The optimized gradient method for full waveform inversion and its spectral implementation

被引:17
作者
Wu, Zedong [1 ]
Alkhalifah, Tariq [1 ]
机构
[1] King Abdullah Univ Sci & Technol, Seism Wave Anal Grp, Thuwal 239556900, Saudi Arabia
关键词
Numerical solutions; Fourier analysis; Inverse theory; Tomography; Wave propagation; REVERSE-TIME MIGRATION; EXTRAPOLATION; APPROXIMATION;
D O I
10.1093/gji/ggw112
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
At the heart of the full waveform inversion (FWI) implementation is wavefield extrapolation, and specifically its accuracy and cost. To obtain accurate, dispersion free wavefields, the extrapolation for modelling is often expensive. Combining an efficient extrapolation with a novel gradient preconditioning can render an FWI implementation that efficiently converges to an accurate model. We, specifically, recast the extrapolation part of the inversion in terms of its spectral components for both data and gradient calculation. This admits dispersion free wavefields even at large extrapolation time steps, which improves the efficiency of the inversion. An alternative spectral representation of the depth axis in terms of sine functions allows us to impose a free surface boundary condition, which reflects our medium boundaries more accurately. Using a newly derived perfectly matched layer formulation for this spectral implementation, we can define a finite model with absorbing boundaries. In order to reduce the nonlinearity in FWI, we propose a multiscale conditioning of the objective function through combining the different directional components of the gradient to optimally update the velocity. Through solving a simple optimization problem, it specifically admits the smoothest approximate update while guaranteeing its ascending direction. An application to the Marmousi model demonstrates the capability of the proposed approach and justifies our assertions with respect to cost and convergence.
引用
收藏
页码:1823 / 1831
页数:9
相关论文
共 23 条
[2]   A PERFECTLY MATCHED LAYER FOR THE ABSORPTION OF ELECTROMAGNETIC-WAVES [J].
BERENGER, JP .
JOURNAL OF COMPUTATIONAL PHYSICS, 1994, 114 (02) :185-200
[3]   MULTISCALE SEISMIC WAVE-FORM INVERSION [J].
BUNKS, C ;
SALECK, FM ;
ZALESKI, S ;
CHAVENT, G .
GEOPHYSICS, 1995, 60 (05) :1457-1473
[4]  
Chu CL, 2011, GEOPHYSICS, V76, pT113, DOI [10.1190/GEO2011-0069.1, 10.1190/geo2011-0069.1]
[5]  
Etgen J.T., 2009, SEG Expanded Abstracts, V28, P2552, DOI DOI 10.1190/1.3255375
[6]  
Fomel S., 2010, SEG Technical Program Expanded Abstracts, V29, P3092
[7]   WAVE-FIELD TRANSFORMATIONS OF VERTICAL SEISMIC PROFILES [J].
HU, LZ ;
MCMECHAN, GA .
GEOPHYSICS, 1987, 52 (03) :307-321
[8]   TOMP - FORTRAN MODULES FOR OPTIMAL-CONTROL CALCULATIONS [J].
KRAFT, D .
ACM TRANSACTIONS ON MATHEMATICAL SOFTWARE, 1994, 20 (03) :262-281
[9]   An effective imaging condition for reverse-time migration using wavefield decomposition [J].
Liu, Faqi ;
Zhang, Guanquan ;
Morton, Scott A. ;
Leveille, Jacques P. .
GEOPHYSICS, 2011, 76 (01) :S29-S39
[10]   An explicit time evolution method for acoustic wave propagation [J].
Liu, Huafeng ;
Dai, Nanxun ;
Niu, Fenglin ;
Wu, Wei .
GEOPHYSICS, 2014, 79 (03) :T117-T124