A discontinuous-grid finite-difference scheme for frequency-domain 2D scalar wave modeling

被引:14
|
作者
Fan, Na [1 ,2 ]
Zhao, Lian-Feng [3 ]
Xie, Xiao-Bi [4 ]
Yao, Zhen-Xing [3 ]
机构
[1] Yangtze Univ, Sch Geophys & Oil Resources, Key Lab Explorat Technol Oil & Gas Resources, Minist Educ, Wuhan, Hubei, Peoples R China
[2] Hubei Cooperat Innovat Ctr Unconvent Oil & Gas, Wuhan, Hubei, Peoples R China
[3] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China
[4] Univ Calif Santa Cruz, Inst Geophys & Planetary Phys, Santa Cruz, CA 95064 USA
基金
中国国家自然科学基金;
关键词
AVERAGE-DERIVATIVE METHOD; FORM INVERSION; TIME-STEPS; DIRECT SOLVER; EQUATION; SIMULATION; PROPAGATION; MIGRATION; OPERATORS; SPACE;
D O I
10.1190/GEO2017-0535.1
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
The discontinuous-grid method can greatly reduce the storage requirement and computational cost in finite-difference modeling, especially for models with large velocity contrasts. However, this technique is mostly applied to time-domain methods. We have developed a discontinuous-grid finite-difference scheme for frequency-domain 2D scalar wave modeling. Special frequency-domain finite-difference stencils are designed in the fine-coarse grid transition zone. The coarse-to-fine-grid spacing ratio is restricted to 2(n), where n is a positive integer. Optimization equations are formulated to obtain expansion coefficients for irregular stencils in the transition zone. The proposed method works well when teamed with commonly used 9- and 25-point schemes. Compared with the conventional frequency-domain finite-difference method, the proposed discontinuous-grid method can largely reduce the size of the impedance matrix and number of nonzero elements. Numerical experiments demonstrated that the proposed discontinuous-grid scheme can significantly reduce memory and computational costs, while still yielding almost identical results compared with those from conventional uniform-grid simulations. When tested for a very long elapsed time, the frequency-domain discontinuous-grid method does not show instability problems as its time-domain counterpart usually does.
引用
收藏
页码:T235 / T244
页数:10
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