An implicit staggered-grid finite-difference method for seismic modelling

被引:11
|
作者
Liu, Yang [1 ,2 ]
Sen, Mrinal K. [2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resource & Prospecting, Beijing 102249, Peoples R China
[2] Univ Texas Austin, Inst Geophys, John A & Katherine G Jackson Sch Geosci, Austin, TX 78758 USA
关键词
Numerical solutions; Computational seismology; Wave propagation; DISCONTINUOUS GALERKIN METHOD; ANISOTROPIC WAVE-PROPAGATION; SURFACE BOUNDARY-CONDITION; HETEROGENEOUS MEDIA; ELEMENT METHODS; ELASTIC-WAVES; ACCURACY; SCHEMES; STABILITY; MIGRATION;
D O I
10.1111/j.1365-246X.2009.04305.x
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
P>We derive explicit and new implicit staggered-grid finite-difference (FD) formulas for derivatives of first order with any order of accuracy by a plane wave theory and Taylor's series expansion. Furthermore, we arrive at a practical algorithm such that the tridiagonal matrix equations are formed by the implicit FD formulas derived from the fractional expansion of derivatives. Our results demonstrate that the accuracy of a (2N + 2)th-order implicit formula is nearly equivalent to or greater than that of a (4N)th-order explicit formula. The new implicit method only involves solving tridiagonal matrix equations. We also demonstrate that a (2N + 2)th-order implicit formulation requires nearly the same amount of memory and computation as those of a (2N + 4)th-order explicit formulation but attains the accuracy achieved by a (4N)th-order explicit formulation when additional cost of visiting arrays is not considered. Our analysis of efficiency and numerical modelling results for elastic wave propagation demonstrates that a high-order explicit staggered-grid method can be replaced by an implicit staggered-grid method of some order, which will increase the accuracy but not the computational cost.
引用
收藏
页码:459 / 474
页数:16
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