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Estimation of near-surface attenuation using inversion of Rayleigh waves with fundamental and higher modes

机译:利用基础且较高模式的瑞利波逆转近视衰减估计

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Wave energy attenuation in near surface is an important physics issue for many applications. Various estimation methods have been developed for measuring Q from Rayleigh waves; however, the conventional methods are based on the assumption of layered earth model. In this paper we proposed a method to estimate near-surface Q from Rayleigh waves with fundamental and higher modes. This method can deal with complex media which are not layered. The simulated annealing algorithm is used and a new objective function is given. The velocities and densities of near-surface materials are assumed to be provided, Rayleigh waves are modeled by finite difference method; then based on the dispersion properties of Rayleigh waves, Rayleigh-wave mode separation is performed. The objective function is calculated using the amplitude information of fundamental- and higher-mode Rayleigh waves. The numerical tests show that our method can obtain accurate Q in complex media.
机译:近曲面的波浪能衰减是许多应用的重要物理问题。已经开发了各种估计方法,用于测量瑞利波的Q;然而,传统方法基于层状地球模型的假设。在本文中,我们提出了一种用基本且更高模式从瑞利波估算近表面Q的方法。此方法可以处理不分层的复杂媒体。使用模拟退火算法,并给出了新的目标函数。假设近表面材料的速度和密度设有,瑞利波通过有限差分法建模;然后基于瑞利波的色散性能,执行瑞利波模式分离。使用基本和更高模式瑞利波的幅度信息来计算目标函数。数值测试表明,我们的方法可以在复杂介质中获得精确的Q.

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