Seismic wavefield modelling in two-phase media including undulating topography with the modified Biot/squirt model by a curvilinear-grid finite difference method

被引:2
|
作者
Yang, Shang-bei [1 ]
Bai, Chao-ying [1 ,2 ]
Greenhalgh, Stewart [3 ]
机构
[1] Changan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
[2] Changan Univ, Inst Computat Geophys, Xian 710054, Shaanxi, Peoples R China
[3] King Fahd Univ Petr & Minerals, Dept Geosci, Dhahran 31261, Saudi Arabia
基金
美国国家科学基金会;
关键词
Seismics; Wave; Modelling; ELASTIC-WAVES; PROPAGATION; VELOCITY; ATTENUATION; DISPERSION; SCHEMES; SQUIRT; BIOT;
D O I
10.1111/1365-2478.12844
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
In this paper, we deduced the corresponding first-order velocity-stress equation for curvilinear coordinates from the first-order velocity-stress equation based on the modified Biot/squirt model for a two-dimensional two-phase medium. The equations are then numerically solved by an optimized high-order non-staggered finite difference scheme, that is, the dispersion relation preserving/optimization MacCormack scheme. To implement undulating free-surface topography, we derive an analytical relationship between the derivatives of the particle velocity components and use the compact finite-difference scheme plus a traction-image method. In the undulating free surface and the undulating subsurface interface of two-phase medium, the complex reflected wave and transmitted wave can be clearly recognized in the numerical simulation results. The simulation results show that the curvilinear-grid finite-difference method, which uses a body-conforming grid to describe the undulating surface, can accurately reduce the numerical scattering effect of seismic wave propagation caused by the use of ladder-shaped grid to fit the surfaces when undulating topography is present in a two-phase isotropic medium.
引用
收藏
页码:591 / 614
页数:24
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