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首页> 外文期刊>Bulletin of the Seismological Society of America >Site Characterization of Strong-Motion Recording Stations of Delhi Using Joint Inversion of Phase Velocity Dispersion and H/V Curve
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Site Characterization of Strong-Motion Recording Stations of Delhi Using Joint Inversion of Phase Velocity Dispersion and H/V Curve

机译:相速度色散和H / V曲线联合反演德里强运动记录站的站点特征

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摘要

Site characterization is one of the most important aspects of any strong-motion instrumentation. Nowadays it has become common practice to provide the characterization details up to bedrock level. Without proper site characterization, strong-motion records of any station cannot be fully utilized. In India, strong-motion instrumentation sites were classified in three categories as per V-S30 values. These V-S30 values were estimated using the Borcherdt (1994) methodology, in which physical properties of visible soil layer are used for V-S30 estimation. Because this methodology does not use any field testing, the probability of getting erroneous results is very high. Hence, to get accurate assessment of site characteristics, we conducted field testing at 19 strong-motion instrumentation sites in Delhi, India. The site characteristics assessed here are determined using joint inversion of multichannel analysis of surface waves and horizontal-to-vertical spectral ratio (HVSR) from ambient noise results simultaneously to estimate shear-wave velocity profiles. The benefit of using this method is that it provides site characteristics assessed through shear-wave velocity profiles up to much deeper soil strata. The results obtained from this analysis are further validated using ground response analysis from recorded ground motions. Further, the profiles obtained are studied for uncertainties using the computer program STRATA. Transfer functions obtained from STRATA are then compared with HVSR of ambient vibration records as well as HVSR from weak-motion earthquake records available for the sites. These curves are found to well matching with each other in this study. Site characterization carried out here will be very useful for studies related to seismic-hazard assessment of the Delhi region and studies related to attenuation models.
机译:现场表征是任何强运动仪器最重要的方面之一。如今,提供高达基岩级别的特征详细信息已成为一种常见的做法。如果没有适当的站点表征,则无法充分利用任何站点的强运动记录。在印度,根据V-S30值,强运动仪表场所被分为三类。这些V-S30值是使用Borcherdt(1994)方法估算的,其中将可见土壤层的物理特性用于V-S30估算。由于此方法不使用任何现场测试,因此获得错误结果的可能性非常高。因此,为了准确评估站点特征,我们在印度德里的19个强运动仪表站点进行了现场测试。此处评估的站点特征是通过对表面波进行多通道分析的联合反演和来自环境噪声结果的水平-垂直光谱比(HVSR)来同时估算剪切波速度分布来确定的。使用这种方法的好处是,它可以提供通过剪切波速度剖面评估的场地特征,直至更深的土壤地层。从记录的地面运动中使用地面响应分析,可以进一步验证从该分析获得的结果。此外,使用计算机程序STRATA对获得的配置文件进行不确定性研究。然后将从STRATA获得的传递函数与周围振动记录的HVSR以及场地可用的弱运动地震记录的HVSR进行比较。在本研究中,发现这些曲线相互之间很好地匹配。此处进行的站点表征对于与德里地区地震危险性评估有关的研究以及与衰减模型有关的研究将非常有用。

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