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基于最优输运原理的陆上单分量资料弹性波全波形反演 被引量:3

Elastic full-waveform inversion of land single-component seismic data based on optimal transport theory
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摘要 陆上地震单分量地震数据只包含纵波信息,没有横波信号。声波全波形反演是最常用的利用纵波数据反演地下纵波速度、密度的方法,但忽略了单分量资料的弹性AVO特征和转换纵波的存在。为此,基于弹性介质假设推导了伪压力弹性波方程,该方程数值模拟结果仍为标量波信号,但具备弹性AVO特征和转换纵波信息,能够指示横波速度的变化。在此基础上构建了利用纵波数据进行弹性参数全波形反演的理论框架。由于全波形反演的高度非线性,准确的初始速度建模尤为重要,引入基于最优输运理论的二次Wasserstein距离(W2范数),在不增加计算量的前提下优化了目标函数的凸性,克服了周期性跳跃导致的局部极值问题。在此基础上,再进行常规的基于L_(2)范数反演,克服了对初始模型的依赖。应用重采样的Marmousi模型验证了该方法仅用纵波数据反演纵、横波速度的有效性,以及避免周期性跳跃方面的优势。将该方法应用于中国东部M工区的实际地震资料,验证了该方法的实用性和稳定性。 The single-component seismic data collected from land only contains P-wave information without S-wave.Acoustic full-waveform inversion(AFWI)is the most commonly used method to invert the P-wave velocity and density with P-wave data.However,it ignores the elastic AVO characteristics of single-component data and the existence of converted P-waves.To tackle this problem,this paper derives a new pseudo-pressure elastic wave equation based on the elastic medium assumption.The numerical simulation result of the equation is still a scalar wavefield but contains elastic AVO characteristics and converted P-wave information,which indicates the change of S-wave velocity.Then we build a theoretical framework of full-waveform inversion(FWI)to invert elastic para-meters using P-wave data.Besides,due to the high non-linearity of the FWI,modeling accurate initial velocity is crucial.In view of this,we introduce the quadratic Wasserstein distance(W2-norm)based on the optimal transport theory to optimize the convexity of objective function and overcomes the local minima caused by periodic skipping without increasing calculations.On this basis,the conventional L_(2)-norm inversion(W2+L_(2) inversion)is carried out,which eliminates the dependence on the initial model.The test using the Marmousi model after resampling verifies the effectiveness of the method in inverting P/S-wave velocities with only P-wave data,as well as its advantages in avoiding periodic skipping.Finally,this method is applied to actual seismic data of Area M in eastern China,and the inversion results illustrate the practicability and stability of the proposed method.
作者 李青阳 吴国忱 王玉梅 慎国强 段沛然 LI Qingyang;WU Guochen;WANG Yumei;SHEN Guoqiang;DUAN Peiran(School of Geosciences,China University of Petroleum(East China),Qingdao,Shandong 266580,China;Laboratory for Marine Mineral Resources,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao,Shandong 266071,China;Geophysical Research Institute of Shengli Oilfield,SINOPEC,Dongying,Shandong 257022,China)
出处 《石油地球物理勘探》 EI CSCD 北大核心 2021年第5期1060-1073,I0011,I0012,共16页 Oil Geophysical Prospecting
关键词 陆上单分量地震数据 伪压力弹性波方程 二次Wasserstein距离 全波形反演 纵横波速度 land single-component seismic data pseudo-pressure elastic wave equation quadratic Wasserstein distance full-waveform inversion P/S-wave velocities
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