Simulation of seismoelectric waves using finite-difference frequency-domain method: 2-D SHTE mode

被引:28
|
作者
Gao, Yongxin [1 ]
Wang, Dongdong [1 ]
Yao, Cheng [1 ]
Guan, Wei [2 ]
Hu, Hengshan [2 ]
Wen, Jian [3 ,4 ]
Zhang, Wei [5 ]
Tong, Ping [6 ,7 ]
Yang, Qingjie [8 ,9 ]
机构
[1] Hefei Univ Technol, Sch Civil Engn, Hefei 230009, Anhui, Peoples R China
[2] Harbin Inst Technol, Dept Astronaut & Mech, Harbin, Heilongjiang, Peoples R China
[3] Univ Sci & Technol China, Lab Seismol & Phys Earths Interior, Hefei 230026, Anhui, Peoples R China
[4] Univ Sci & Technol China, Sch Earth & Space Sci, Hefei 230026, Anhui, Peoples R China
[5] Southern Univ Sci & Technol, Sch Earth & Space Sci, Shenzhen 518055, Peoples R China
[6] Nanyang Technol Univ, Sch Phys & Math Sci, Div Math Sci, Singapore, Singapore
[7] Nanyang Technol Univ, Asian Sch Environm, Singapore, Singapore
[8] Chinese Acad Sci, Inst Geodesy & Geophys, Ctr Computat & Explorat Geophys, 340 Xudong Rd, Wuhan 430077, Hubei, Peoples R China
[9] State Key Lab Geodesy & Earths Dynam, 340 Xudong Rd, Wuhan 430077, Hubei, Peoples R China
基金
中国国家自然科学基金;
关键词
Electrical properties; Electromagnetic theory; Numerical modelling; Body waves; Interface wave; Wave propagation; EARLY ELECTROMAGNETIC-WAVES; POROUS-MEDIA; FIELD-MEASUREMENTS; ELASTIC WAVES; SOIL TEXTURES; ROCK SAMPLES; FLUID; CONVERSIONS; PROPAGATION; EQUATIONS;
D O I
10.1093/gji/ggy433
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 develop a finite-difference frequency-domain (FDFD) method to simulate the 2-D SHTE-mode seismoelectric waves. The method approximates the spatial derivatives and non-derivative terms of the wave equations using the weighted-averaging finite-difference operators in a 25-point computational stencil. To suppress the reflections of the seismic and EM waves from the truncated boundaries, we apply the perfectly matched layers (PMLs) surrounding the interior modelled area to absorb the seismic waves, and add several additional layers out of the PMLs to absorb the EM waves. We validate the FDFD method by comparing the FDFD solutions in a two-layer model with the solutions from an analytically-based method. The results show that the FDFD solutions agree excellently with analytical solutions in both the seismic and EM signals, proving that the FDFD method is an efficient and powerful tool in modelling the seismoelectric waves. The FDFD method proposed in this paper requires no quasi-static approximation, and thus can be used to accurately model and interpret the seismoelectric responses in a complex stratum.
引用
收藏
页码:414 / 438
页数:25
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