首页> 外文会议>World conference on earthquake engineering >ESTIMATION OF S-WAVE VELOCITY STRUCTURES BY USING MICROTREMOR H/V SPECTRA TECHNIQUE BASED ON BOTH RAYLEIGH- AND LOVE- WAVES
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ESTIMATION OF S-WAVE VELOCITY STRUCTURES BY USING MICROTREMOR H/V SPECTRA TECHNIQUE BASED ON BOTH RAYLEIGH- AND LOVE- WAVES

机译:基于瑞利和爱情的微局H / V光谱技术估计S波速度结构

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It is important to clarify basement structures of urban areas from a viewpoint of earthquake engineering. Microtremor H/V spectra techniques had been conventionally used to estimate the basement depth based on medium responses of horizontal to vertical amplitude ratio of Rayleigh wave. It is insufficient to consider only Rayleigh wave because microtremor consists of not only Rayleigh wave but also Love wave. This study tried to estimate the velocity structures from microtremor H/V spectra based on the theory of surface wave H/V spectra [Arai and Tokimatsu [1]]. This theory needs both Rayleigh and Love waves to explain microtremor H/V spectra. But, the power ratio of Rayleigh and Love waves in microtremors had not been estimated. We apply three-component spatial auto-correlation analysis, which we have developed, to obtain the power ratio of Rayleigh to Love waves in microtremors. By using this analysis we can obtain the power ratio based on tri-axial microtremor array records empirically. We carried out microtremor observations at three sites in Morioka City, the northern Honshu, Japan. We employ a circular seismic array with seven tri-axial sensors. The array observation aims to obtain the dispersion curve of phase velocity of Rayleigh wave and the power ratio of Rayleigh to Love wave, respectively. Estimated power ratios were around 1.0 at all sites. Therefore, we assumed that the ratios were 1.0 in order to calculate surface wave H/V spectra. The microtremor H/V spectra were estimated from the average of spectra at all sensors. We used genetic algorithm inversion technique to determine velocity structures from microtremor H/V spectra because the inversion of structures from microtremor H/V spectra is a non-linear problem. They also agree with the structures estimated from the dispersion curves of Rayleigh phase velocity by using a classical array technique. And synthetic surface wave H/V spectra calculated from the structure are concordant with observed microtremor H/V spectra. The results suggest that the use of both Rayleigh and Love wave is necessary to estimate velocity structures using microtremor H/V spectra.
机译:从地震工程的角度来看,重要的是澄清城市地区地区结构。 MicroTremor H / V光谱技术通常用于基于水平到瑞利波垂直幅度比的介质响应来估计地下深度。只需要考虑瑞利波是不足的,因为微调不仅包括瑞利波,而且是爱情波。本研究试图根据表面波H / V光谱理论估计来自微调H / V光谱的速度结构[ARAI和TOKIMASU [1]]。这种理论需要瑞利和爱情波来解释微调H / V光谱。但是,尚未估计瑞利和爱情波的功率比。我们应用了我们开发的三组分空间自相关分析,以获得Rayleigh的电力比在Microotremors中的波浪。通过使用该分析,我们可以根据经验上获得基于三轴微反线阵列记录的功率比。我们在日本北部摩里奥市的三个地点进行了微调观察。我们采用圆形地震阵列,具有七个三轴传感器。阵列观察分别旨在分别获得瑞利波的相速度的分散曲线和瑞利到爱波的功率比。估计的功率比在所有网站上约为1.0。因此,我们假设比率为1.0以计算表面波H / V光谱。从所有传感器的光谱的平均值估计微良H / V光谱。我们使用遗传算法反演技术来确定来自微调H / V光谱的速度结构,因为来自微调H / V光谱的结构的反转是非线性问题。它们还通过使用经典阵列技术来达到从Rayleigh阶段速度的色散曲线估计的结构。与该结构计算的合成表面波H / v光谱与观察到的微良H / V光谱有助于一致。结果表明,使用MicroTremor H / V光谱需要使用Rayleigh和Love波的使用来估计速度结构。

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