Advanced three-dimensional electromagnetic modelling using a nested integral equation approach

被引:17
作者
Chen, Chaojian [1 ]
Kruglyakov, Mikhail [1 ,2 ,3 ]
Kuvshinov, Alexey [1 ]
机构
[1] Swiss Fed Inst Technol, Inst Geophys, CH-8092 Zurich, Switzerland
[2] Inst Phys Earth, Geoelectromagnet Res Ctr, Moscow 108840, Russia
[3] Univ Otago, Dept Phys, Dunedin 9016, New Zealand
关键词
Electromagnetic theory; Geomagnetic induction; Magnetotellurics; Numerical modelling; INDUCTION LOGGING PROBLEMS; 3D; EM; FIELDS; SOLVER; DECOMPOSITION; CONDUCTIVITY;
D O I
10.1093/gji/ggab072
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
Most of the existing 3-D electromagnetic (EM) modelling solvers based on the integral equation (IE) method exploit fast Fourier transform (FFT) to accelerate the matrix-vector multiplications. This in turn requires a laterally uniform discretization of the modelling domain. However, there is often a need for multiscale modelling and inversion, for instance, to properly account for the effects of non-uniform distant structures and, at the same time, to accurately model the effects from local anomalies. In such scenarios, the usage of laterally uniform grids leads to excessive computational loads, in terms of both memory and time. To alleviate this problem, we developed an efficient 3-D EM modelling tool based on a multinested IE approach. Within this approach, the IE modelling is first performed at a large domain and on a (laterally uniform) coarse grid, and then the results are refined in the region of interest by performing modelling at a smaller domain and on a (laterally uniform) denser grid. At the latter stage, the modelling results obtained at the previous stage are exploited. The lateral uniformity of the grids at each stage allows us to keep using the FFT for the acceleration of matrix-vector multiplications. An important novelty of the paper is the development of a 'rim domain' concept that further improves the performance of the multinested IE approach. We verify the developed tool on both idealized and realistic 3-D conductivity models, and demonstrate its efficiency and accuracy.
引用
收藏
页码:114 / 130
页数:17
相关论文
共 54 条
[1]  
[Anonymous], 2010, DATA SCI J
[2]  
[Anonymous], 2005, Fast multipole methods for the Helmholtz equation in three dimensions
[3]  
[Anonymous], 2012, MAGNETOTELLURIC METH, DOI DOI 10.1017/CBO9781139020138
[4]   Three-dimensional induction logging problems, Part I: An integral equation solution and model comparisons [J].
Avdeev, DB ;
Kuvshinov, AV ;
Pankratov, OV ;
Newman, GA .
GEOPHYSICS, 2002, 67 (02) :413-426
[5]  
Avdeev DB, 2002, IZV-PHYS SOLID EART+, V38, P975
[6]   High-performance three-dimensional electromagnetic modelling using modified Neumann series. Wide-band numerical solution and examples [J].
Avdeev, DB ;
Kuvshinov, AV ;
Pankratov, OV ;
Newman, GA .
JOURNAL OF GEOMAGNETISM AND GEOELECTRICITY, 1997, 49 (11-12) :1519-1539
[7]   GOEMAGNETIC VARIATIONS AND ELECTRICAL CONDUCTIVITY OF UPPER MANTLE [J].
BANKS, RJ .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1969, 17 (05) :457-&
[8]   Global Bathymetry and Elevation Data at 30 Arc Seconds Resolution: SRTM30_PLUS [J].
Becker, J. J. ;
Sandwell, D. T. ;
Smith, W. H. F. ;
Braud, J. ;
Binder, B. ;
Depner, J. ;
Fabre, D. ;
Factor, J. ;
Ingalls, S. ;
Kim, S-H. ;
Ladner, R. ;
Marks, K. ;
Nelson, S. ;
Pharaoh, A. ;
Trimmer, R. ;
Von Rosenberg, J. ;
Wallace, G. ;
Weatherall, P. .
MARINE GEODESY, 2009, 32 (04) :355-371
[9]  
Bohlander Jennifer., 2007, Antarctic coastlines and grounding line derived from MODIS Mosaic of Antarctica (MOA), National Snow and Ice Data Center
[10]   SINGULAR VALUE DECOMPOSITION OF INTEGRAL-EQUATIONS OF EM AND APPLICATIONS TO THE CAVITY RESONANCE PROBLEM [J].
CANNING, FX .
IEEE TRANSACTIONS ON ANTENNAS AND PROPAGATION, 1989, 37 (09) :1156-1163