A new elastic wave equation for decoupling P-wave and S-waves and its application

IF 4.4 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS
Computers & Geosciences Pub Date : 2026-02-01 Epub Date: 2025-10-14 DOI:10.1016/j.cageo.2025.106065
Meng Guo , Bingshou He , Qianqian Ci
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引用次数: 0

Abstract

The imaging of P-wave and S-wave in reverse time migration (RTM) of elastic waves is often achieved by cross-correlating P-waves or S-waves with different propagation directions. This requires us to obtain the Poynting vector or optical flow vector of each imaging point at different times during the wavefield extrapolation process and use it to indicate the direction of wave propagation. But we can only obtain the Poynting vector of the mixed wavefield of P-wave and S- waves, and we cannot obtain the Poynting vector of pure P-wave or pure S-wave when using the existing velocity-stress elastic wave equations for the wavefield extrapolation process. Therefore, the propagation direction obtained is also a mixed wavefield rather than pure P-wave or pure S-wave, and this does not meet the requirements for elastic wave RTM and will cause errors. The existing first-order velocity-dilation-rotation elastic wave equation, although it overcomes the aforementioned issues, cannot accurately describe the law of wave propagation at the wave impedance interface due to the assumption of a homogeneous medium. Especially when the interface of P-wave and S-wave velocities is not consistent, it will lead to errors in the reflection, transmission, and conversion wavefields when using this equation for elastic wavefield extrapolation. In addition, severe energy leakage effects will occur at the interface of S-wave velocity when using this equation, which will lead to inaccurate S-wave imaging. In this paper, we propose a new elastic wave equation for decoupling P-wave and S-waves based on the assumption of an inhomogeneous medium, which not only gives the propagation direction of pure P-wave and pure S-wave, but also completely overcomes the above problems. Using the new equation of the Poynting vector in the elastic wave field to perform cross-correlation imaging, the model calculations show that the imaging results eliminate the noise generated by RTM, demonstrating the accuracy and applicability of the equation.
纵波与横波解耦的弹性波动方程及其应用
弹性波逆时偏移(RTM)中的纵波和横波成像通常是通过不同传播方向的纵波或横波相互关联来实现的。这就要求我们在波场外推过程中,获取每个成像点在不同时刻的坡印亭矢量或光流矢量,并用它来指示波的传播方向。但我们只能得到纵波和横波混合波场的Poynting矢量,而用现有的速度-应力弹性波方程进行波场外推时,无法得到纯纵波或纯横波的Poynting矢量。因此,得到的传播方向也是混合波场,而不是纯p波或纯s波,这不符合弹性波RTM的要求,会产生误差。现有的一阶速度-膨胀-旋转弹性波动方程虽然克服了上述问题,但由于假设介质均质,无法准确描述波在波阻抗界面处的传播规律。特别是当纵波和横波速度界面不一致时,用该方程进行弹性波场外推时,会导致反射、透射和转换波场出现误差。此外,使用该方程时,在横波速度界面处会产生严重的能量泄漏效应,导致横波成像不准确。本文基于非均匀介质的假设,提出了一种新的纵波与横波解耦的弹性波动方程,不仅给出了纯纵波和纯横波的传播方向,而且完全克服了上述问题。利用弹性波场中新的Poynting矢量方程进行互相关成像,模型计算表明,成像结果消除了RTM产生的噪声,证明了该方程的准确性和适用性。
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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来源期刊
Computers & Geosciences
Computers & Geosciences 地学-地球科学综合
CiteScore
9.30
自引率
6.80%
发文量
164
审稿时长
3.4 months
期刊介绍: Computers & Geosciences publishes high impact, original research at the interface between Computer Sciences and Geosciences. Publications should apply modern computer science paradigms, whether computational or informatics-based, to address problems in the geosciences.
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