结果进行了比较。在此基础上,作者讨论了微区化的有效性。

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