An optimal 9-point, finite-difference, frequency-space, 2-D scalar wave extrapolator

被引:357
作者
Jo, CH [1 ]
Shin, CS [1 ]
Suh, JH [1 ]
机构
[1] SEOUL NATL UNIV,DEPT PETR & MINERAL ENGN,SEOUL 151742,SOUTH KOREA
关键词
D O I
10.1190/1.1443979
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 study, a new finite-difference technique is designed to reduce the number of grid points needed in frequency-space domain modeling. The new algorithm uses optimal nine-point operators for the approximation of the Laplacian and the mass acceleration terms. The coefficients can be found by using the steepest descent method so that the best normalized phase curves can be obtained. This method reduces the number of grid points per wavelength to 4 or less, with consequent reductions of computer memory and CPU time that are factors of tens less than those involved in the conventional second order approximation formula when a band type solver is used on a scalar machine.
引用
收藏
页码:529 / 537
页数:9
相关论文
共 13 条
[1]   ACCURACY OF FINITE-DIFFERENCE MODELING OF ACOUSTIC-WAVE EQUATION [J].
ALFORD, RM ;
KELLY, KR ;
BOORE, DM .
GEOPHYSICS, 1974, 39 (06) :834-842
[2]  
Conte Samuel Daniel, 2017, Elementary Numerical Analysis, An Algorithmic Approach
[3]   THE APPLICATION OF HIGH-ORDER DIFFERENCING TO THE SCALAR WAVE-EQUATION [J].
DABLAIN, MA .
GEOPHYSICS, 1986, 51 (01) :54-66
[4]  
GEORGE A, 1981, COMPUTER SOLUTION LA
[5]   COMPUTATIONAL ASPECTS OF THE CHOICE OF OPERATOR AND SAMPLING INTERVAL FOR NUMERICAL DIFFERENTIATION IN LARGE-SCALE SIMULATION OF WAVE PHENOMENA [J].
HOLBERG, O .
GEOPHYSICAL PROSPECTING, 1987, 35 (06) :629-655
[6]   FORWARD MODELING BY A FOURIER METHOD [J].
KOSLOFF, DD ;
BAYSAL, E .
GEOPHYSICS, 1982, 47 (10) :1402-1412
[7]  
Lysmer J., 1972, Methods Comput. Phys, V11, P181, DOI [DOI 10.1016/B978-0-12-460811-5.50009-X, 10.1016/B978-0-12-460811-5.50009-X]
[8]  
Marfurt K., 1989, HDB GEOPHYSICAL EXPL, P203
[10]   FREQUENCY-DOMAIN ELASTIC WAVE MODELING BY FINITE-DIFFERENCES - A TOOL FOR CROSSHOLE SEISMIC IMAGING [J].
PRATT, RG .
GEOPHYSICS, 1990, 55 (05) :626-632