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

Author:

Fan Na1ORCID,Zhao Lian-Feng2,Xie Xiao-Bi3,Yao Zhen-Xing2

Affiliation:

1. Yangtze University, School of Geophysics and Oil Resources, Key Laboratory of Exploration Technologies for Oil and Gas Resources of Ministry of Education, Wuhan, China and Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Wuhan, China..

2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Key Laboratory of Earth and Planetary Physics, Beijing, China..

3. University of California at Santa Cruz, Institute of Geophysics and Planetary Physics, Santa Cruz, California, USA..

Abstract

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 [Formula: see text], where [Formula: see text] 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.

Funder

National Natural Science Foundation of China

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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