Regularized seismic full waveform inversion with prior model information

被引:135
作者
Asnaashari, Amir [1 ,4 ]
Brossier, Romain [2 ,4 ]
Garambois, Stephane [3 ,4 ]
Audebert, Francois [5 ]
Thore, Pierre [6 ]
Virieux, Jean [3 ,4 ]
机构
[1] Univ Grenoble 1, Inst Earth Sci, Grenoble, France
[2] Univ Grenoble 1, Dept Earth Sci, Grenoble, France
[3] Univ Grenoble 1, Grenoble, France
[4] CNRS, Inst Sci Terre ISTerre, Grenoble, France
[5] TOTAL E&P CSTJF, Pau, France
[6] TOTAL E&P, Geosci Res Ctr, Aberdeen, Scotland
关键词
CONTRAST-SOURCE INVERSION; FREQUENCY-DOMAIN; TOMOGRAPHY; ALGORITHMS;
D O I
10.1190/GEO2012-0104.1
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
Full waveform inversion (FWI) delivers high-resolution quantitative images and is a promising technique to obtain macroscale physical property model of the subsurface. In most geophysical applications, prior information, such as that collected in wells, is available and should be used to increase the image reliability. For this, we propose to introduce three terms in the definition of the FWI misfit function: the data misfit itself, the first-order Tikhonov regularization term acting as a smoothing operator, and a prior model norm term. This last term is the way to smoothly introduce prior information into the FWI workflow. On a selected target of the Marmousi synthetic example, significant improvement was obtained when using the prior model term for noise-free and noisy synthetic data. The prior model term may significantly reduce the inversion sensitivity to incorrect initial conditions. The limited range of spatial wavenumber sampling by the acquisition may be compensated with the prior model information, for multiple-free and multiple-contaminated data. Prior and initial models play different roles in the inversion scheme. The starting model is used for wave propagation and therefore drives the data-misfit gradient, whereas the prior model is never explicitly used for solving the wave equation and only drives the optimization step as an additional constraint to minimize the total objective function. Thus, the prior model is not required to follow kinematic properties as precisely as the initial model, except in zones of poor illumination. In addition, we investigate the influence of a simple dynamic decreasing weighting of the prior model term. Once the cycle-skipping problem has been solved, the impact of the prior model term is gradually reduced within the misfit function to be driven by seismic-data only.
引用
收藏
页码:R25 / R36
页数:12
相关论文
共 39 条
[1]   Application of the finite-difference contrast-source inversion algorithm to seismic full-waveform data [J].
Abubakar, Aria ;
Hu, Wenyi ;
Habashy, Tarek M. ;
van den Berg, Peter M. .
GEOPHYSICS, 2009, 74 (06) :WCC47-WCC58
[2]  
[Anonymous], 1979, SIAM REV, DOI DOI 10.1137/1021044
[3]   A PERFECTLY MATCHED LAYER FOR THE ABSORPTION OF ELECTROMAGNETIC-WAVES [J].
BERENGER, JP .
JOURNAL OF COMPUTATIONAL PHYSICS, 1994, 114 (02) :185-200
[4]   Seismic imaging of complex onshore structures by 2D elastic frequency-domain full-waveform inversion [J].
Brossier, Romain ;
Operto, Stephane ;
Virieux, Jean .
GEOPHYSICS, 2009, 74 (06) :WCC105-WCC118
[5]   MULTISCALE SEISMIC WAVE-FORM INVERSION [J].
BUNKS, C ;
SALECK, FM ;
ZALESKI, S ;
CHAVENT, G .
GEOPHYSICS, 1995, 60 (05) :1457-1473
[6]   A LIMITED MEMORY ALGORITHM FOR BOUND CONSTRAINED OPTIMIZATION [J].
BYRD, RH ;
LU, PH ;
NOCEDAL, J ;
ZHU, CY .
SIAM JOURNAL ON SCIENTIFIC COMPUTING, 1995, 16 (05) :1190-1208
[7]  
Cohen J. K., 2008, CWPSU
[8]   Non-linear inversion using general measures of data misfit and model structure [J].
Farquharson, CG ;
Oldenburg, DW .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1998, 134 (01) :213-227
[9]   Full waveform tomography for radially anisotropic structure: New insights into present and past states of the Australasian upper mantle [J].
Fichtner, Andreas ;
Kennett, Brian L. N. ;
Igel, Heiner ;
Bunge, Hans-Peter .
EARTH AND PLANETARY SCIENCE LETTERS, 2010, 290 (3-4) :270-280
[10]   Solutions, algorithms and inter-relations for local minimization search geophysical inversion [J].
Greenhalgh, Stewart A. ;
Bing, Zhou ;
Green, Alan .
JOURNAL OF GEOPHYSICS AND ENGINEERING, 2006, 3 (02) :101-113