A multigrid integral equation method for large-scale models with inhomogeneous backgrounds

被引:18
作者
Endo, Masashi [1 ]
Cuma, Martin [1 ]
Zhdanov, Michael S. [1 ]
机构
[1] Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA
关键词
multigrid; integral equation method; large-scale; inhomogeneous background conductivity;
D O I
10.1088/1742-2132/5/4/007
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
We present a multigrid integral equation (IE) method for three-dimensional (3D) electromagnetic ( EM) field computations in large-scale models with inhomogeneous background conductivity (IBC). This method combines the advantages of the iterative IBC IE method and the multigrid quasi-linear (MGQL) approximation. The new EM modelling method solves the corresponding systems of linear equations within the domains of anomalous conductivity, D(a), and inhomogeneous background conductivity, D(b), separately on coarse grids. The observed EM fields in the receivers are computed using grids with fine discretization. The developed MGQL IBC IE method can also be applied iteratively by taking into account the return effect of the anomalous field inside the domain of the background inhomogeneity Db, and vice versa. The iterative process described above is continued until we reach the required accuracy of the EM field calculations in both domains, D(a) and D(b). The method was tested for modelling the marine controlled-source electromagnetic field for complex geoelectrical structures with hydrocarbon petroleum reservoirs and a rough sea-bottom bathymetry.
引用
收藏
页码:438 / 447
页数:10
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