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Inversion of waveforms from Xiangtang borehole seismic array for soil dynamic property

机译:相塘钻孔地震阵列波形反演的土壤动力特性。

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In order to understand the site soil response of the Xiangtang borehole seismic array under real strong ground motion, reveal the site response, verify the technique of borehole exploration, and improve the precision of in-situ test and laboratory test, this paper presents a new approach, which is composed of two methods. One is the layered site seismic response method, whose layer transform matrix is always real. The other is a global-local optimization technique, which uses genetic algorithm (GA)-simplex method. An inversion of multi-component waveforms of P, SV and SH wave is carried out simultaneously. By inverting the records of three moderate and small earthquakes obtained from the Xiangtang borehole array (2# ) site, the soil dynamic characteristic parameters, including P velocity, damping ratio and frequency-dependent coefficient b, which has not been given in previous literatures, are calculated. The results show that the soil S wave velocity of the Xiangtang 2# borehole is generally greater than that obtained from the 1994 in-situ test, and is close to the velocity of the 3# borehole, which is more than 200 m away from the 2# borehole. Meanwhile, perceptible soil nonlinear behavior under peak ground motion of about 60×10-2 m/s2 is detected by the inversion analysis. The presented method can be used for studying the soil response of other borehole array sites.
机译:为了了解向塘井筒地震阵列在真实强地震动作用下的场地土响应,揭示场地响应,验证井筒勘探技术,提高现场测试和实验室测试的精度,提出了一种新的方法。方法,它由两种方法组成。一种是分层现场地震响应方法,其层变换矩阵始终是真实的。另一种是全局局部优化技术,它使用遗传算法(GA)-简单方法。同时对P,SV和SH波的多分量波形进行反演。通过反演向塘井筒阵列(2#)现场获得的3次中小地震记录,可以得到以往文献中未曾给出的土壤动力学特征参数,包括P速度,阻尼比和频率相关系数b,计算。结果表明,向塘2#井眼的土壤S波速度一般大于1994年现场测试获得的土壤S波速度,与3#井眼的速度相近,而3#井眼的井眼距离S距井眼200 m以上。 2#钻孔。同时,通过反演分析发现了在峰值地面运动约60×10-2 m / s2时可感知的土壤非线性行为。所提出的方法可用于研究其他井眼阵列位置的土壤响应。

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