Three-dimensional massively parallel electromagnetic inversion .1. Theory

被引:144
作者
Newman, GA
Alumbaugh, DL
机构
[1] Geophysics Department, Sandia National Laboratories, Albuquerque, NM 87185-0750
关键词
electromagnetic modelling; inversion; tomography;
D O I
10.1111/j.1365-246X.1997.tb01559.x
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
An iterative solution to the non-linear 3-D electromagnetic inverse problem is obtained by successive linearized model updates using the method of conjugate gradients. Full wave equation modelling for controlled sources is employed to compute model sensitivities and predicted data in the frequency domain with an efficient 3-D finite-difference algorithm. Necessity dictates that the inverse be underdetermined, since realistic reconstructions require the solution for tens of thousands of parameters. In addition, large-scale 3-D forward modelling is required and this can easily involve the solution of over several million electric field unknowns per solve. A massively parallel computing platform has therefore been utilized to obtain reasonable execution times, and results are given for the 1840-node Intel Paragon. The solution is demonstrated with a synthetic example with added Gaussian noise, where the data were produced from an integral equation forward-modelling code, and is different from the finite difference code embedded in the inversion algorithm.
引用
收藏
页码:345 / 354
页数:12
相关论文
共 17 条
[1]   Three-dimensional massively parallel electromagnetic inversion .2. Analysis of a crosswell electromagnetic experiment [J].
Alumbaugh, DL ;
Newman, GA .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1997, 128 (02) :355-363
[2]   Three-dimensional wideband electromagnetic modeling on massively parallel computers [J].
Alumbaugh, DL ;
Newman, GA ;
Prevost, L ;
Shadid, JN .
RADIO SCIENCE, 1996, 31 (01) :1-23
[3]   Approximate sensitivities for the electromagnetic inverse problem [J].
Farquharson, CG ;
Oldenburg, DW .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1996, 126 (01) :235-252
[4]  
GROPP W, 1995, USING MPI PORTABLE P
[5]  
HABASHY TM, 1995, INT S 3 DIM EL
[6]   METHODS OF CONJUGATE GRADIENTS FOR SOLVING LINEAR SYSTEMS [J].
HESTENES, MR ;
STIEFEL, E .
JOURNAL OF RESEARCH OF THE NATIONAL BUREAU OF STANDARDS, 1952, 49 (06) :409-436
[7]   3-DIMENSIONAL MAGNETOTELLURIC INVERSION USING CONJUGATE GRADIENTS [J].
MACKIE, RL ;
MADDEN, TR .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1993, 115 (01) :215-229
[8]   METHODS FOR CALCULATING FRECHET DERIVATIVES AND SENSITIVITIES FOR THE NONLINEAR INVERSE PROBLEM - A COMPARATIVE-STUDY [J].
MCGILLIVRAY, PR ;
OLDENBURG, DW .
GEOPHYSICAL PROSPECTING, 1990, 38 (05) :499-524
[9]  
Menke W., 1984, GEOPHYSICAL DATA ANA
[10]   TRANSIENT ELECTROMAGNETIC RESPONSE OF A 3-DIMENSIONAL BODY IN A LAYERED EARTH [J].
NEWMAN, GA ;
HOHMANN, GW ;
ANDERSON, WL .
GEOPHYSICS, 1986, 51 (08) :1608-1627