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不同散射模式下S波包络合成
引用本文:景月岭,何李浩,李明会,张宇璇,郑司元. 不同散射模式下S波包络合成[J]. 地震学报, 2021, 43(6): 679-689. DOI: 10.11939/jass.20200208
作者姓名:景月岭  何李浩  李明会  张宇璇  郑司元
作者单位:中国合肥230001 合肥工业大学土木与水利工程学院;中国北京100089 清华大学水沙科学与水利水电工程国家重点实验室;中国合肥230001 合肥工业大学土木与水利工程学院
基金项目:中央高校基本科研业务费专项资金(PA2019GDPK0036)和清华大学水沙科学与水利水电工程国家重点实验室开放基金(sklhse-2020-D-04)共同资助
摘    要:为揭示地震波在地壳小尺度非均匀介质中的散射过程,更准确地描述地震波的包络展宽现象,本文基于多次各向异性散射理论,采用离散波数法求解能量密度积分方程,选取高斯型自相关函数表征的散射模式,得到S波能量密度包络.基于此,本文首先分析了单次散射和多次散射在形成S波能量密度包络中的贡献规律;然后探讨了吸收系数和总散射系数对合成S...

关 键 词:各向异性  散射理论  高斯型介质  前散射模式  S波包络
收稿时间:2020-12-21

S wave envelope synthesis based on different scattering patterns
Jing Yueling,He Lihao,Li Minghui,Zhang Yuxuan,Zheng Siyuan. S wave envelope synthesis based on different scattering patterns[J]. Acta Seismologica Sinica, 2021, 43(6): 679-689. DOI: 10.11939/jass.20200208
Authors:Jing Yueling  He Lihao  Li Minghui  Zhang Yuxuan  Zheng Siyuan
Affiliation:1.Civil and Hydraulic Engineering,Hefei University of Technology,Hefei 230001,China2.State Key Laboratory of Hydroscience and Engineering,Tsinghua University,Beijing 100089,China
Abstract:In order to reveal the scattering process of seismic waves in the small scale inhomogeneous medium of the crust and to describe the envelopment broadening phenomenon of seismic waves more accurately, a discrete wave-number method is used to solve the improved seismic wave energy density integral equation based on the multiple anisotropic scattering theory, and the scattering pattern represented by Gaussian autocorrelation function is selected to obtain the S wave energy density envelope. Firstly, we analyzed the contribution of single scattering and multiple scattering to the energy density envelope of S wave. Then, we discussed the effects of absorption coefficient and total scattering coefficient on the synthesis of S wave energy density envelope. Finally, we compared the differences of the energy density envelope of S wave synthesized in different scattering patterns. The results show that: ① The contribution of single scattering and multiple scattering to the seismic wave scattering process is consistent, and for the near earthquakes (hypocentral distance is less than 100 km), the single scattering model can be used to match the S-wave energy density envelope. As the hypocentral distance increases, the multiple forward scattering pattern can approach the total energy density envelope more quickly. ② As the absorption coefficient increases, the amplitude of the direct S wave and the coda wave will decrease. And when the total scattering coefficient increases, the amplitude of the direct S wave will decrease, while the coda wave amplitude of the S wave will increase. ③ In the forward scattering pattern, with the increase of hypocentral distance, the energy density envelope of S-wave appears the peak delay, the envelope is widened, and the attenuation consistency of the coda wave is accelerated. 
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