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傅里叶有限差分法三维波动方程正演模拟
引用本文:张金海,王卫民,赵连锋,姚振兴.傅里叶有限差分法三维波动方程正演模拟[J].地球物理学报,2007,50(6):1854-1862.
作者姓名:张金海  王卫民  赵连锋  姚振兴
作者单位:中国科学院地质与地球物理研究所,北京 100029
基金项目:中国科学院知识创新工程重要方向项目(KZCX2-YW-101)资助
摘    要:傅里叶有限差分(FFD)法兼有相位屏法和隐式有限差分法二者的优势,能够处理复杂地质构造中的波传播问题,但在三维情形下,算子的双向分裂会引起明显的方位各向异性误差.本文用Fourier变换计算双向分裂过程中的高阶交叉项,消除了方位各向异性误差.该方法充分利用了FFD法在双域实现的算法结构,明显减少了由于引入误差校正所带来的计算量.将该方法应用于修改后的三维French模型的地震正演问题,并将得到的叠后记录、单炮记录同全波有限差分法的模拟结果进行对比,结果证实了该方法对一次反射波具有较高的模拟精度,在内存需求和计算效率方面则具有更大的优势.

关 键 词:三维正演模拟  傅里叶有限差分  双向分裂  波动方程  
文章编号:0001-5733(2007)06-1854-09
收稿时间:2007-4-4
修稿时间:2007-04-04

Modeling 3-D scalar waves using the Fourier finite-difference method
ZHANG Jin-Hai,WANG Wei-Min,ZHAO Lian-Feng,YAO Zhen-Xing.Modeling 3-D scalar waves using the Fourier finite-difference method[J].Chinese Journal of Geophysics,2007,50(6):1854-1862.
Authors:ZHANG Jin-Hai  WANG Wei-Min  ZHAO Lian-Feng  YAO Zhen-Xing
Institution:Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China
Abstract:Fourier finite-difference(FFD) operator has both of the advantages of Fourier and finite-difference methods,it can handle the wave propagations in complex media with large velocity contrasts and wide propagation angles.In 3-D case,however,two-way splitting may cause artificial azimuthal anisotropy.In this paper,we handle the remnants of the conventional two-way splitting technique by Fourier transforms,and the azimuthal anisotropy is removed.Based on the dual-domain scheme of the FFD method,the proposed algorithm significantly reduces computational cost caused by error correction.Compared with the finite-difference method by the zero-offset records and shot profiles based on 3-D modified French model,the proposed method can properly model the primary reflected waves and is much more attractive in both computational cost and storage demand.
Keywords:3-D modeling  Fourier finite-difference  Two-way splitting  Wave equation
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