3D acoustic and elastic VTI modeling with optimal finite-difference schemes and hybrid absorbing boundary conditions

被引:3
|
作者
Xu ShiGang [1 ,2 ]
Liu Yang [1 ,2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, CNPC Key Lab Geophys Prospecting, Beijing 102249, Peoples R China
来源
关键词
Numerical modeling; Finite-difference; Optimized scheme; Anisotropic wave equation; Hybrid absorbing boundary condition; Graphic processing unit; PERFECTLY MATCHED LAYER; SEISMIC-WAVE EQUATION; SAMPLING APPROXIMATION; SPATIAL DERIVATIVES; ANISOTROPIC MEDIA; GRAZING-INCIDENCE; LEAST-SQUARES; PROPAGATION; DISPERSION; ORDER;
D O I
10.6038/cjg2018L0250
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 coefficients of the conventional finite-difference (FD) stencil are commonly determined by the Taylor-series expansion method (TEM), which can produce major numerical dispersion errors at large wavenumbers. To solve this problem, we develop a novel optimal explicit FD method (FDM) for the second-order spatial derivative. We first combine the TEM and multiple sampling to the spatial dispersion relation, and then construct an intuitive and effective objective function using the maximum-norm method (MNM) and solve it by the Remez iteration algorithm (RIA). The maximum-norm (MN)-based FDM is adopted to solve the 3D acoustic and elastic vertical transversely isotropic (VTI) wave equations. Moreover, we extend the 2D hybrid absorbing boundary conditions (HABCs) to 3D acoustic and elastic VTI media, and improve the absorbing effectiveness through reasonably adjusting wavefield velocities in the absorption areas based on anisotropy properties. To improve computational efficiency for a 3D case, we utilize graphic processing unit (GPU) instead of traditional central processing unit (CPU) architecture. Numerical accuracy analyses indicate that the optimal scheme has better tolerance to the numerical dispersion at large wavenumbers than the conventional TEM. Numerical modeling experiments for 3D homogeneous and modified Hess VTI models demonstrate that the proposed schemes have greater accuracy and efficiency than the conventional schemes and achieve significant absorbing effects.
引用
收藏
页码:2950 / 2968
页数:19
相关论文
共 55 条
  • [1] [Anonymous], 1934, Compt. Rend. Acade. Sc.
  • [2] Finite-difference modelling of S-wave splitting in anisotropic media
    Bansal, Reeshidev
    Sen, Mrinal K.
    [J]. GEOPHYSICAL PROSPECTING, 2008, 56 (03) : 293 - 312
  • [3] A PERFECTLY MATCHED LAYER FOR THE ABSORPTION OF ELECTROMAGNETIC-WAVES
    BERENGER, JP
    [J]. JOURNAL OF COMPUTATIONAL PHYSICS, 1994, 114 (02) : 185 - 200
  • [4] A NONREFLECTING BOUNDARY-CONDITION FOR DISCRETE ACOUSTIC AND ELASTIC WAVE-EQUATIONS
    CERJAN, C
    KOSLOFF, D
    KOSLOFF, R
    RESHEF, M
    [J]. GEOPHYSICS, 1985, 50 (04) : 705 - 708
  • [5] Chen JB, 2012, GEOPHYSICS, V77, pT201, DOI [10.1190/geo2011-0389.1, 10.1190/GEO2011-0389.1]
  • [6] Description of qP-wave propagation in anisotropic media, Part I: Pseudo-pure-mode wave equations
    Cheng Jiu-Bing
    Kang Wei
    Wang Teng-Fei
    [J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2013, 56 (10): : 3474 - 3486
  • [7] Chu CL, 2012, GEOPHYSICS, V77, pT57, DOI [10.1190/GEO2011-0180.1, 10.1190/geo2011-0180.1]
  • [8] CLAYTON R, 1977, B SEISMOL SOC AM, V67, P1529
  • [9] THE APPLICATION OF HIGH-ORDER DIFFERENCING TO THE SCALAR WAVE-EQUATION
    DABLAIN, MA
    [J]. GEOPHYSICS, 1986, 51 (01) : 54 - 66
  • [10] Di Bartolo L, 2012, GEOPHYSICS, V77, pT187, DOI [10.1190/geo2011-0345.1, 10.1190/GEO2011-0345.1]