杨晓婷, 王宁, 郎超. 0: 基于近似解析离散化算子的频率域弹性波全波形反演方法. 地震学报. doi: 10.11939/jass.20230038
引用本文: 杨晓婷, 王宁, 郎超. 0: 基于近似解析离散化算子的频率域弹性波全波形反演方法. 地震学报. doi: 10.11939/jass.20230038
XiaoTing YANG, Ning WANG, Chao LANG. 0: A frequency domain elastic wave full waveform inversion method based on nearly analytic discrete operator. Acta Seismologica Sinica. doi: 10.11939/jass.20230038
Citation: XiaoTing YANG, Ning WANG, Chao LANG. 0: A frequency domain elastic wave full waveform inversion method based on nearly analytic discrete operator. Acta Seismologica Sinica. doi: 10.11939/jass.20230038

基于近似解析离散化算子的频率域弹性波全波形反演方法

A frequency domain elastic wave full waveform inversion method based on nearly analytic discrete operator

  • 摘要:       全波形反演是一种利用地震波传播的动力学特征来获取地下介质物性参数的反演方法,可为揭示地下精细结构提供重要依据. 本文以弹性波方程作为数学模型来模拟地震波传播规律并进行相应的反演方法研究. 为提高计算效率与反演结果的准确性,近似解析离散化(NAD)算子可用于频率域弹性波方程的正演模拟. 本文在NAD离散的基础上推导阻抗矩阵的稀疏分块结构与反演目标函数对模型参数的梯度计算公式,由此建立基于NAD算子的频率域弹性波全波形反演方法. 为验证该方法的有效性,文中通过数值实验对多种典型介质模型进行反演计算,均得到了理想的反演结果.

     

    Abstract:      Full waveform inversion is an inversion method to obtain the physical parameters of subsurface media by using the dynamic characteristics of seismic wave propagation, which can provide an important basis for revealing the fine structure of subsurface. In this paper, the elastic wave equation is used as mathematical model to simulate the propagation law of seismic wave and the corresponding inversion method is studied. In order to improve the computational efficiency and the accuracy of the inversion results, the nearly analytic discrete ( NAD ) operator can be used for the forward modeling of the frequency-domain elastic wave equation. In this paper, based on the NAD discretization, the sparse block structure of the impedance matrix and the gradient calculation formula of the inversion objective function to the model parameters are derived, and the frequency-domain elastic wave full waveform inversion method based on the NAD operator is established. In order to verify the effectiveness of the method, a variety of typical medium models are inverted by numerical experiments, and the ideal inversion results are obtained.

     

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