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基于变差分系数的变网格弹性波全波形反演

张红静 贺慧丽 孙文博 孙鹏远 李红辉 周辉

石油地球物理勘探2024,Vol.59Issue(3):514-522,9.
石油地球物理勘探2024,Vol.59Issue(3):514-522,9.DOI:10.13810/j.cnki.issn.1000-7210.2024.03.014

基于变差分系数的变网格弹性波全波形反演

Full-waveform inversion of elastic waves in variable grids based on variable difference coefficients

张红静 1贺慧丽 2孙文博 3孙鹏远 2李红辉 2周辉4

作者信息

  • 1. 东华理工大学核资源与环境国家重点实验室,江西南昌 330013||东华理工大学地球物理与测控技术学院,江西南昌 330013
  • 2. 东方地球物理公司物探技术研究中心,河北涿州 072751
  • 3. 中海油研究总院有限责任公司勘探开发研究院,北京 100028||海洋油气勘探国家工程研究中心,北京 100028
  • 4. 中国石油大学(北京)油气资源与工程全国重点实验室,北京 102249||中国石油大学(北京)CNPC物探重点实验室,北京 102249||中国石油大学(北京)地球物理学院,北京 102249
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摘要

Abstract

Full-waveform inversion fully utilizes all the information of seismic wave propagation,including am-plitude,phase,and travel time,which can obtain inversion results with higher resolution and accuracy com-pared with travel time tomography.When the velocity in the shallow layer of the medium is low,fine grids are usually used to sample the low-velocity layer,so as to ensure the accuracy of forward modeling.However,sub-dividing the entire model into finer grids will increase computational complexity and storage requirements,and oversampling will occur in the high-velocity regions of the model.These problems are further amplified in the process of full-waveform inversion.To address these issues,this study introduced a finite difference forward modeling method of the elastic wave equation in variable grids based on variable difference coefficients.Firstly,the difference coefficient of variable grid wave field simulation was derived based on Taylor expansion,and the variable grid wave field simulation was realized.Secondly,the forward modeling method of variable difference coefficients was applied to the forward modeling,residual backpropagation,and wave field reconstruction of the full-waveform inversion,and the full-waveform inversion of elastic waves in variable grids based on the variable difference coefficient was realized.In the full-waveform inversion,the multi-scale inversion strategy and the conventional conjugate gradient method were used for the iterative solution.The fine grids were used to divide shallow low-velocity layers,and coarser grids were used to divide the middle and deep layers with high ve-locity,which ensured the accuracy of inversion for the shallow layers while avoiding oversampling in the middle and deep layers.The inversion results of the model data demonstrate that the full-waveform inversion in variable grids based on variable difference coefficients can effectively characterize the low-velocity anomalies compared with full-waveform inversion in uniform coarse grids.The test of noisy data shows that the proposed full-waveform inversion method has strong noise resistance.

关键词

弹性波/全波形反演/变差分系数/变网格正演/有限差分

Key words

elastic wave/full-waveform inversion/variational difference coefficient/forward modeling of variable grids/finite difference

分类

天文与地球科学

引用本文复制引用

张红静,贺慧丽,孙文博,孙鹏远,李红辉,周辉..基于变差分系数的变网格弹性波全波形反演[J].石油地球物理勘探,2024,59(3):514-522,9.

基金项目

本项研究受核资源与环境国家重点实验室开放基金项目"井震结合下基于谱蓝化—有色反演的松辽盆地南部姚家组砂岩型铀矿预测方法研究"(2022NRE16)、东华理工大学博士科研启动基金项目"可控震源扫描技术及高阶谐波消除方法研究"(DHBK2019083)和中国石油天然气集团公司前瞻性基础性项目"物探岩石物理与前沿储备技术研究"(2021DJ3506)联合资助. (2022NRE16)

石油地球物理勘探

OA北大核心CSTPCD

1000-7210

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