首页> 外文会议>International Symposium on Structural Engineering >THE STUDY ON CONTRIBUTION COMPARISON BETWEEN DIRECT WAVE PLUS SINGLE SCATTERING WAVE AND MULTIPLE SCATTERING WAVE ON S WAVE ENVELOPE SYNTHESIZED BY MULTIPLE NON-ISOTROPIC SCATTERING THEORY
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THE STUDY ON CONTRIBUTION COMPARISON BETWEEN DIRECT WAVE PLUS SINGLE SCATTERING WAVE AND MULTIPLE SCATTERING WAVE ON S WAVE ENVELOPE SYNTHESIZED BY MULTIPLE NON-ISOTROPIC SCATTERING THEORY

机译:多种非各向同性散射理论合成了直接波加上单散射波和多散射波与多散射波的贡献比较研究

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In this paper,based on Sato's non-isotropic scattering theory,a seismic wave density integral equation is improved by introducing a characteristic source time,which is used to define the initial impulse width at the source.Then,based on non-isotropic patterns derived from the inhomogeneous random media,a discrete wave-number method is used to solve the improved S wave energy density integral equation.And the S wave velocity envelope is obtained according to the relationship between energy density and velocity.Based on different non-isotropic scattering patterns,the effect of group of direct wave and single scattering term and multiple scattering terms on S wave velocity envelope is originally investigated.From the analysis result,the result from the group of direct wave and single scattering term match the whole velocity envelope of S wave pretty well at small hypocentral distance(less than 100km).Therefore,in this case,the multiple scattering terms can be neglected and the single scattering model can be used to simulate the S wave scattering process.With increasing of hypocentral distance,multiple scattering terms will be gradually dominated over the group of direct wave and single scattering term.Compared with results from backward and isotropic scattering pattern,the contribution of multiple scattering terms from forward scattering pattern grew more rapidly.And multiple scattering terms must be considered to model the whole S wave velocity envelope when the hypocentral distance is larger than 100km.Consequently,adaptability conditions of the single,multiple scattering theory are clarified,respectively.
机译:本文基于佐藤的非各向同性散射理论,通过引入特征源时间来改善地震波密度整体方程,其用于在源上定义源极的初始脉冲宽度。该基于导出的非各向同性模式从非均匀的随机介质,使用离散波数方法来解决改进的S波能量密度整体方程。根据能量密度和速度之间的关系获得的S波速度包络。基于不同的非各向同性散射图案,直接波和单次散射术语的效果和S波速度包络上的多种散射术语最初研究。分析结果,直接波组和单散射术语的结果匹配S的整个速度包络在小型斜视距离(小于100km)的比较良好。因此,在这种情况下,可以忽略多种散射术语并且单一的SCAT可以使用模型模拟S波散射过程。随着斜视距离的增加,多种散射术语将逐渐占据直接波和单次散射术语的组中..具有来自后向和各向同性散射模式的结果,贡献从前向散射模式的多个散射术语迅速增长。当斜斜屏距离大于100km时,必须考虑多个散射术语模拟整个S波速度包络。分别阐明了单一,多种散射理论的适应性条件。

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