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Simplified Dispersion Curves of Earthquake Love Wave for Rotational Seismic Motion Estimation

机译:旋转地震运动估计的地震爱波的简化色散曲线

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In the simulation of the rotational seismic ground motion, the apparent velocity of Love wave is always assumed to be equal to the S wave velocity of top layer of the site approximately, with the dispersion of surface wave not being fully considered. In this paper, the effect of the velocity structure to the Love wave dispersion is discussed based on the stiffness matrix theory. It shows that to assume the velocity to be equal to the S wave velocity of the top layer may greatly overestimate the low frequency rotational seismic motion. A simplified dispersion curve, is suggested for rotational seismic ground motion simulation. The shape of the bilinear curve is shaped by 3 parameters. They are the corner frequency, the minimum phase velocity and the velocity ratio. The parameters are affected by the velocity structure of the site.
机译:在旋转地震运动的模拟中,始终认为爱波的表观速度等于大致的表面波的顶层的S波速度等于,具有不完全考虑的表面波的分散。 本文基于刚度矩阵理论讨论了速度结构对爱波色散的影响。 它表明,假设速度等于顶层的S波速度可能大大高估低频旋转地震运动。 提出了一种简化的分散曲线,用于旋转地震地面运动模拟。 双线性曲线的形状由3个参数成形。 它们是角频率,最小相速度和速度比。 参数受到网站的速度结构的影响。

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