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Vulnerability and Site Effects in Earthquake Disasters in Armenia (Colombia). I—Site Effects

机译:亚美尼亚(哥伦比亚)地震灾害中的脆弱性和现场影响。 I-现场效果

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The city of Armenia, Colombia has been repeatedly subjected to moderate magnitude earthquakes. Damage in that city for the 1999 (Mw6.2) event was disproportionate (maximum observed EMS-92 intensity of IX), even considering the small epicentral distance (18 km). Two main factors have been invoked: Site effects and vulnerability of the building stock. We re-analyze available data on site effects, including: Records of aftershocks of the 1999 event, ambient noise records obtained using standalone stations, array records of ambient noise, and available shear wave profiles from seismic cone measurements. We estimate local amplification from spectral ratios of earthquake records relative to a reference site, the horizontal relative to the vertical component (HVSR, Horizontal-to-Vertical Spectral Ratios) of earthquakes and ambient noise records, and ratios of response spectra relative to a reference site or to simulated ground motion. These estimates are compared to amplification functions computed for 1D soil models, inverted from microtremor array observations. Our estimates of site effects for Armenia are therefore robust and bring together results previously available only in internal reports. We show that spectral ratios relative to a reference site may fail to estimate the amplification level. Site effects in Armenia are relatively homogeneous. Although site amplification is very significant and contributed to the observed damage, it does not account for the irregular damage distribution observed in 1999.
机译:哥伦比亚亚美尼亚市曾多次遭受中度地震。即使考虑到较小的震中距离(18 km),该城市在1999年(Mw6.2)事件中的破坏程度也不成比例(最大观测到的IX的EMS-92强度)。调用了两个主要因素:场地影响和建筑存量的脆弱性。我们重新分析有关现场影响的可用数据,包括:1999年地震的余震记录,使用独立站点获得的环境噪声记录,环境噪声的阵列记录以及来自地震锥测量的可用剪切波剖面。我们根据相对于参考地点的地震记录的频谱比率,相对于地震和环境噪声记录的垂直分量(HVSR,水平对垂直频谱比率)的水平以及响应频谱相对于基准的比率来估计局部放大现场或模拟地面运动。将这些估计值与为一维土壤模型计算的放大函数进行比较,该函数是从微震阵列观察中得出的。因此,我们对亚美尼亚的场地影响估算是可靠的,并将以前只能在内部报告中获得的结果汇总在一起。我们表明,相对于参考位点的光谱比可能无法估计扩增水平。亚美尼亚的地盘影响相对均匀。尽管站点放大非常重要,并且对观察到的破坏有所贡献,但它并不能解释1999年观测到的不规则破坏分布。

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