Finite-Difference Contrast Source Inversion Method for Elastic Wave Equation

S. Wang, Haiyang Li, D. Wang, S. Zhou
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引用次数: 0

Abstract

Summary This abstract extends the finite-difference contrast source inversion (FD-CSI) method to reconstruct the P-wave and S-wave velocity for two-dimensional elastic wave inversion in the framework of the full-waveform inversion. The FD-CSI method is an iterative nonlinear inversion method, which exhibits several strengths. First, the finite-difference operator only relies on the background media and the given frequency, both of which are unchanged during inversion. Therefore, the full forward problem is required to be solved only once at the beginning of the inversion process, which makes the method very computationally efficient and ideal for large-scale 3D inversion calculations. Another attractive feature of the inversion method is that it is with strong capability in dealing with nonlinear inverse problems in an inhomogeneous background medium, because a 25 points finite-difference operator is used to represent the differential operator governing the two-dimensional elastic wave propagation. Numerical reconstruction results show that the inversion method has an excellent performance for reconstructing P-wave and S-wave and can provide more accurate velocity information for seismic data processing and interpretation.
弹性波动方程的有限差分对比源反演方法
本文扩展了有限差分对比源反演(FD-CSI)方法,在全波形反演的框架下重建二维弹性波反演的纵波和横波速度。FD-CSI方法是一种迭代非线性反演方法,具有许多优点。首先,有限差分算子只依赖于背景介质和给定频率,这两者在反演过程中是不变的。因此,在反演过程开始时只需要求解一次全正演问题,这使得该方法的计算效率非常高,非常适合大规模的三维反演计算。该方法的另一个吸引人的特点是,由于采用25点有限差分算子来表示控制二维弹性波传播的微分算子,因此具有很强的处理非均匀背景介质非线性反演问题的能力。数值重建结果表明,该方法具有较好的纵波和横波重建效果,可为地震资料处理和解释提供更准确的速度信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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