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首页> 外文期刊>Geophysical Research Letters >Field relations among coseismic ground motion, water level change and liquefaction for the 1999 Chi-Chi (M-w=7.5) earthquake, Taiwan - art. no. 1890
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Field relations among coseismic ground motion, water level change and liquefaction for the 1999 Chi-Chi (M-w=7.5) earthquake, Taiwan - art. no. 1890

机译:台湾1999年集集(M-w = 7.5)地震的同震地震动,水位变化和液化之间的场关系-艺术。没有。 1890年

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1] Field-based, basin-wide relations are discovered among coseismic ground motion, water-level change and liquefaction induced by the 1999 (M-w = 7.5) Chi-Chi earthquake, Taiwan. The relations imply thresholds of 4.4 m/s(2) and 0.6 m/s in the spectral acceleration and velocity at 1 Hz, respectively, below which pore pressure does not change appreciably and above which pore pressure increases exponentially with increasing acceleration and velocity. Liquefaction occurs when the 1-Hz spectral acceleration and velocity and the peak ground acceleration exceed -16 m/s(2), -2.4 m/s, and -2.5 m/s(2) (-0.26 g), respectively. Broad consistency between the present and previous results suggests that the relations may be transferable to other areas and may provide fundamental constraints for modeling coseismic pore-pressure increase and liquefaction. [References: 21
机译:1]在台湾1999年的Chi-Chi地震引起的同震地面运动,水位变化和液化之间发现了基于场的盆地范围关系。这种关系意味着在1 Hz处的频谱加速度和速度阈值分别为4.4 m / s(2)和0.6 m / s,低于该阈值时,孔隙压力不会发生明显变化,高于此阈值时,孔隙压力会随着加速度和速度的增加呈指数增加。当1-Hz频谱加速度和速度以及地面峰值加速度分别超过-16 m / s(2),-2.4 m / s和-2.5 m / s(2)(-0.26 g)时,就会发生液化。当前结果与先前结果之间的广泛一致性表明,这种关系可能会转移到其他地区,并可能为模拟同震孔隙压力增加和液化提供基本约束。 [参考:21

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