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
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Changan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R ChinaChangan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
Yang, Shang-bei
[1
]
Bai, Chao-ying
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机构:
Changan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
Changan Univ, Inst Computat Geophys, Xian 710054, Shaanxi, Peoples R ChinaChangan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
Bai, Chao-ying
[1
,2
]
Greenhalgh, Stewart
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机构:
King Fahd Univ Petr & Minerals, Dept Geosci, Dhahran 31261, Saudi ArabiaChangan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
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
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.
机构:
Changan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R ChinaChangan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
Yang ShangBei
Bai ChaoYing
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机构:
Changan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
Changan Univ, Inst Computat Geophys, Xian 710054, Shaanxi, Peoples R ChinaChangan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
Bai ChaoYing
Zhou Bing
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机构:
Khalifa Univ Sci & Technol, Petr Inst, POB 2533, Abu Dhabi, U Arab EmiratesChangan Univ, Sch Geol Engn & Geomat, Dept Geophys, Xian 710054, Shaanxi, Peoples R China
Zhou Bing
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,
2018,
61
(08):
: 3356
-
3373