A sliced-3D approach to finite-difference time-domain modeling by optimizing perfectly matched layers

被引:0
|
作者
Delf, Richard [1 ]
Giannopoulos, Antonios [2 ]
Bingham, Robert G. [1 ]
Curtis, Andrew [1 ]
机构
[1] Univ Edinburgh, Sch GeoSci, Edinburgh EH8 9XP, Midlothian, Scotland
[2] Univ Edinburgh, Sch Engn, Edinburgh EH9 3JL, Midlothian, Scotland
基金
英国自然环境研究理事会;
关键词
WAVE-FORM INVERSION; FREQUENCY-SHIFTED PML; MIGRATION; IMPLEMENTATION; PROPAGATION; ANTARCTICA;
D O I
10.1190/GEO2020-0222.1
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
Finite-difference time-domain forward modeling is often used to gain a more quantitative understanding of the interactions between electromagnetic fields and targets. To undertake full 3D simulations, the computational demands are challenging, so simulations are often undertaken in two dimensions, in which assumptions in the propagation of electromagnetic fields and source type can result in errors. We have developed the concept of a sliced-3D simulation, wherein a thin slice of a 3D domain with strictly 2D geometry is used to minimize computational demands while obtaining synthetic waveforms that contain full 3D propagation effects. This approach requires optimization of perfectly matched layer (PML) boundary condition parameters so as to minimize the errors associated with the source being located close to the boundary, and as a result of grazing-incident angle wave conversion to evanescent energy. We explore the frequency dependence of PML parameters, and we establish a relationship between complex frequency stretching parameters and effective wavelength. The resultant parameter choice is shown to minimize propagation errors in the context of a simple radioglaciological model, in which 3D domains may be prohibitively large. and for a near-surface cross-borehole survey configuration. a case in which full-waveform inversion may typically be used.
引用
收藏
页码:H43 / H52
页数:10
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