{"title":"Optical flow vector of elastic waves in TI media","authors":"Huixing Zhang, Yancang Feng, Bing-Shout He","doi":"10.1190/geo2023-0231.1","DOIUrl":null,"url":null,"abstract":"The propagation direction of the wavefield is particularly important for migration imaging in the reverse-time migration (RTM) of elastic waves in TI media. However, due to the problem of computational instability of the Poynting vector, the wave field propagation direction estimated based on the Poynting vector method has errors and cannot accurately indicate the real propagation direction of the elastic wavefield. To solve this problem, a method for calculating the optical flow vector of elastic waves in TI media is proposed to obtain the propagation direction. The optical flow vector of elastic waves in TI media is determined by applying the spatial and temporal derivatives of the wavefield at each time step, under the assumption that the wavefields are almost the same at subsequent time steps and are smooth in the spatial direction. As the additional smoothing item is added and the multiple iterative algorithm is introduced in calculating the optical flow vector, the direction is calculated more accurately than the Poynting vector. Based on the optical flow vectors, we can separate the source-wavefield and receiver-wavefield into four directions: up-going, down-going, left-going and right-going wavefields, respectively, and finally perform elastic reverse-time migration (ERTM) imaging based on the optical flow vector traveling-wave separation. We utilize a layered model and the BP model to test our method. The testing results demonstrate that the optical flow vector can overcome the Poynting vector limitations and get more accurate and reliable information regarding the direction of elastic wave propagation in TI media, as well as precisely separate the wavefields. The separated wavefields for migration effectively improve the quality of the ERTM.","PeriodicalId":509604,"journal":{"name":"GEOPHYSICS","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2024-04-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"GEOPHYSICS","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1190/geo2023-0231.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The propagation direction of the wavefield is particularly important for migration imaging in the reverse-time migration (RTM) of elastic waves in TI media. However, due to the problem of computational instability of the Poynting vector, the wave field propagation direction estimated based on the Poynting vector method has errors and cannot accurately indicate the real propagation direction of the elastic wavefield. To solve this problem, a method for calculating the optical flow vector of elastic waves in TI media is proposed to obtain the propagation direction. The optical flow vector of elastic waves in TI media is determined by applying the spatial and temporal derivatives of the wavefield at each time step, under the assumption that the wavefields are almost the same at subsequent time steps and are smooth in the spatial direction. As the additional smoothing item is added and the multiple iterative algorithm is introduced in calculating the optical flow vector, the direction is calculated more accurately than the Poynting vector. Based on the optical flow vectors, we can separate the source-wavefield and receiver-wavefield into four directions: up-going, down-going, left-going and right-going wavefields, respectively, and finally perform elastic reverse-time migration (ERTM) imaging based on the optical flow vector traveling-wave separation. We utilize a layered model and the BP model to test our method. The testing results demonstrate that the optical flow vector can overcome the Poynting vector limitations and get more accurate and reliable information regarding the direction of elastic wave propagation in TI media, as well as precisely separate the wavefields. The separated wavefields for migration effectively improve the quality of the ERTM.
波场的传播方向对于 TI 介质中弹性波的反向时间迁移(RTM)中的迁移成像尤为重要。然而,由于 Poynting 向量的计算不稳定性问题,基于 Poynting 向量方法估算的波场传播方向存在误差,无法准确指示弹性波场的真实传播方向。为解决这一问题,提出了一种计算 TI 介质中弹性波光流矢量的方法,以获得传播方向。TI 介质中弹性波的光流矢量是在假定后续时间步的波场几乎相同且在空间方向上平滑的前提下,通过应用每个时间步的波场的空间和时间导数确定的。由于在计算光流矢量时增加了额外的平滑项并引入了多重迭代算法,因此方向的计算比波因廷矢量更精确。根据光流矢量,我们可以将源波场和接收波场分别分离为四个方向:上行波场、下行波场、左行波场和右行波场,最后根据光流矢量行波分离进行弹性反向时间迁移(ERTM)成像。我们利用分层模型和 BP 模型来测试我们的方法。测试结果表明,光流矢量可以克服 Poynting 向量的限制,获得更准确可靠的 TI 介质中弹性波传播方向的信息,并精确分离波场。用于迁移的分离波场可有效提高 ERTM 的质量。